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| author | nfenwick <nfenwick@pglaf.org> | 2025-02-07 12:11:56 -0800 |
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| committer | nfenwick <nfenwick@pglaf.org> | 2025-02-07 12:11:56 -0800 |
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diff --git a/.gitattributes b/.gitattributes new file mode 100644 index 0000000..d7b82bc --- /dev/null +++ b/.gitattributes @@ -0,0 +1,4 @@ +*.txt text eol=lf +*.htm text eol=lf +*.html text eol=lf +*.md text eol=lf diff --git a/LICENSE.txt b/LICENSE.txt new file mode 100644 index 0000000..6312041 --- /dev/null +++ b/LICENSE.txt @@ -0,0 +1,11 @@ +This eBook, including all associated images, markup, improvements, +metadata, and any other content or labor, has been confirmed to be +in the PUBLIC DOMAIN IN THE UNITED STATES. + +Procedures for determining public domain status are described in +the "Copyright How-To" at https://www.gutenberg.org. + +No investigation has been made concerning possible copyrights in +jurisdictions other than the United States. Anyone seeking to utilize +this eBook outside of the United States should confirm copyright +status under the laws that apply to them. diff --git a/README.md b/README.md new file mode 100644 index 0000000..d1c54fb --- /dev/null +++ b/README.md @@ -0,0 +1,2 @@ +Project Gutenberg (https://www.gutenberg.org) public repository for +eBook #55150 (https://www.gutenberg.org/ebooks/55150) diff --git a/old/55150-0.txt b/old/55150-0.txt deleted file mode 100644 index ff8f275..0000000 --- a/old/55150-0.txt +++ /dev/null @@ -1,4331 +0,0 @@ -The Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -This eBook is for the use of anyone anywhere in the United States and most -other parts of the world at no cost and with almost no restrictions -whatsoever. You may copy it, give it away or re-use it under the terms of -the Project Gutenberg License included with this eBook or online at -www.gutenberg.org. If you are not located in the United States, you'll have -to check the laws of the country where you are located before using this ebook. - -Title: Many-Storied Mountains - The Life of Glacier National Park - -Author: Greg Beaumont - -Release Date: July 19, 2017 [EBook #55150] - -Language: English - -Character set encoding: UTF-8 - -*** START OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - - - - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - - - - - - - ★GPO:1978-261-215/3 - For sale by the - Superintendent of Documents, - U.S. Government Printing Office, - Washington, DC 20402. - Stock Number 024-005-00709-1. - - Library of Congress Cataloging In Publication Data - - Beaumont, Greg, 1943- - Many-storied mountains. - - (Natural history series) - 1. Natural history—Montana—Glacier National Park. - 2. Glacier National Park. I. Title. II. Series: Natural history series - (Washington, D.C.) - OH105 M9B43 500.9′786′52 78-606071 - - - - - Many-storied Mountains - The Life of Glacier National Park - - - Written and - photographed by - Greg Beaumont - - 1978 - Natural History Series - Division of Publications - National Park Service - U.S. Department of the Interior - - [Illustration: The landform of Glacier National Park is a monument - to the power of moving ice. This view from Stoney Indian Pass is - startlingly different from the scene of a million years ago, when - the glaciers of the Pleistocene were sculpturing the land. Only the - higher peaks would then have been visible above the blanket of ice - that flowed like a slow-moving river down into the Mokowanis Valley - and out into the Great Plains beyond.] - - -About This Book - -This natural history of the mountain wilderness called Glacier National -Park is not a guidebook, but provides an overview of the ecology of the -region. At the same time, it is a personal statement, revealing one -individual’s response to this rugged, delicate land. - -For their consistent cooperation and helpfulness, I wish especially to -thank Chief Naturalist Ed Rothfuss and his capable staff. Technical and -field assistance came from many; for special thanks, I would like to -single out Art Sedlack, Francis Singer, Bert Gildart, Walt Martin, Craig -Kuchel, and Danny On. The manuscript profited greatly from the criticism -of Douglas Chadwick, to whom I am deeply grateful. - - —G.B. - - -The National Park Service Division of Publications gratefully -acknowledges the financial support given this book project by the -Glacier Natural History Association, Inc., West Glacier, Mont. - - - - - Contents - - - Song of the High Peaks 1 - Cycles and Seasons 5 - Bedrock: The First Story 6 - The Rising of the Sun and the Running of the Deer: A Glacier - Year 39 - Plant-and-Animal Communities 43 - Over Going-to-the-Sun Road 44 - Groves and Grasslands: The Prairie Sea 46 - The Forest 70 - Scrub Forest 105 - Tundra 109 - Water Communities 114 - Shooting Stars 121 - Appendix 125 - Pictorial Features - The Mountains of Glacier 10 - The Forests of Glacier 48 - The Vital Predator 78 - Protective Coloration 84 - _Ursus arctos horribilus:_ The Vulnerable King 88 - Bald Eagles and Kokanee Salmon: A Recent Gathering 92 - A Triumph of Many Colors 96 - Fire Succession: Key to Continuity 100 - - -Illustrations by Celia Strain/Morgan-Burchette Assoc. - - [Illustration: Soaring eagle] - - - - - Song of the High Peaks - - -April again and the wind turns on the Great Plains. Wedges of geese, -high and determined, began this storm of spring, their voices sharp as -the morning frost. Sicklebills cry to claim the land, sandhill cranes -wheel and talk overhead, and everywhere the killdeer shout. -Pasqueflowers push the bleak soil aside, beginning the westward rush -that I must join, seeking again the sight of mountains. - -In Glacier National Park the land is folded up. On the east, Chief -Mountain, Curly Bear, and Rising Wolf break the prairie’s hold. When the -early French fur trappers saw these peaks glistening in the distance -with summer-long snows and perpetual ice, they named this region “the -land of shining mountains.” But for all the ice and snow that reflect -the summer sun, the park’s present glaciers are but snowflakes compared -to the mighty rivers of ice that carved this land. Glaciation, the -magnificent sculptor, left its bold signature everywhere, and this park -honors with its name the force that shaped it. - -But the essential excitement of this land is more than cliff face, -spire, and sudden storm. It comes to you when you realize that here is -an aggregation of dramatically differing life zones, where a day’s walk -can easily take you from prairie and forest to treelimit and tundra; -where a dense forest of redcedar and hemlock, similar to the rain -forests of the Pacific coast, exists a score of kilometers from the -great prairie sea. - -Or it comes when you discover that these mountains—young and sharp with -shadows, snow-jeweled and newly gowned with forests—are chiseled from -the oldest unaltered sedimentary rocks on earth. - -I come from the prairie and love its broad strokes; I’ve learned to hear -the singing in the grass and to see those long, slow seasons soar the -level horizons like gliding hawks. But here I learned to match my days -against a wild earth, and in me grew the mysterious need to know a -mountain from its every side. Mountains that wear the dawn like yellow -hats, repeated in the named and nameless lakes. Mountains that stretch -the storms between them and balance rainbows ridge to ridge. - -I must see again the secret forest places, where the paleflowered -wood-nymphs hover like a breath, and know once more the endless meadows -painted camas blue. - -I need the perfect freedom of this land, to be able to say, _today I -will climb Siyeh_: to stand, for a time, on the rugged shoulders of this -upright earth. - - [Illustration: The sharp spire of little Matterhorn and the broad - face of Mt. Edwards loom above Going-to-the-Sun Road in the upper - McDonald Valley. During warm days in spring the valleys of the park - resound with the thunder of avalanches.] - - [Illustration: Twilight view.] - - - - - Cycles and Seasons - - -Bedrock: The First Story - -On the trail that connects the Logan Pass visitor center to Hidden Lake -overlook there is a shallow pond. Near Hidden Pass, it collects its -meltwater from the Continental Divide and sends it down the shallow -gorge that drains the Hanging Gardens; as a waterfall it plunges into -the upper St. Mary Valley where it becomes Reynolds Creek; joined by -other tributaries, it continues its long journey to Hudson Bay. - -The surface of this pond is seldom still, for the wind treats it like a -sea. Because the water is shallow, the wave action wrinkles the bottom -mud into ripple patterns, mimicking the churning waves. - -I like to come here early in the morning. Sometimes, arriving before the -wind awakes, I catch reflections of the surrounding mountains. Beyond -the low bench of Logan Pass the Garden Wall begins, running northward -with the Divide. In the eastern valley the pitched peak of -Going-to-the-Sun hunkers in the morning light like a tensed warrior. To -the south, the incisor Bearhat, beautiful cloud cutter of Hidden Lake -Valley, juts above the nearby saddle of the pass. But over this place, -standing as fresh monuments to an age of ice, tower the cliffs of -Clements and the pyramid Reynolds. - -I am sitting on a wedge of red rock. Its surface exhibits a wrinkled -pattern identical to the ripples in the soft mud of the shallow pond. -The distance is not great; with a stick I could reach out and touch the -mud. Yet this represents a gulf no bird can fly, for between the ripples -of this rock and the ripples of this mud lie billions of vanished -mornings, a constellation of years. - -These red, green, tan, white, black and purple bands of rock that layer -Glacier’s mountains comprise the oldest unaltered sedimentary rocks on -Earth. They were laid down in Precambrian time, more than a billion -years ago, when life was just beginning, as the deposits of an inland -sea. - -For millions of years, sand, mud and carbonates washed into the ancient -sea, compressing the lower layers into mudstones and limestones, -building up a sediment thickness that may have been as much as 10,000 -meters (_see_ metric conversion table on page 136). - -When we look at the sharp contours of Glacier’s mountains, we see the -evidence of uplift, overthrust and glaciation. But on the geologic clock -these are recent events, a mere eyeblink of time ago. For the vast -majority of years, the rocks lay undisturbed and level beneath the sea -and land. - -To understand better the tremendous time scale these rocks represent, we -need a way to visualize the vast collection of years. If we were to make -a movie of these geologic events, we would first need to determine how -many years each minute should represent. Since the Pleistocene lasted -about 3,000,000 years (its four ice ages sculpting the present muscle of -this land), let us make each minute portray a million years. To -chronicle these rocks we will then need a film 60 hours long! - -Not until the fifty-seventh hour of our film will the Mesozoic lowlands -begin to bulge with the coming Rocky Mountain chain. During the long -preceding hours we would have seen little else but sea—withdrawing, -advancing, deep and shallow; yellow, green, and brown with great -colonies of algae. Unseen below the water, lava has spilled out -occasionally on the sea bottom; once, it intruded between the rock -layers below, forming the conspicuous, 60-meter-thick band of black -diorite that we see today on many mountain faces in Glacier. - -During this time of initial uplift an amazing process is going on deep -underground. A major fault has developed, fracturing the buckled layers -of rock. A vast mountain plate begins to slide eastward, over-riding and -submerging the rock layers to the east and opening the wide trench that -is today the North Fork Valley. Known as the Lewis Overthrust, this -gigantic earth-force has created an unusual situation: ancient rock -strata lying atop recent rock strata. - -Now less than 3 minutes of film remain. The arrival of the ice is -imminent. We look at the landscape of featureless mountains and wonder -at the dramatic difference that this last 3 million years will make. We -do not see the familiar forests and lakes, the savage peaks, and the -broad, deep valleys of this present land. These mountains are gentle, -arid, and shallow-valleyed. The vague outlines are there; we recognize -the general alignments of the drainage systems, the bloated domes from -which sharp peaks will be cut. The mountains are connected to one -another by blunt ridges and smooth saddles, and the shadows they cast -are dull, dunelike. - -Suddenly the ice is there, filling the landscape, with only the -mountaintops protruding. Four times in these last 3 minutes of film the -ice sheets advance and retreat, each time leaving an altered landscape. -Strange lakes and forests fill the gaps between the glacial invasions. -Then we see the mountains we now know come into being rapidly, as if the -land were being hacked into shape by giant cleavers. - -After this flicker of Pleistocene time, the film ends, the forests -return, and familiar lakes shine beneath the sun again—these lakes and -forests we had thought to be timeless. - - -■ -Up springs the morning wind from Hidden Valley, making the nearby alpine -fir branches whiz with its passing and shattering the perfect reflection -of Bearhat Peak on the pond. From where I sit, it is a short distance to -Hidden Pass; so I leave the pond and walk to the overlook to see again -the fine basin quarried by an ancient glacier. - -Hidden Lake, deep, far below, so blue, fits into its cliffed, crooked -valley like a polished boomerang. Closely ringed by ridge and -peak—distant Sperry Glacier and pointed Gunsight peering up from the -southern jumble, and broad Bearhat impossibly close—this lovely lake is -almost lost amid such sharp proclamations of rock. Its outlet gorge -gives a narrow view across the angled, hidden valleys of Avalanche and -McDonald, past the pyramid of Stanton, to the low, faraway undulations -of the Whitefish Range. - -Glaciation is a cruel master of mountains, biting deeply into their bulk -and leaving sheer, spectacular contours when the glaciers disappear. The -landforms here attest to their power, everywhere exhibiting the effects -of glaciation. - -In eating back the mountain headwall, alpine glaciers formed rounded -depressions, called cirques. Unlike the narrow clefts left by running -water, these broad, deep basins look as though they were made by -ice-cream scoops gouging into the rock. Hidden, Ptarmigan, Iceberg, and -Avalanche Lakes sit in well-developed cirque basins, and many mountains -are dimpled by the beginnings of other cirques—the conspicuous -amphitheater on the south shoulder of Heaven’s Peak, for example. - -Occupying all major drainage systems, glaciers modified the contour of -the valleys, changing them from their narrow, stream-cut V-shapes into -broad U-shapes. Into these wide main valleys, waterfalls plunge from -higher, smaller valleys. Like rivers, flowing glaciers have tributaries. -Lacking the ice mass and cutting power of the main glaciers, these -tributary ice fingers could not bite as deeply into the bedrock. When -the ice melted, hanging valleys were left stranded high above the main -valley floor. Hidden Lake sits in one of these hanging valleys, and from -it Hidden Creek plunges 750 meters into Avalanche Basin toward McDonald -Creek. - -On my many previous visits to this pass I have been too busy enjoying -the wildflowers, the weather, or the scenery to realize what an open -textbook of glaciation is everywhere displayed. - -I stand here on a small saddle of a pass. Wherever glaciers met, passes, -or cols, were created. A high, notched pass like this one (or -Swiftcurrent or Gunsight) reveals recent connections. Broad, lower -passes, such as Logan, resulted where the ice early overran the mountain -ridge and had a chance to work longer. - -Where two glaciers worked on opposing sides of a ridge and failed to -meet, they formed an arête—a thin, steep-walled remnant resembling a saw -blade. Another ice age would probably consume the park’s many thin -arêtes, such as the Garden Wall and Ptarmigan Wall; but it would also -create new ones from existing ridges. - -Further testimony to the sculpting power of ice is presented by Mt. -Reynolds, looming to the east. The most dramatic feature of a glaciated -landscape is the pyramid-shaped mountain called a horn—and Reynolds is a -perfect example. Horns were formed when three or more glaciers cloaked -the mountain, excavating its sides toward its core and gradually -transforming its original domed shape into a sheer-sided peak. Glacier -has many remarkable horns, from the sleek spire of St. Nicholas in the -south to exquisite Kinnerly in the northern Kintla valley. - -Sperry Glacier stares back at me from the flank of Gunsight. Glaciers -found in the park today are not remnants of the last ice phase, which -ended here about 8,000 years ago, but are newly formed, having come into -existence some 4,000 years ago. They reflect a cooling trend in the -present climate. - -Shrinking steadily from their period of greatest extent in the middle of -the last century, these modern glaciers finally stabilized in the late -1940s and since then have shown only a slight increase in area. - -Movement distinguishes glaciers from icefields, and the movement of ice -is a force on as well as a feature of a landscape. A glacier excavates -by abrading and plucking at the rock. Alternately melting and freezing, -ice at the headwalls plucks out blocks of rock. Ultimately the rocks are -deposited along the sides or at the feet of the glacier as moraine -debris. But as they move in the grip of the ice, they constantly abrade -the rock surfaces they encounter. Polished rock beds of past glaciers -show striations—grooves gouged by rock fragments imbedded in the moving -ice. - -Flow rate of a glacier depends upon the thickness of the ice and the -degree of slope. Under tremendous pressure, ice becomes plastic, like -thick taffy. Unlike kilometer-thick continental glaciers, which may move -a hundred meters a day, small alpine glaciers seldom progress more than -two or three centimeters per day. - -Although a glacier moves, it gets nowhere if in a state of -equilibrium—when annual melting equals annual accumulation. Snow mass -gained at the sun-shielded headwall is usually lost as melt at the -exposed snout. Glaciers such as Sexton or Weasel Collar, whose snouts -perch on cliff edges, also lose mass by calving. Thunder you hear on a -late-summer day near such a glacier may actually be the sound of ice -pushed off from the lip of a cliff. - -Walking back to the visitor center, I suddenly stop where the trail -skirts the steep moraine of Mt. Clements. From the opposite side of the -moraine five mountain goats have appeared. Spotting me on the trail -below, they also halt. But before I can get to my camera they are off in -a stiff-legged gallop, running in single file along the crest of the -moraine to the distant safety of the mountain face. - -Moraines are ridges of rock debris piled up along the edges and -terminuses of glaciers. Like a bracelet lying against the wall of this -mountain, the circle of steeply piled debris marks the extent of a -small, recently vanished glacier. Ghost of the power that once resided -here, a stagnant icefield lies beneath the confining walls of the -moraine. The recent accumulation of these rock fragments is a mighty -accomplishment, attesting to the force of moving ice. - - _continued on p. 38_ - - [Illustration: The Mountains of Glacier - - Lying astride the Continental Divide in the Northern Rockies, - Glacier is above all else a mountain park. The special beauty of its - lakes, streams, and forests derives from the microclimates and - varied topography and soil produced by mountain-building and - mountain-eroding forces.] - - [Illustration: Overthrust Mountains - - 1 A hypothetical block of the Earth’s crust in the region of Glacier - National Park as it existed more than 60 million years ago. The two - layers shown actually represent many strata of sedimentary rocks. - - 2 Lateral pressure begins to force the rock layers to buckle. - - 3 A large fold has been created, forcing the rock strata to double - over and overturning some layers. A break, or _fault_, is forming at - the plane of greatest stress. - - 4 The break has been completed and the strata west of the fault have - slid eastward, up and over the rocks east of the fault. - - 5 The Glacier landscape today. Throughout the millions of years - during which the folding, faulting, and overthrusting have been - taking place, the process of erosion has continued; a thousand - meters of stratified rocks have been worn away, so that only a - remnant of the overthrust layers can be seen today. Because - Glacier’s eastern slope represents the eroded face of the overthrust - block, the mountain range rises precipitously from the prairie, with - no foothills breaking the abrupt transition from open prairie to - mountain valley.] - - [Illustration: The peaks in this photograph (a view to the northwest - from Marias Pass) are remnants of the overthrust block, which moved - eastward. The dividing line between the light-colored rocks and the - gray talus slopes beneath them is the Lewis Overthrust Fault.] - - [Illustration: Glaciation - - 1 This is how the landscape in this region might have appeared - before the onset of the Pleistocene, millions of years ago. Note the - stream-eroded, V-shaped valleys. The climate at that time was dry. - - 2 Glaciers began to form high on the peaks, crept downward, and - joined to form larger glaciers. - - 3 After many centuries of glaciation, tributary glaciers have cut - back into the peaks, forming basins called _cirques_. Thick - glaciers, moving rapidly and carrying rock fragments, have abraded - the main valleys’ floors and sides, widening and deepening the - valleys into characteristic U-shapes.] - - V-shaped Valley - Tributary Glacier - Unglaciated Peak - Headwall - Meltwater Stream - Nose of Glacier - Crevasse - - [Illustration: 4 In the present landscape, free of all but remnant - glaciers, small lakes called _tarns_ occupy many of the cirque - basins; and waterfalls plunge into the main valleys from higher, - shallower, tributary valleys, called _hanging valleys_. _Alluvial - cones_—recent accumulations of rock debris—have begun to build along - the valley walls. In the main valley, a _moraine_ (a deposit of rock - materials left by the retreating glacier) has formed a dam that - holds back a large lake. - - During all this time, all parts of the terrain not buried under ice - and snow have been weathered and eroded by nonglacial forces. Thus - the contours of the jagged peaks and sheer cliffs have been - softened.] - - Unglaciated V-shaped Valley - U-shaped Valley - Hanging Valley - Cirque - Tarn - Alluvial Cone - Moraine - Morainal Lake - - [Illustration: Glacial landforms can be identified in this view of - the Mokowanis Valley.] - - [Illustration: A Divided Climate - - Because of an eastward flow of cool, moist Pacific air masses, the - climate of northwestern Montana, including the western portion of - Glacier National Park, differs from that of other portions of - Montana. As a result of increased precipitation, Glacier’s western - valleys support a rich flora, more typical of the Pacific Northwest. - - West - - Moist Pacific air - - As the moisture-laden Pacific winds are pushed up the windward - slopes of Glacier’s mountains, the air cools and water vapor - condenses, forming fog or clouds. Rain or snow begins to fall as the - air continues to rise and cool. By the time the air mass reaches the - crest and flows down the leeward slopes, most of the moisture has - been lost. - - Western slopes average about 70 cm. of precipitation at elevations - between 900 and 1,100 m. Upper elevations average 200 to 250 cm., - mostly in the form of snow; and 300 to 500 cm. is common. - - East - - Dry chinook winds - - Eastern slopes, under the influence of Continental air masses, - receive less annual precipitation. West Glacier’s annual average is - 66.5 cm. Babb, a small town east of the park, averages 49.3 cm. - Frequent high winds east of the Divide further reduce moisture - through evaporation. - - Exposed to Arctic air masses flowing down from Canada, locations - east of the Divide also suffer more severe winter conditions than do - protected western valleys. Average January temperature is -5°C at - West Glacier, -8° at Babb. - - Moreover, 80 percent of the winter days in the western portion of - the park are overcast, a condition almost identical to that of - Seattle, Wash. This serves to moderate winter temperatures and to - minimize evaporation.] - - [Illustration: Moss campion and mountain forget-me-not colonize a - fellfield. Fellfields are rocky alpine sites that are slightly less - than 50% bare rock, interspersed with such plant pioneers as cushion - plants, mosses, and lichens.] - - [Illustration: High lakes generally occupy cirque basins. These - depressions in the valley bedrock, quarried by glaciers, are deepest - near the headwall where ice thickness was greatest. Cold and deep, - and ice-free only weeks each year, tarns cannot support vascular - plants or vertebrates. Iceberg Lake, shut off from the sun most of - the year by the encompassing 1,000-meter walls of Mt. Wilbur and the - Ptarmigan Wall, is never completely free of ice.] - - [Illustration: Lake McDonald, 16 kilometers long, 2 kilometers wide, - and 134 meters deep, is the largest lake in the park. Its basin is - the classic U-shaped glacial valley. Forested lateral moraines on - either shore gently rise 600 meters above lake level. - Going-to-the-Sun Road snakes along the eastern shore, and Logan Pass - lies near the center of the photograph, behind the peaks of the - Lewis Range.] - - [Illustration: Subjected to the drying and shaping effects of wind - both winter and summer, this Douglas-fir, growing in the prairie - community near St. Mary, will attain neither the symmetrical shape - nor the great size of the Douglas-firs growing in moister, more - sheltered sites on the western slopes of the Continental Divide.] - - [Illustration: Freeze-and-thaw cycles continually fracture and - loosen rocks along joints, making them subject to removal by the - actions of water, gravity, and avalanche. The resulting fans of rock - debris (talus cones) indicate the extent of erosion since the - withdrawal of the Pleistocene glaciers.] - - [Illustration: Although moving water is an agent of erosion—the - primary destructive force of mountain masses—it also permits life. - Even small watercourses, such as this freshet, abound with plant and - invertebrate life.] - - [Illustration: Going-to-the-Sun Mountain, towering above the St. - Mary Valley, from the trail to Siyeh Pass. The coniferous forest at - its base and the alpine tundra plants at its summit are closely - juxtaposed in space; but if these two communities grew at the same - elevation they would be separated by thousands of kilometers. Hiking - from St. Mary Lake up to Siyeh Pass is going, in effect, from - Montana to the Arctic Circle; but here the life zones are compressed - and sharply divided rather than extended and overlapping.] - - [Illustration: Setting moon and snow shelf near the summit of - Heavens Peak. Note stratification of Precambrian sediments.] - - [Illustration: Western redcedars line the shores of Lake McDonald. - Because of prevailing air currents from the Pacific coast, winters - in the protected western valleys are moist and comparatively mild, - and this deep body of water freezes over an average of only one - winter in four.] - - [Illustration: Moose often follow the spring snowmelt upwards to the - headwaters of drainages. This bull will remain at Thunderbird Pond, - at the base of Brown Pass, until autumn, when it will return to its - Waterton Valley wintering ground.] - - [Illustration: Because of the high reproductive capacity of insects - and small mammals, if all their offspring survived the earth’s plant - life would be consumed within one year. This is prevented by natural - controls such as predation and parasitism. The American kestrel - (“sparrow hawk”) feeds primarily on large insects and on small - rodents such as the meadow vole here.] - - [Illustration: Gray jays are found in the deep coniferous forests of - the park. In some parks gray jays, or “camp robbers,” loiter about - campgrounds and picnic areas begging or stealing food. In Glacier, - however, they are seldom noticed as they search out seeds, berries, - and insects.] - - [Illustration: A generalized predator, the coyote will eat almost - anything, from berries to carrion. When man eliminated most of the - coyote’s enemies and competitors, including the wolf, grizzly, and - cougar, it enlarged its range to fill the void. Intelligent and - social, the coyote thrives despite man’s persecution. Although most - numerous in the prairie community, it ranges up to timberline.] - - [Illustration: The spruce grouse is a year-round resident of the - spruce/fir and lodgepole communities. It forages on the ground for - seeds and insects, in winter turning to needles. Several other - species of grouse occupy different habitats in Glacier.] - - [Illustration: Chipmunks are found in every community, from prairie - to tundra, in Glacier. Each of the park’s three very similar species - has its preferred habitat. The diurnal counterpart to nocturnally - active mice, which have the same diet of seeds, berries and - occasional insects, chipmunks adapt easily to the presence of people - and become nuisances if encouraged by handouts. Feeding rodents is - dangerous and is harmful to them. By altering their diets and - blunting their cautious instincts, daily exposure to “free lunches” - makes the animals less fit to face the harsh realities of their - natural environment.] - - [Illustration: Unlike whitetail deer, which remain in lowland areas - all year, mule deer range upward into high meadows during the - summer. The bucks, especially, are wanderers and travel together. - Velvet antlers, worn during the time of summer sociability, presage - the autumn contests to come.] - - [Illustration: The checkerspot butterfly belongs to the most diverse - group of animals on the planet—the insects, whose importance can - hardly be overestimated. They not only help recycle nutrients in the - living community and provide an abundant food base for other - lifeforms, but are instrumental in pollinating most of the earth’s - terrestrial plants.] - - [Illustration: Alpine vegetation must be able to survive freezing - temperature during the growing season, since winter conditions are - possible even in summer. Early bloomers, such as the glacier lily, - endure repeated snowfalls during the unstable weather conditions of - June.] - - [Illustration: Unlike mountain goats, these bighorn rams will desert - the alpine zone at the approach of winter; they will join other - bighorns congregating in the lower valleys.] - - [Illustration: In November bighorn sheep rams end their summer-long - isolation from the ewes, move down from the higher slopes, and begin - a bloodless but taxing ritual of strength and endurance to determine - the harem master. The sharp reports of clashing horns may carry for - kilometers, and the contests continue for weeks until the dominant - ram emerges. (Note the Many Glacier hotel complex in the valley - below.)] - - [Illustration: Hummingbirds, like shrews and other small-bodied, - warm-blooded animals, exist at the theoretical thresh-hold of life. - Because of their small size, body volume is not large enough in - relation to surface area to prevent a rapid loss of body heat. To - compensate for this, metabolic rates must be high; food is rapidly - processed and used up. Thus, since fat reserves are not practical on - such small animals, they must eat at frequent intervals. - - Two species of hummingbirds—the rufous and the calliope—are found in - Glacier. Pictured is a female rufous (which weighs about the same as - a dime) landing on its lichen decorated nest to feed its two young - on a protein-rich mixture of nectar and small insects.] - - [Illustration: The insect-eating yellowthroat prefers moist - habitats. Unlike many of its treetop-dwelling relatives, this tiny - (10-11 cm.) warbler is usually seen near or on the ground.] - - [Illustration: Bands of bighorn ewes and lambs do not summer as high - as the rams and are often encountered in the scrub-forest zone. Note - the gnarled limber pine in the foreground of this photograph taken - on the south face of Altyn Peak.] - -Reaching the mountain wall, the goats scramble upward to a ledge, -sending scree streams pouring from several clefts. Encountering a -narrow, steep snowbank, they do not hesitate but continue across the -slope. Above the rock fingers of this peak the gathering clouds grow -black. A sudden crack of thunder hurries me down the trail. - -Although geologically young, the Rocky Mountains in Glacier are composed -of soft sedimentary rocks that are easily assailed by the many agents of -weathering and erosion. If not rejuvenated by continual uplift, these -magnificent peaks will glimmer but briefly in the long memory of the -planet. - -Already the sharp countenance of this land is being softened by the -ongoing forces of erosion. Chief among these is water, which attacks the -mountains everywhere. In addition, frost action continually exploits -rock fractures, breaking down blocks of rock into talus and scree. -Avalanche and rockfall sweep down the slopes. Layers of softer rock -erode quickly, undercutting more resistant rock and creating overhangs -which gravity, in time, will collapse. - -The lashing rain catches me on this sun-and-storm-contested pass. Ice, -gravity, wind, and especially water—all attack a land that dares the -clouds. - - -The Rising of the Sun and the Running of the Deer: A Glacier Year - -As if to make up for the days-long darkness of this last blizzard, the -peaks today wear snow plumes—long, graceful trails of white, curving up -into an ice-blue sky. Yesterday the snow-mad wind raced through the -forest. Today the motionless trees are cloaked in heavy, glistening -robes, the leafless aspen and young larch bent down. - -Moderate snowfall helps many plants and animals survive the winter. For -ground dwellers it provides insulation from the wildly fluctuating -winter temperatures encountered east of the Divide, protecting the -hibernators and providing cover for the many small mammals that remain -active during the winter. Wind-swept ground freezes deep; but under a -mantle of snow life-sustaining heat is trapped, permitting many animals -to survive and allowing the work of decomposers to continue. - -But this has been a winter of too much snow and too many temperature -extremes. The heavy snowpack has forced the sharp-hoofed deer to yard up -in great numbers; unable to range freely in deep snow, they are forced -into smaller and smaller confines where their numbers allow them to -break and maintain trails. But in time they exhaust the food supply. -Younger deer, unable to reach the increasingly higher browse line, -starve first. Then the does, heavy with unborn fawns, grow weak and fall -to predators. So the imprisoned herds dwindle quickly this year, -sometimes less than a kilometer from plentiful browse. - -Deep snow is also death for many seed-eating birds. As they are unable -to scratch for food, their body furnaces quickly fail, and during a -night of cold wind their fluffed corpses drop into the snow. - -Exposed to the noon sun, the snow surface thaws; when refrozen, it is -restructured to crystalline ice. If snow repeatedly thaws and freezes, -an ice barrier is formed, shutting off vital air exchange. Plants are -then subject to rot, and micro-animal life is smothered. Travel beneath -the snow is made more difficult for mice and shrews and they are -deprived of food and cover. Under such conditions their numbers rapidly -decline. - -But while many starve in a winter of deep snow, others benefit. The -exposed traffic of small mammals is to the owl’s advantage. Foxes and -coyotes more easily run down rabbits and hares on crusted snow. Deer -and, to a lesser extent, wapiti and moose—their hoofs punching through -the snowpack—swiftly tire in deep snow and become helpless before cougar -or wolf, whose lighter weight is supported by the crust. - -Grim as this winter’s toll becomes, enough will survive to begin the -process of renewal in spring. Last winter, a season of light snow, was a -time of hardship for predators. The deer remained strong, the wapiti -remote on high, windswept ridges, and the small mammals hidden. - -Only the water ouzel, winter after winter, seems not to notice the -hardships of the season. Lord of his small world of open water, he sings -in February, wading and swimming his diminished stream to find a -never-failing supply of water insects and small fish. It is a voice of -spring—glad, wild, continual as the moving water—an incongruous song in -this winter-shrouded land. - -But with the growing stature of the sun, the grip of winter softens. The -firs and spruce send their loads of snow sliding to the ground. Streams -begin to sing again and soon the lakes increase, the booming of -splitting ice breaking the silence of the valleys. Avalanches thunder -down the steeper slopes, carrying trees to the swollen streams. Rivers -hiss and rage, speeding the debris along. A spring that comes too -suddenly will bring flood to lower elevations. - -Snow geese thread through the valleys, and ground squirrels tunnel up -through snow to find invasions of birds returning from the south. Soon -the three-petaled wakerobins appear, chasing the snowline up the ridges. -Glacier lilies and Calypso orchids are next, and with the shooting stars -spring arrives. - -The melting snow releases a new group of animals to populate the -winter-thinned land. Up come chipmunks. Bears reappear. Young red -squirrels, helpless and blind, squirm in their nest holes. Hidden dens -rustle with pups and kits. Soon warm days will bring them out and the -business of learning to cope with their world will begin. - -All life responds irresistibly to the growing strength of the Sun. -Cottonwood, willow, and maple come into flower and unfold new leaves; -green needle clusters spot the limbs of larches that in winter had -seemed lifeless snags among the other conifers. Beneath the soil of -prairie, meadow, and forest, in the mud of lakes and ponds, other life -stirs; armies of insects, spiders, crustaceans, amphibians, and fish -will strive to complete their life cycles against the formidable odds of -a predatory world. - -Spring reaches higher up the mountains, the lowlands passing into -summer. Wapiti and mountain sheep follow the rising tide of succulent -browse up to the high meadows. In forest, grove, and meadow and along -the stream new fledglings appear—thrush, vireo, hummingbird, waxwing, -harlequin duck, bluebird, osprey, and flicker—as holes, nests, and -cavities brim with begging mouths. - -In the alpine meadows, where snow overlaps the spring and winter follows -hard behind the summer, the growing season is short and the climate -unstable. Sensing the stronger light, flowers push up impatiently -through the snow and hasten into bloom. Pikas and marmots scurry and -sunbathe among the rocks of scree slopes. - -Summer matures in ripening huckleberries, and the bears that grazed the -spring grasses now gorge themselves fat. Dry days of August bring -probing lightning, threatening the forests with fire. - -Sweeps of beargrass reach their climax now in the highest meadows. In -dizzy succession wildflowers set seed. Fat and sluggish, marmots and -ground squirrels disappear beneath the rocks. The golden eagle must -search longer each day to find prey within its vast domain. - -Autumn lingers in the valleys and on the flanks of low ridges. The -morning sun glints on hoarfrost, firing the yellow leaves of larch, -aspen, birch, maple, and cottonwood, and shines on the blood-red berries -of mountain-ash. Soon a night of killing frost will bring down the -corpses of insects and spiders by the millions. The reptiles and -amphibians, being cold-blooded animals, seem out of place in this -long-wintered land. Unable to maintain body temperatures appreciably -above their surroundings, they are the first to seek the protection of -hibernation, collecting in dens or burying themselves beneath the ooze -of pond bottoms. - -Songbirds gather and leave the valleys. The harsh cries of jays sound -ominous now in the forest. Only the chickadees seem to ignore the long -tree shadows; their ceaseless conversations carry through the leafless -underbrush as they busily search for seed. - -Velvet has gone to bone, and in these final noon-warm days the rut runs -through the land. It begins in the valleys in September with the -joustings of deer and moose and the buglings of bull wapiti puncturing -the forest silence. By November the higher meadows ring with the -collisions of bighorn rams who compete for ewes by smashing together -their massive, curled horns. On high slopes mountain goat billies -posture and swagger; head to tail, they circle, threatening each other -with dagger-like horns. - -From Flathead Lake, 100 stream kilometers to the south, kokanee salmon -return to spawn in the clear, cold shallows of McDonald Creek. Gathering -bald eagles surround the stream, again and again lifting vulnerable fish -from pool and riffle. Perched by the hundreds along the stream course, -their white heads and tails glistening against the dark trees, they -stand out like lanterns strung for a banquet. - -Now the stinging wind comes down from the peaks and shuts the lakes. -Life slows or sleeps. Ptarmigan, snowshoe hare, and longtail weasel, all -wearing winter white, seek shelter and food in a silent land where -spring and yellow lilies seem forever lost. - - -■ -All life faces one ultimate challenge: to survive or not, to reproduce -or fail, to bring one’s kind to tomorrow’s sun or vanish forever. This -land is harsh. To survive in nature demands skill in the individual, -excellence in the species, and a chance from the environment. - - [Illustration: The mink, a solitary predator associated with - low-elevation watercourses, preys on anything it can catch and - subdue.] - - - - - Plant-and-Animal Communities - - -Over Going-to-the-Sun Road - -I like to begin with St. Mary, a lake the whitecaps love to run. From -the far passes the several winds gather and collect, arranging long -lines of white waves for the race downlake. Past the purple scree of -Mahtotopa and Little Chief they go, white as the headdress of -Going-to-the-Sun Mountain, colliding, collapsing along the promontory -snares about the Narrows. Onward they press, spreading out and setting -sail for the straight rush to the final shore where a line of -cottonwoods sings with a sound like applause. - -Across the lake the timbered ridge starkly contrasts the finger of -prairie that claims the north shore. This is a flower-glad place, a -meeting-ground for mountain and prairie plants. Along the road the -grassland holds the conifers back, allowing only scattered clumps of -aspens. - -Finally, at Rising Sun, beneath the shadow of Goat Mountain, the prairie -ends and wind-seasoned Douglas-firs announce the coming forest. - -There’s excitement now, with the prairie heat gone, the wind scent raw -with fir and high meadows, honed by waterfall and tall, dank rock. Our -mountain thirst is never extinguished, and a road that tightens down to -cliff face and sudden turn brings back to our blood the ancient need to -go to the highest place. - -There is sword-edged Citadel, and the snow-flanked spike of Fusillade -holding court like a queen in this valley of peaks; then the dome of -Jackson and the Gunsight notch. Our eyes are kept high, transfixed at -last by looming Heavy Runner and the distant promise of Reynolds. - -Looking for mountain goats, we scan the walls around the sweep of Siyeh -Bend, catching a glimpse of the trail that crosses the scree to hidden -Piegan Pass. - -Beargrass heads lean out above the road like old men conferring on the -view. The purple trumpets of penstemon crowd the rocks, and spots of -Indian paintbrush lead like a blood-trail to the higher slopes. - -Intoxicated now, feeling the fresh full force of the wind from Logan -Pass, we race on. We hardly notice the struggle of the forest in -Reynolds Creek far below, how it thins and loses strength in its own -hard climb. We sweep past it on the broad magnificence of this pass. - -Level but a moment, the road dips to a shelf on the headwall above Logan -Creek and swings over the great sculptured cliff of the Garden Wall. For -several kilometers this masterpiece of a road glides down a constant -grade, squeezed between rock face and space, twisting into tight -drainages—a road for storm lovers, wet with spray and snow-seep, its -quick turns concealing sudden winds. - -Mighty, snow-robed Heaven’s Peak appears, taking our attention from the -Pass-group mountains and the hanging valley that spills Birdwoman Falls. -Northward is the great array of peaks encircling distant Flattop, -jumbles of mountains and glaciers. How are we to notice the forest far -below? - -Not until we have passed the Loop and are moving past the blackened -snags of a recent burn do we realize the stature of this forest. The -long road down will take us into a valley much deeper than any on the -eastern side. Near Avalanche Creek are trees we have seen nowhere else -in the park—giant western redcedars, western hemlocks with their nodding -tops, monstrous black cottonwoods with bark so deeply furrowed that it -looks hewn by hatchet. - -We take a long ride down the valley, past the low pyramid of Mt. -Stanton, final peak in the Livingston Range. Near the outlet end of Lake -McDonald, birch and aspen again appear in numbers, and the road enters a -crowded stand of lodgepole pine. - -Our memories cluttered with mountains, waterfalls, and snowfields, we do -not quite realize the significance of this 80-kilometer journey. We have -crossed the boundaries of several different plant-and-animal -communities, spanning a range of climate that would be encountered on a -5,000-kilometer north-south journey at sea level. - -At first glance the various trees, wildflowers, and animals seem -randomly distributed, scattered about like the distant mountains. But -mountainous terrain represents an organized high-rise approach to life. -From the lowest, most protected valley to the highest wind-and-ice-cut -summit, the life-forms align themselves, each according to its own -climatic tolerance. - -Here too can be seen the great cycles of nature: fire and regrowth, the -building of soil and its erosion, the incessant duel of the eaters and -the eaten. - -In the following sections we will spend some time in these various -communities, from prairie to tundra. - - -Groves and Grasslands: The Prairie Sea - -There is something about spring on the prairie that gets me up before -dawn. I like to watch the seasons change their guard over the landscape, -from the wintry cold of pre-dawn dark to the spring-scented morning air -to the hot summer-foretaste of the noon May sun. - -Hoarfrost surrounds these patches of pasqueflowers, blue goblets on -downy stems. On this windless night, frost has formed everywhere, -reclaiming for a time its vast winter range, sparkling over the green -handiworks of spring. - -But the god of the growing grasslands is the sun, and it now proclaims -itself, stretching out to make the mountains shine. With its assault the -frost collapses, becoming bright beads on grass tip and leaf joint by -which a beetle might refresh itself. - -Spring is best perceived ant-level, at its ground beginnings, where the -bright yellow-green tips of new grass shoots reclaim the winter-blighted -land. I look closely at a drag line of spider silk; a necklace of -dewdrops slides down, collects to a moment’s greatness, in which I -briefly see a curved horizon, the morning sunburst, and myself, before -it falls away. - -Getting up from my prone position, my belly damp from the prairie earth, -I startle a whitetail jackrabbit; bounding high, it zigzags off. The -commotion disturbs a distant badger, which faces about from its diggings -to confront danger in whatever form it might take. It swings its snout -to scent the air. Somewhat uncertainly, it returns to the business of -hunting, then hesitates, swings about once more and waits, myopic, -patient. - -Satisfied at last, the spurt of the now distant rabbit lost in its -brain, the creature snorts a defiance at the mystery and resumes its -morning gopher hunt. - -Overhead a marsh hawk skims past, its flight erratic as a butterfly’s. -Far away a magpie rattles at the passing hawk and takes flight, briefly -flashing black and white. - - -■ -It is easy to see only pieces in the natural puzzle—a badger throwing -dirt, horned larks dipping into wind, black ants dragging the rosette of -a dead spider—and be satisfied with the scattered scenes. But at last, -to make it meaningful, we must complete the picture. There is that -special joy in discovering larger schemes: green plants utilizing -sunlight; a rabbit building its days at the plants’ expense; the falcon -tearing the rabbit meat for its young; magpies picking at the fallen -falcon; and then, in the end, all returning to the earth. - -Here on the prairie, as in every plant-and-animal association, the -ancient drama repeats itself over and over; the distant tundra is a -drastically different stage with different actors, but the cycle is the -same. Life depends upon the interaction of all its many forms. Unseen -bacteria are as necessary to the land as green grass; the meadow vole -and the coyote are as much a part of the prairie as the grasses. - -The secret of life rests in the wonder of photosynthesis. Only green -plants can manufacture food from the earth’s raw minerals. This is the -vital first step upon which the great pyramid of animal and plant life -is built. Using energy from the sun, green plants combine water and -carbon dioxide to synthesize sugar, and give off oxygen as a by-product. -The caterpillar takes its energy from the plant tissue, converting to -protein the sugar and minerals in its body. The caterpillar is then food -for a spider or other predator. A yellow warbler may take the spider and -in turn be ambushed by the prairie falcon. Thus the energy produced by -the plant travels through the food chain. When the prairie falcon dies, -scavengers—including insects and other invertebrates, birds, and -mammals—redistribute its wealth among themselves; the rest is decomposed -by bacteria. Thus, eventually, the nutrients on which the plants depend -return to the soil. - -When we look at any living organism, whether it is plant, herbivore, -carnivore, parasite, scavenger, or decomposer, we are soon made aware of -its associations with other living things, each puzzle piece leading us -to another and another. We begin to see a picture whole—the fox, meadow -mouse, grasshopper, bunchgrass, and sparrow hawk—all interlocked. - -Geologically speaking, grasslands are a recent development. As the Rocky -Mountains were being uplifted, the prevailing warm, moist climate began -to change. The rising mountain mass intercepted moisture-laden winds -that blew in from the Pacific, creating a rain shadow that lengthened -eastward as the mountains rose higher. A continental climate, -characterized by severe winters and dry, wildfire summers gradually took -shape, extinguishing the great forests that had grown across the -continent’s interior. Herbaceous plants, which had been evolving amid -the forests, inherited the land. - -Unlike trees, grasses die back to the ground each winter, hoarding their -life-germ beneath the protecting soil. Growing not from the tip but from -the joints, grasses regenerate quickly after fire or grazing. Suspension -of the normal metabolic processes enable the grasses to go dormant and -thus survive periods of severe heat and drought. - -Although the great prairie sea washes up against Glacier’s eastern -boundary, with estuaries probing into the mountain valleys on the drier, -south-facing slopes, the grassland community comprises less than 5 -percent of the land area of Glacier National Park. This includes the -puddles of prairie west of the Divide that interrupt the dense -coniferous forests along the North Fork of the Flathead River. - -From the pasqueflowers that bloom in early May to the asters and -goldenrod of September, these summer-long gardens of grasses and flowers -lean with the wind. Here are timothy, oatgrass and the -bunchgrasses—rough fescue, bluebunch fescue, and bluebunch wheatgrass. -Among the grasses bloom bitterroot, blue camas, lupine, gaillardia, -balsamroot, cinquefoil, sticky geranium, and wild rose. - - _continued on p. 68_ - - [Illustration: The Forests of Glacier - - From the lush redcedar-hemlock forest in the McDonald Valley to the - subalpine fir, whitebark pine, and Engelmann spruce struggling for - existence near treeline, the forests of Glacier reflect the - conditions of temperature, exposure, soil, and drainage prevailing; - and each forest has its characteristic association of understory - trees and shrubs, herbaceous ground cover, and vertebrate and - invertebrate animal life.] - - [Illustration: Life Zones - - Many physical and climatic factors determine the range of Glacier’s - plant-and-animal communities. Boundaries between communities are - seldom sharply defined, but rather merge together in broad zones of - transition. - - With elevation gain, average daily temperature drops at the rate of - 5° per 900 meters. Precipitation, wind velocity, and evaporation - loss increase. Soil thins. These factors, along with others such as - fire frequency, north or south exposure, and availability of - moisture, combine to determine the range of each community. - - In the forest community below 1,800 meters, Douglas-fir, lodgepole - pine, and western larch predominate. In the valleys, Engelmann - spruce and subalpine fir are found. The somewhat lower and much - better watered western valleys of the park support western redcedar - and western hemlock. - - Treeline is the upper limit to which the tolerances of trees to - environmental conditions permit them to grow. Because there are so - many controlling factors (wind, temperature, exposure to sunlight, - snow cover, etc.) treeline in the diagram is only approximate. In - Glacier it averages 2,000 meters. Avalanche chutes or sheer cliff - walls may suppress it to below 1,500 meters; on protected slopes it - may be as high as 2,150 meters. - - At the eastern edge of the park below 1,200 meters, the forest gives - way to the prairie community, composed mostly of soft-stemmed plants - adapted to the conditions of low precipitation that prevail here in - the rainshadow of the mountain range. Clumps of aspen, found in the - prairie in sheltered spots, occur here in the transition zone - between prairie and forest.] - - [Illustration: A Mountain Profile - - This diagram represents the eastward-facing slope of a hypothetical - mountain near the eastern boundary of Glacier National Park. Its - life communities are somewhat different from those of mountain - slopes at the western edge, chiefly because of the differential in - annual precipitation. - - Illustration: Here, above approximately 2,750 meters, in a realm of - ice, snow, and barren rock, there is little life. - - Alpine tundra - - Below 2,750 meters and above 2,000 meters, depending on other - factors such as exposure to sun and wind and steepness of terrain, - exists the alpine tundra community, with vegetation similar to that - of the vast, essentially level, treeless zones of the Arctic. - - Scrub-forest - - Roughly between 1,800 and 2,000 meters, the dominant vegetation is - scrub-forest. Trees here are stunted; except in sheltered spots they - are more or less prone rather than upright. Net growth is slow, not - only because of the short growing season but also because of the - pruning effect of icy mountain winds. Very few tree species can - survive in this harsh habitat. - - Coniferous forest - - In the forest community below 1,800 meters, Douglas fir, lodgepole - pine, and western larch predominate. In the valleys, Engelmann - spruce and subalpine fir are found. The somewhat lower and much - better watered western valleys of the park support western redcedar - and western hemlock. See page 54 - - Prairie - - At the eastern edge of the park below 1,200 meters, the forest gives - way to the prairie community, composed mostly of soft-stemmed plants - adapted to the conditions of low precipitation that prevail here in - the rainshadow of the mountain range. Clumps of aspen, found in the - prairie in sheltered spots, occur here in the transition zone - between prairie and forest.] - - [Illustration: The Forest Community - - A forest is organized vertically like an apartment house or office - building, with layers corresponding to stories. The _canopy_ is the - branches and foliage of tall trees that form a roof over the - community. Below the canopy are the _understory_ trees: young - individuals of the canopy species; and small, shade-tolerant trees - that will never become part of the canopy. Beneath the understory - branches is the _shrub layer_, occupied by knee-high-to-man-high - woody plants; beneath that is the _herb layer_, where most of the - ferns, wildflowers, grasses, and smaller woody plants grow. The - _forest floor_ is the zone of mosses, mushrooms, creeping plants, - and forest litter (leaves, twigs, needles, feathers, bits of bark, - animal droppings, etc.). The forest has a “basement,” too, - interlaced by plant roots, mycelia of fungi, and tunnels of myriad - animals. - - Each layer of the forest has its characteristic animal species, but - most forage over more than one level. Some nest in one story and - feed in another. The red squirrel races back and forth from the - forest floor to the highest branches. - - The forest community also has a socio-economic organization. Every - animal (and plant) takes up space and consumes a portion of the - available nutrients. Each has a place in the community food - chain—as, for example, _herbivore_, _carnivore_, or _scavenger_. - Each directly or indirectly affects all the other organisms. - - The Forest Community - - The role of a species in the community, like the job and social - function of a person, is its _niche_. Similar species of animals - have different niches, thus lessening competition for food and - living space. Thrushes hunt close to the ground; vireos and kinglets - hunt among the branches; flycatchers snap up airborne insects. The - flicker feeds upon insects, excavates nesting holes that are later - occupied by other species such as squirrels and owls, and is preyed - upon by the great horned owl; its niche is _insect exterminator / - food for carnivores / homebuilder_. The great horned owl, hunting - mammals, birds, and reptiles by night, preys on species different - from those hunted by the goshawk, and thus occupies a parallel - niche. When it dies, its remains, like those of other animals, are - decomposed and return to the soil.] - - Canopy - Great Horned Owl - Yellow-bellied Sapsucker - Understory - Flying Squirrel - Shrub Layer - Ruffed Grouse - Herb Layer - Red Squirrel - Western Toad - Forest Floor - Shorttail Weasel - Scavenging Insects - Deer Mouse - Garter Snake - Soil Layer - Ground Squirrel - Earthworm - Masked Shrew - - [Illustration: Sun, Green Plants, and Animals - - The sun is the source of energy for any plant-and-animal community. - Green plants draw nitrogen and minerals from the soil, and in a - process called photosynthesis use sunlight to convert raw materials - (carbon dioxide and water) into carbohydrates (sugar, starch, - cellulose), giving off oxygen as a by-product. Besides burning - oxygen, animals depend on plants for food. - - Green Plants, trees and shrubs, grasses and sedges, wildflowers, - ferns, mosses, algae and lichens—are fed upon by animals, which are - unable to manufacture their own food. - - The Redback Vole, like other rodents, pikas and hares, seed-eating - birds, grazing and browsing hoofed animals, and herbivorous insects, - derives its energy from the seeds and other parts of green plants - that it eats. - - The Garter Snake, feeding upon the vole, is dependent upon plants - even though it does not eat them. - - The Great Horned Owl, preying upon the garter snake, is one more - step removed from the green plants—but still dependent on them. - - Scavengers such as carrion beetles feed upon the carcass of the owl; - the remains are then attacked by Decomposers, primarily bacteria, - that break down the animal tissues into basic organic compounds. - - The Soil, enriched by the minerals and carbon and nitrogen compounds - added to it by the decomposers (and by other processes such as fire) - supports new green plant growth. - - Thus energy derived from the sun flows through the ecosystem in a - food chain. A plant-and-animal community is a complex, interlocking - web of such food chains.] - - Sun - Green Plants - Redback Vole - Garter Snake - Great Horned Owl - Scavengers, Decomposers - Soil - - [Illustration: A Pyramid of Numbers - - Necessarily, the number of plants in an ecosystem far exceeds the - number of plant eaters, and the number of prey species must exceed - the number of predators. During its lifetime, a golden eagle will - consume a vast number of lesser animals. The combined mass of prey - animals necessary to sustain an eagle greatly outweighs the eagle - itself. Ecologists refer to this proportional relationship of mass - between each link in the food chain as the _pyramid of numbers_. - - The diagram represents a numbers pyramid for the alpine zone. - Because of its limiting environment, the alpine zone supports a - lesser plant mass than the forest zone. As a result, the carrying - capacity of the alpine is less than that of the forest. - - 1 Kilo - - _Tertiary_ (third-order) _consumers_ are the predators (Golden - Eagle, Swainson’s Hawk, etc.) that feed upon other predators. - Because of the 90% loss of energy at each level of the food chain, - there will be very few hawks and eagles in comparison to the numbers - of marmots. - - 10 Kilos - - _Secondary consumers_ are the predators (weasels, shrews, - carnivorous insects and birds, etc.) that eat herbivores. The - animals at this level of the pyramid are often—though not - always—larger than the animals they feed upon. But they are much - less numerous, because it takes many prey animals to sustain one - predator. - - 100 Kilos - - _Primary consumers_ (plant eaters, or herbivores) convert plant - tissue into animal flesh. In the process about 90% of the energy - stored as plant food is lost, mostly as heat energy. In the alpine - community the herbivores include pikas, marmots, ground squirrels, - and ptarmigan, as well as herbivorous insects. - - 1,000 Kilos - - _Producers_ are the green plants at the base of the food pyramid, - manufacturing food for the animals of the alpine community. The - _biomass_ (total weight) of each level of the food chain is ten - times (more or less) the weight of the stage above it: 1,000 kilos - of green plants will produce only 100 kilos of primary consumers.] - - [Illustration: Great horned owls are the nocturnal equivalent of - Cooper’s hawks and goshawks in the low-elevation forests of the - park. Large and powerful, they are capable of taking prey as big as - skunks. This young bird, disturbed on its day roost, clacked its - bill and fluffed its feathers in a menacing manner.] - - [Illustration: The only sizable mature stand of ponderosa pine found - within the park is along the North Fork truck trail. A scattering of - old ponderosas growing at the lower end of Lake McDonald suggests - that at one time ponderosa forests were more extensive in this - region than at present.] - - [Illustration: A black bear near treelimit. Bears will eat almost - anything, from ants to carrion, grass to garbage. Color phases - include brown and blonde bears. Unlike the larger, more aggressive - grizzly, which ranges out onto the plains, black bears are strictly - forest creatures.] - - [Illustration: The water ouzel, or dipper, a creature of fast - mountain water, is admirably outfitted to cope with its demanding - environment. Stubby wings, chunky body, short tail, and oily plumage - allow it to walk under water, where it scavenges for aquatic insect - larvae and small fish. In flying up- and down-stream, ouzels never - shortcut but follow the winding streamcourse. - - As long as there is open water, the dipper suffers no hardship from - the mountain winter. Then, when the land is shut down and lakes are - frozen over, this little bird carries on in its mountain-stream - habitat, plunging into the cold water to find food, and pausing - occasionally to sing.] - - [Illustration: Ouzels construct their nests of living moss on cliff - faces or ledges where constant spray keeps the moss moist. At - fledging, the four young of this nest in Avalanche Gorge tumbled one - by one into the torrent below, to be collected by the adults in - quieter water downstream. Within a day they appeared to have - mastered the underwater gymnastics and were feeding on their own.] - - [Illustration: From their lowland wintering grounds, wapiti move up - to higher elevations in spring. Summer range in the park is - abundant, but winter range is limited; as a result, wapiti have a - tendency to increase their populations beyond the carrying capacity - of available winter range. In a severe winter many starve. But in a - balanced ecosystem such loss is not waste, for the carrion helps - sustain scavengers; it is an important initial food source for bears - emerging from hibernation.] - - [Illustration: Cedar waxwings nest in moist areas of low valleys - where fruits and berries are abundant. Although they also subsist on - insects (which they can capture on the wing), their weakness for - fruit is so pronounced that the birds will sometimes gorge - themselves until rendered incapable of flight.] - - [Illustration: The Columbian ground squirrel is found at all park - elevations, from prairie to alpine meadow. Hibernation occupies - almost three-quarters of its five-year lifespan. Unlike other park - ground squirrels, it lives in colonies. Although not as tightly - structured as a prairie dog town, the association is beneficial to - all members in that danger is readily detected.] - - [Illustration: The tundra community is encountered above Preston - Park on the Siyeh Pass trail. Mt. Reynolds, a classic example of a - horn, dominates the distant Logan Pass area.] - - [Illustration: Camas blooms in the prairie community along the Red - Eagle road. An important staple, camas bulbs were gathered as food - by Indians.] - -Conspicuous also are many insects—including grasshoppers; flies; ants, -wasps and bees; butterflies and moths; bugs; and beetles—which fulfill -important roles as herbivores, carnivores, and scavengers while also -acting as pollinators for flowering plants and providing an abundant -food source for other animals. - -Below the ground are the tunnels. Burrowing is an important means of -survival on the open prairie, and life underground is extensive. Some of -the animals are rarely seen—the northern pocket gopher, for example, -with a diet of underground insects, grubs, worms, and roots, spends most -of its life tunneling just below the surface. Others, like the badger, -leave their burrows during the day to dig for rodents. Most conspicuous -of the burrowing animals in the park’s grasslands is the Columbian -ground squirrel. Its alert upright stance has earned it the nickname -“picket pin.” When danger approaches from the air or on land, its shrill -alarm whistle passes the warning to others of its kind. - -Where prairie and forest meet, a never-ending struggle for dominion is -waged. The isolated patches of prairie that dot the North Fork Valley -near Polebridge hold the great forest of the park’s northwest region at -bay. - -This broad valley, floored with coarse glacial outwash and terraced -downward to the deep channel of the North Fork River, presents a graphic -battleground between grass and tree. Lining the upper terraces, from -which they glower down on the dry, well drained grass flats like a line -of warriors, are the Douglas-fir, western larch, and ponderosa pine. -Seedling trees continually invade the prairie. But most perish early, -their shallow roots no match for the extensive root systems of the -fast-growing, moisture-greedy grasses. If encouraged by a series of wet -summers, however, the young lodgepoles quickly gain stature. They had -made significant inroads at Big Prairie when the disastrously dry summer -of 1967 killed most of these 15-year-old pioneer trees. - -These North Fork grasslands and the immediately surrounding lodgepole -pine forests are an important spring range. Deer, wapiti, and -grizzly—and, in the wetter areas, moose—graze or browse here. And here, -low on the western slopes of the Livingston Range, are the park’s only -stands of ponderosa pine, a tree that prefers warm, dry habitats. As a -result, at low elevations it often merges with the prairie community. - -Groves of aspen colonize the eastern prairies in areas where there is -sufficient water and protection from wind. These aspen parklands are -important havens for animals. Wherever two differing communities -interact, a phenomenon known as “edge effect” occurs. Here wildlife -exists in abundance; the animals that favor forest cover mingle freely -with those that prefer open areas. Aspen groves—supporting grasses, -herbs, and shrubs beneath their thin canopies—are favored haunts for -grouse, varying hare, deer, and wapiti, all of which find among the -trees abundant food, shelter and concealment. Populations of insects, -small mammals, and birds, which are high for the same reasons, attract a -wide range of predators. - -Isolated aspen groves are characteristically dome-shaped. Because aspens -are capable of reproducing themselves vegetatively, the grove slowly -expands outward from the parent tree. As a result, most of these groves -are either exclusively male or exclusively female. - -Since quick-growing aspens provide a bountiful food source for beaver, -streams near these trees are often dammed by the rodents flooding -lowlands and creating additional habitat in the form of willow flats. -Another “edge effect” is established, attracting animals found near -water. Waterfowl, marsh birds, moose, mink, muskrat, skunks, amphibians, -and many others find such areas to their liking. - - -■ -Before the appearance of the white man, these eastern prairies were a -paradise for animals. Once, on the summit of Rising Wolf, light-headed -from the climb and the view of endless prairie, I fancied that I saw -that vast, undisturbed animal panorama spread before me. - -Principally there were the bison, darkening the uneven land. Pronghorn -bands flashed white on ridgetops, and moose moved through the long -fingers of willow that extended eastward with the rivers. Caribou and -wolves inhabited the shadows. Among vast cities of prairie dogs, swift -fox and grizzly roamed. There were the clamorings of sandhill crane, and -white clouds of trumpeter swans. - -This land, endowed with a wealth of wild grass, wore its wilderness -well. - - -The Forest - -On Gunsight Pass, the rain lancing down, I found a sharpedged rock that -split the continent in two. On both sides the rain rivulets ran down, a -fraction of an inch determining the stream’s destination: Pacific or -Atlantic. - -The Continental Divide is a mighty barrier, a line of consequence that -does more than determine watersheds. Its effect in Glacier is dramatic, -as a look at the forests will reveal. - -Obstructing the eastward flow of the moisture-laden Pacific winds, the -Divide extracts a heavy annual tribute of precipitation from the air -mass, forcing it to rise up the mountain chain, where it cools and -condenses. Chief benefactors are the low western valleys, which respond -with a lush growth of Pacific coastal-type forests. - -The eastern valleys, however, deprived of abundant annual moisture and -exposed to the wind and temperature ravages of the prairie’s continental -climate, support a dramatically different kind of forest. Here Engelmann -spruce and subalpine fir are the climax trees, contrasted with such -trees as the western redcedar and western hemlock of the mild and moist -McDonald valley. - -Elevation exerts an additional restriction on the distribution of tree -species. Since climatic conditions vary with change in elevation—lower -temperatures resulting in shorter growing seasons, and increased wind -exposure resulting in greater loss of moisture through evaporation—we -would expect to find the forest composition change as we ascend a -mountain slope. In Glacier, eastern valleys average 240 meters higher -than western, and thus even if they had more moisture they would not -sustain the redcedars and hemlocks. All plants have range limits, some -narrow, some broad; and they excel where their particular set of -preferences as to moisture, soil, sunlight, and wind exposure are best -met. On sites that do not meet their optimum requirements, they face -being crowded out by species better adapted to the prevailing -conditions. - -Physical features of the land determine vegetation also. Certain trees -prefer the moist areas along a streambed—the great black cottonwoods, -for example. And on steep hillsides, avalanches prevent the growth of -climax trees, permitting instead only shrubby, pliant -growth—mountain-ash, mountain maple, alder, menziesia. - -Forest communities are named for their dominant tree species. Thus, an -area in which Douglas-fir dominates is called a “Douglas-fir forest.” -Glacier does have forests in which Douglas-fir is the climax species; -these are chiefly dry areas, below 1,800 meters, with south and west -exposures. But we usually associate the park with its Engelmann -spruce-subalpine fir forests, found extensively between 1,200 and 2,100 -meters, and with the western redcedar-western hemlock forests in the -McDonald valley. - -Because forests mature slowly and change is usually imperceptible, we -are tempted to think of them as static and eternal. But since a forest -is a community of living things, it responds to changes in the -environment. Subtle physical or climatic changes, such as a rising or -falling water table or a slight increase or decrease in annual -precipitation, will favor some species of trees and hinder others, -eventually altering the composition of the forest. - -Other changes are more dramatic. Most notable of these is fire. - - - From Fire to Forest - -Heat lightning, glimmering soundless behind the western peaks. Then the -first low rumble. At first the flashing had been from cloud to cloud, -but now, as the storm nears, the first ground-spears appear, lighting up -the night. Here is a big storm, many-celled, engulfing more and more -territory beneath its angry bulk. Lightning dances into the dry August -forest. In their towers the lookouts stay awake. - -Close strike and a flare-up! The ridge snag burns like a Roman candle, -sending bright embers down. Valley, ridge, and peak blink on and off -with blue light as the storm roars like night-firing artillery. - -Passing overhead, the low cloud belly brings a sudden lash of rain. But -it is not enough: tomorrow will mean long hours of fire watch. - -The next day dawns clear, a morning of heavy dew. The ridge strikes did -not ignite the forest. Inspecting the storm path, aircraft and lookouts -find no evidence of fire. - -But two days later, in a morning of high wind, thin smoke plumes rise -upward. Smoldering in the thick duff of the forest floor, a lingering -hot spot explodes with the fanning wind. It quickly spreads from a -hectare to ten while the quadrants are called in and the hot-shot crews -dispatched; then to a hundred, bringing in the smoke jumpers and -mobilizing the vast fire-control network. A thousand hectares, perhaps -ten thousand might burn this week of big fires. - -In the resulting skeleton forest, the scene of devastation is almost -overpowering: life seems forevermore excluded from this blackened ruin. -But fire is nothing new to forest communities. We may think fire demonic -because it takes from our life span this block of mature forest, a sight -we will never again see in this place. But nature does not operate in -terms of human time scales. This forest is simply pushed back closer to -its starting point, to begin again its long progression toward a climax -vegetation cover. - - - Forest Succession - -Through a series of complex vegetation stages, each characterized by -different herbs, trees, and shrubs, the forest slowly returns to the -type of vegetation best suited to the physical and climatic conditions -of the site; this is called a climax community. The fact that most of -Glacier’s forests are in some stage of recovery from fire accounts in -part for the mosaic of forest cover found here. - -The forest of Huckleberry Mountain on the Camas Creek road was consumed -in the 1967 fire. By 1969, among the charred, lifeless trunks of the -former forest, lush grass and sunloving fireweed, thistle, and -paintbrush were growing. And by 1974 lodgepole pine seedlings along the -road were a meter or two high. Lodgepole is a fast-growing tree that -requires full sun to germinate. Forest fire is necessary for the -regeneration of these trees: the intense heat causes the tightly closed -cones to open, releasing the seeds that will establish the forest. So -young pines developed among fireweed, spiraea, willow, and mountain -maple shrubs. - -The lodgepole forest near the western entrance to the park has been -developing since 1929, when fire destroyed the redcedar-hemlock forest -in the area between Apgar and West Glacier. Beneath the scattered spires -of old larch that survived the burn, the lodgepoles have now grown up, -forming a canopy that shades the forest floor. Because lodgepole live -only about 80 years and will not germinate in shade, this forest will -not exist long. Shade-tolerant Douglas-fir, white pine, Engelmann spruce -and western redcedar seedlings are now taking hold. But the physical -characteristics of this area—the climate, terrain, and soil—are -ultimately most favorable for western redcedar and hemlock; and unless -other disruptions intervene, this area will eventually again become a -dense redcedar-hemlock forest. - -But this will not happen quickly. The soil after hundreds of years of -collecting debris will again become rich and moist. Young hemlocks will -germinate on and near decaying logs. When old larches, firs, and pines -fall, the slow-growing redcedars and hemlocks will take their places in -the canopy. - -Forest succession is a more complicated story than this; it is a -fascinating study involving herbs, shrubs, small and large trees, and -animal populations. From location to location it will vary; only in its -broad outlines is it predictable. It is based on the observation that, -given time, a forest—or any other plant community—will progress until it -reaches climax—that is, the stage that will perpetuate itself. - - -■ -How then are we to think about fire? Increasingly, experts are concerned -not so much with fire suppression as with fire management. For -suppression has at least three disadvantages: it allows the accumulation -of unburned fuels that can result in “fire storms” when they are finally -ignited; an undiversified climax forest is more vulnerable to disease -than is a mixed forest; and a dense forest canopy discourages shrub -growth, an important food source for deer, wapiti, moose, and smaller -animals. - -As the well-being of the deer herd depends on the predators that thin -its numbers, so the long-term well-being of the forest depends on fire -to rejuvenate it periodically. We must realize that wilderness is -identified with fire, landslide, avalanche, windfall, and flood. Nature -not only has learned to cope with these agents of change—she depends -upon them for maintaining the delicate balances between landscape and -life. There is in the business of nature, after all, more than the -pleasing of man’s eye. - - - Spruce Morning - -Of all times to get a rock in my boot! I had just started out, the -morning was still cool in this eastern valley, and the heavy pack was -not yet biting into my shoulders. Sitting down beside the trail, I -leaned the pack against the base of an old spruce and began unlacing. - -I could hear the scratching of the red squirrel descending to -investigate, but I didn’t look up until it let go with long indignant -chatter at finding its territory invaded. I plunked out the pebble and -began relacing my boot. Cautiously the squirrel came down, pausing -frequently to scold, its lower jaw quivering with rage and exposing -yellow rodent teeth. Neighboring squirrels joined in and soon the trees -danced with flicking tails. - -Down the squirrel came, almost to the ground, then raced back up the -tree, stopping at each lateral branch to deliver a vocal broadside. -Finding no danger to themselves, the other squirrels soon quit the -uproar and went about their morning business. I was beginning to suspect -that I was committing some graver offense than the mere exercise of -squatters’ rights—perhaps I threatened its cache of fir cones. Then into -the corner of my vision shot another form, streaking soundless as a -shadow; the squirrel also saw it—but too late. With a thin terrified -squeak, the rodent started to go higher; but the pine marten was above -it. The squirrel quickly reversed itself, sending bits of bark showering -down. - -As the squirrel leaped from the tree in desperation, the marten overtook -it in mid-air; they came down together. Clamping the limp creature -firmly in its jaws, the marten strode up the incline of a fallen spruce. -Before it hopped off onto a shelf of higher ground to disappear, it -looked briefly back at me. I fancied I could read, fixed in its eyes, a -certain recognition of my having distracted its prey. - -A breeze made me shiver, snapping me back from that swift vision of -luxuriant fur, that blinding grace which flashed its orange throat-patch -through the trees, and I realized I was sweating. For a moment I had -been that squirrel, eyes wide with terror, seeing fate bear down, and -powerless before the natural order of things. - -The incident got the other squirrels singing again; but the confidence -was gone, and soon it was quiet. What dreams do squirrels dream, I -wondered, looking around. I saw that place more clearly then, having -been caught between a marten and its prey. I saw each spruce: its age, -its condition, the onslaughts it had borne; the beargrass coming up in -an opening; and down the trail a meadow that was yellow, white, and red -with sulphur plant, mariposa, and Indian paintbrush. Bees, flies, -spiders, and butterflies worked that little garden tucked among the -crowding trees. Countless forms of life beneath the soil and bark, in -tunnel, crevice, hole, and pocket, working unseen to sustain their -lives, and somehow, when all were added up, maintaining the forest as -well. - -A flicker called, its loud _Klee-yer_ breaking the forest hush. Birds, -mammals, plants, insects—all hide together here, their lives so -skillfully embroidered that no loose thread exists that my mind might -grasp to unravel and understand the work. - -The forest had once been a place that obstructed my view, a great blank -to stride through, a few hours of necessary blur before the high lake or -pass was reached. Now I was quite content to remain awhile beneath these -great-boled trees. - - -■ -A forest, like the mountains themselves, supports various levels of -life. The floor and substratum are a great processing plant where -bacteria, fungi, and insects work, decomposing the plant and animal -litter, recycling dead and discarded tissue back to simpler organic -compounds, gases, and minerals, thereby providing sustenance for growing -plants. As spiders, shrews, wrens, and thrushes seem to know, there is -good hunting on the forest floor. - -Just above the forest floor is the herb layer, a seasonal layer of -growth including flowers, mushrooms, grasses, and other small plants. - -Above that grows the shrub layer, then the understory of young trees -awaiting their chance to take a place in the forest’s canopy high above. -From the swaying canopy, exposed to the full force of sun and wind, to -the dim, moist floor, the forest provides a wide range of habitat. - -Relatively few animals live in the treetops. The almost incessant motion -makes nesting too hazardous for birds. Red squirrels venture up to cut -cones in the canopy, but store their booty and make their nests farther -down. - -In the mid-range between canopy and understory, goshawks and Cooper’s -hawks nest. Woodpeckers, nuthatches, and sapsuckers forage on the tree -trunks and nest in cavities they excavate or appropriate. Red squirrels -and the nocturnal flying squirrels create a major traffic here, along -with the martens and owls that hunt them. - -The understory and shrub layers house the greatest numbers of nesting -birds. Here the effects of storm and rain are minimized and protective -cover is greatest. Vireos, thrushes, warblers, hummingbirds, bluebirds, -flycatchers, and others can be found among the tangle of this sometimes -impenetrable layer. - -The most populated area, the forest floor, supports an astonishing -abundance of organisms. Below the busy traffic of mice, shrews, and -larger animals is a bewildering array of insects and other -invertebrates. The attrition rate in the litter of the forest floor—a -continual battleground difficult to comprehend—is enormous. The smaller -the organism, the greater its numbers are likely to be. This humus-rich, -moist soil teems with bacteria, and a handful will contain surprising -numbers of small spiders, pseudo-scorpions and almost microscopic mites. - -Each year some two to three thousand kilograms, dry weight, of falling -material litter an average hectare of forest. All this plant and animal -waste—twigs, leaves, limbs, fallen trees, feathers, hair, feces, and -carcasses—is processed by the armies of decomposers that thrive on the -forest floor. With the aid of larger creatures that break up the plant -and animal tissue, most microscopic bacteria are able to decompose from -a hundred to a thousand times their own weight every day. - -Few trees die of old age in the forest. The seedling mortality rate is -necessarily high, since far greater numbers of seeds germinate each year -than can reach maturity. Of those that do, many fall victim to the -ever-present dangers of disease, insect infestation, windfall, stream -erosion, and fire. Insects alone present a formidable threat to trees, -for they have evolved every means of attack—chewing and mining leaves, -boring into twigs, eating cambium and heartwood, sucking sap, triggering -galls. If the insect world did not police itself, aided by spiders, -insectivorous birds and other animals, forests and other plantlife would -quickly fade before the chewing, boring, sucking horde. - - -■ -Through the trees the light on Citadel shows the morning slipping by. As -I start to get up I see a garter snake sliding out into the dusty trail, -seeking the sun-warmed earth. Moving slowly, alert for danger, it probes -the air frequently with its sensitive tongue. But against the -lightcolored duff its dark shape offers a fine target, begging attack. A -chipmunk, watching from a nearby lookout stump, twitches its tail -nervously over its back, curious—perhaps suspicious—at the sight of a -snake. Very slightly the snake’s head goes up, its tongue flickering. -For a few seconds reptile and rodent regard each other. Then the -chipmunk drops back soundlessly into its hollow stump, and the snake -lowers its head onto warm ground. - -Some day soon, a sparrowhawk or weasel will interrupt the snake’s -morning sun-bath. The snake will fuel bird or mammal for a time, as -mice, fledgling birds, and insects now sustain the snake. The chipmunk -too, rummaging nearby, lives in shadows of talon and tooth. - -Until that time of sharp encounter, each has its own niche, a way of -life, a shaft of sun, and food enough. - - - A Walk in the Redcedar Forest - -Climax! The word takes on a true significance here, among these -broad-based trees. When you enter this forest the road noise does not -follow far—as, when you walk into a cave and turn a corner, sound and -light are left behind. There is a surprising spaciousness, a feeling of -openness in a mature western redcedar forest. With scant understory and -the canopy so far above and everywhere complete, it seems like some -vast, high-ceilinged catacomb, pillared by the huge, shaggy-barked -cedars and the deeply scored trunks of the black cottonwoods. The floor -is strewn with fallen giants in magnificent disarray, uplifted roots -still grasping fractured rock. - -A rainy day is a good time to walk a cedar trail, when the dull light -seems to shine from the wet moss, making the underleaves of devil’s-club -and Rocky Mountain maple glow. Wind and rain, like light, penetrate with -difficulty the latticework of this canopy; thin lines of fog develop -over the bogs. The air is fresh with growing plants, snow-cold still -when the first spring flowers appear. - -Fiddleheads of unfolding lady ferns line the trail in May, pushing up -from the hub of last year’s leveled, lifeless fronds. Beds of trillium -shine their white, three-pointed flowers like flashlights in the dark -recesses. Unlike the small, hidden calypso orchid, which bears its -purple spikes and yellow throat low above the moss, the trilliums make -no secret of spring growth. They are bold, handsome plants, broad-leaved -and tall, with waxy white petals that tinge to purple in their -month-long bloom. - -Moss covers everything. Boulders are green and weightless-looking, -resilient and topped with miniature forests of cedar seedlings. Ancient -fallen trees are disguised with blankets of moss, sprouting hemlock here -and there. The rich greens that characterize Glacier’s summers seem to -begin here amid the moisture-glossed leaves of twinflower, bunchberry -and bead-lily. - -Later, the spiders will spin thousands of kilometers of gossamer -filament among the trees. The orb-weavers will hang their webs high and -low, suspended in every opening. Walking through the forest then, you -will see shafts of sunlight whirling in the higher webs until they seem -like tops set spinning among the treetrunks. - -Indianpipes, the “ghost flowers” that need no light to grow, will break -through the forest soil. Like mushrooms, with fruiting bodies that are -nourished by underground mycelia, these saprophytes absorb their -nutrients from a fungus that covers their roots. - -Receiving an average of about 18 centimeters more annual precipitation -than forests east of the Divide, Glacier’s redcedar-hemlock community -hoards its moisture. Its dense growth and the surrounding mountain walls -inhibit the circulation of drying winds. Mosses and ferns transpire -their moisture, which you can feel; place your hand close, and you will -sense a coolness like the air exuding from an ice cave. Draped from the -tree limbs are long filaments of squawhair and goatsbeard, black and -grey lichen strands that flourish in the damp air. - -Except for the black bear, few large animals inhabit the deep forest. -Grizzlies find better forage in meadows or along the forest edge. Since -shade discourages shrubby undergrowth, deer and wapiti will search -elsewhere for browse. In summer, wapiti, grizzlies, and mule deer bucks -tend to wander up into high meadows. - -Contrasted to the noisy, conspicuous birds of the prairie—meadowlarks -and bobolinks—birds of the forest seem elusive and secretive. Although -numerous, the varied thrushes, Townsend’s solitaires, and Swainson’s -thrushes are seldom seen; but when approached, they fly silently off and -are swallowed by the forest shadow. - -There seems to be serenity in a mature forest, as though the struggle -for life is somehow suspended, the needs of the animals here less -urgent, muffled. The towering redcedar forest seems to be no battlefield -at all, but rather a monument to what Earth can do. - - - The Perpendicular Night - -Behind Avalanche campground a trail leads back toward Lake McDonald -Lodge. I decided to follow it one June evening, to experience the -sensation of the deep forest changing into night. With the nearby -mountain wall intercepting the sun, dusk comes early to this valley. On -the prairie, night passes across the landscape in an even line, -forthright as a waxing tide; you can almost feel the globe in its -turning from the sun. There is reassurance in the night’s coming, its -steady purple doming over the sky. - -But here darkness seems to sprout from the earth. It collects beneath -the hemlock clumps, bridges the creekbottoms. It seems to flit from -place to place. You look about, uneasy, trying to catch it here or -there, but always miss its infiltrations. It captures the narrow -clearings when you look away; pockets of tree-darkness join together, -forcing the light upward until the tree-tops seem impossibly bright and -distant. - -Through the trees I could see a dozen fires dance in the growing shadow, -wood-smoke and camp sounds filling the air. Turning uptrail, I felt a -reluctance to leave the presence of those fires—a senseless feeling, but -strong. A growing forest-dread impelled me almost physically backward to -those circles of firelight. I felt the need to be near a fire, to be -reassured by heat and light. Fire was our greatest friend, our greatest -weapon. With it we beat the long ages of ice and held the forest gloom -away. There was no harm here, only silence; yet the longer I walked, -with beard-moss hanging down like daggers all around, the more I craved -the comradeship of fire. - - _Continued on p. 104_ - - The Vital Predator - - The merciless law of predation might at first thought seem cruel; - but the predator plays a vital part in maintaining the balance of - the biotic community. Without the controlling factor of predation, - prey species quickly enlarge their populations. If plant eaters are - not checked, the resulting excess population exceeds the carrying - capacity of the range. Food supply rapidly diminishes. In a damaged - range, competition and stress result, usually culminating in a - massive die-off through starvation and disease. - - Ironically, predators thus provide a service to their prey. First to - fall to the predator are the old, the diseased, the unwary, and the - young. By removing many young and old deer from a typical herd, - cougars lessen competition among the deer for choice range, thus - tending to keep herbivore numbers at parity with the land’s carrying - capacity. Only the strongest and wariest deer survive, ensuring that - the fittest will continue the species. When man upsets this delicate - balance—destroying predators in the hope of increasing numbers of - game animals—the result is ecological disaster. In the 1930s, in a - misguided attempt to “preserve” the whitetail deer herds of the - park’s North Fork area, many coyotes and cougars were exterminated. - In 1935 alone, 50 cougars were killed. Relieved of the pressure of - predation, the deer flourished. In a few years, however, the - normally adequate range was severely overbrowsed. Suffering also - from this imbalance were wapiti (“elk”) and moose, ungulates that - share the winter range with deer. - - Some predators are more specialized than others. The Canada lynx, - for example, has oversize feet, an adaptation that helps it move - across deep snow without breaking the surface. As a result, it is an - efficient predator of the snowshoe hare, another large-footed - animal. Relying on this adaptation, the lynx feeds almost - exclusively on snowshoe hares. Consequently, its numbers inevitably - fluctuate with the 10-year “boom and bust” cycle of the snowshoe. - - The coyote, on the other hand, is a generalized predator, exploiting - whatever prey is currently abundant. Should mice or ground squirrels - be in short supply, it will subsist on anything from grasshoppers to - berries until favored prey again becomes available. (Animals that - normally eat both plant and animal food are referred to as - omnivores.) Generalized predators are thus better equipped to - survive temporary ecological imbalances, maintaining their numbers - at relatively consistent levels from year to year. - - Carnivores all, the animals on these pages illustrate various - adaptations for capturing prey. - - [Illustration: The population of the Canada lynx, which is widely - distributed in Glacier’s coniferous forests, fluctuates in cycles. - The lynx is abundant or scarce depending on the population condition - of its chief prey, the equally cyclic snowshoe hare.] - - [Illustration: The cougar, which feeds primarily on deer, requires a - large territory. Because of its strength, stealth, and speed, - American folklore has given this wary cat a false reputation as a - man-stalker.] - - [Illustration: The red fox depends largely on a well-developed sense - of smell to locate its prey; it also relies on its keen eyesight, - speed, and agility to capture mice, hares, birds, and whatever else - it can run down or surprise.] - - [Illustration: To feed its demanding young, the Swainson’s thrush - hunts for insects along the forest floor and in the dense - underbrush. This thrush relies on its secretive behavior to protect - its nest near the ground from detection by other predators.] - - [Illustration: Armed with enlarged forelegs, the crab spider waits - on or near flowers to ambush visiting bees, flies, or other insects. - Its venom produces a quick kill, allowing it to attack insects many - times its own size.] - - [Illustration: The spotted frog is a large-mouthed predator that not - only eats water striders and other insects but also gulps down - smaller frogs and small fish.] - - Protective Coloration - - To escape extermination, each species must in some manner foil its - enemies. Protective coloration is one of the more common adaptations - helping to do this. Most animals resemble their environment to some - extent. The conspicuous markings of some, like the bitter-tasting - monarch butterfly or the striped skunk, seem to function as a - warning to prospective predators that it is in their best interest - to look elsewhere for a meal. - - Some animals, such as the white-tailed ptarmigan and the snowshoe - hare, have seasonal changes in plumage or pelage, wearing white in - winter and brown in summer. Even predators, such as longtail and - shorttail weasels, benefit from seasonal camouflage. Protective - coloration makes them less noticeable to prey species and to larger - predators. - - Many insects, too, change coloration with the season. Bright green - grasshoppers of early summer become more brown with each molt, - matching the changes in the surrounding vegetation. - - _Obliterative shading_ is especially important to animals that - frequent more than one habitat. Seen from above, turtles match their - dark background; from below, because of their lighter underbody - shading they blend into the bright skylight. - - _Disruptive coloration_ aids in breaking up an animal’s outline. - Butterflies and moths commonly have disruptive wing markings. The - distinctive shapes of eyes can be concealed. Eye coloration may - mimic body color—as in the green katydid—or the eye may continue - disruptive body markings. - - Ground-nesting birds are especially vulnerable to attack. Their eggs - tend to be heavily blotched with earthy colors, making them less - conspicuous. Chicks also carry these disruptive colorations on natal - down. - - Most mammals, with coats of brown or gray, are inconspicuous when - motionless. Deer fawns are endowed with speckled coats, mimicking - the sun-flecked forest floor; this disruptive coloration, coupled - with absence of scent and their instinctive “freezing” behavior, - makes it difficult for predators to detect them. - - The whitetail deer not only uses its white “flag” to warn others in - the herd of danger; it also allows a pursuing predator to use it as - a target. When the tail is suddenly dropped—abruptly obliterating - the bright white patch—the deer seems to disappear into its dim - surroundings. - - Since overly conspicuous animals are prone to predation, natural - selection favors development of appropriate camouflage. - - [Illustration: For such ground-dwelling birds as the white-tailed - ptarmigan, camouflage is an important survival adaptation. The - ptarmigan changes its plumage to match its surroundings: it is white - in winter, speckled in summer. Moving slowly and refraining from - flight, it is less likely than more-active birds to be detected by - sharp-eyed, motion-conscious predators.] - - [Illustration: Birds that when hatched are covered with down and are - able to move about freely are called _precocial_. They are less - dependent upon their parents than are _altricial_ young, which are - naked and helpless when they hatch; but they must rely heavily on a - resemblance to their surroundings for survival during their first - flightless weeks. This spruce grouse chick, which blends into its - sunflecked forest-floor habitat, is an example of a precocial bird.] - - [Illustration: The bold disruptive pattern of the killdeer chick’s - plumage helps this precocial bird avoid detection in its - open-prairie environment. This adaptation, coupled with the chick’s - instinct to freeze at the approach of danger, ensures that enough - young will survive to perpetuate the species.] - - _Ursus arctos horribilus_: The Vulnerable King - - At the apex of the food pyramid, this great beast is unquestionably - the king of Glacier’s biotic community. Yet the long-range future of - the grizzly bear is uncertain. With the grizzly exterminated from - most of its former range—which once extended into the midcontinent - and south into Mexico—its numbers have dwindled in proportion to its - diminished range. Present concentrations in the contiguous United - States remain in and around Yellowstone and Glacier National Parks. - Probably fewer than 200 of these magnificent creatures live in - Glacier National Park. - - Grizzlies are easily distinguished from the more common black bear. - In addition to larger size and heavier build, grizzlies have a - characteristic shoulder hump; long, conspicuous claws; and a broad, - concave face that gives them a “dished-in” appearance. Fur is - usually brown; like the fur of the black bear, however, color may - range from black to yellowish. Light tipped hairs make the fur - appear frosted, giving rise to the nickname, “silvertip.” - - Grizzlies, popularly considered arch predators, are more accurately - described as omnivores. Carrion, grasses, cow parsnip, and several - species of berries, bulbs, and tubers make up a grizzly’s diet, - along with insects, small mammals, and an occasional ungulate that - it can catch. As a result, grizzlies play several roles in the - biotic community, functioning as herbivore, scavenger, and predator. - - Ranging widely in all life zones, grizzlies follow the spring - snowmelt up to the alpine meadows, returning to lower elevations to - hibernate from November until April. One to three cubs are born in - midwinter during hibernation. Since the maternal bond lasts two - years, a sow will accept a mate only every other year. Mortality of - subadults is high, resulting principally from competition among the - bears themselves. As with most animals, range—habitat—appears to be - the limiting factor of grizzly populations. - - The grizzly is normally shy and fearful of man—but highly - unpredictable. Wounded or sick bears, sows defending cubs, young - adults, and bears that have become conditioned to human scent are - the most dangerous. As humans continue to encroach on grizzly - territory, odds of confrontation also increase. Recent fatalities - and personal injuries inflicted by grizzlies pose a vexing problem - to the National Park Service, which is charged with visitor safety - on the one hand and protection of the park’s remaining grizzly - population on the other. Continuing study of grizzly ecology and - increasingly enlightened bear management programs will, it is hoped, - allow man and bear to co-exist in a wilderness both require. - - [Illustration: Grizzlies are fond of succulent spring grasses.] - - [Illustration: Traversing all life zones in the park, the grizzly is - a true opportunist, eating anything from ants and berries to - wapiti.] - - [Illustration: Seldom will a grizzly exceed 225 kilograms in - Glacier. This is a young adult.] - - Bald Eagles and Kokanee Salmon: A Recent Gathering - - In 1916 the kokanee salmon, a small, land-locked form of the Pacific - coast species, was planted in the Flathead drainage. With the first - planting augmented by additional stockings, the fish thrived in - cold, deep Flathead Lake, and, to a lesser extent, in Lake McDonald. - The salmon fed almost exclusively on zooplankton. - - By the mid-1930s, salmon runs were becoming established. The outlet - of Lake McDonald provides an ideal spawning site for the salmon. The - fast-flowing water is clear, cold, and shallow, and the creek bed is - gravelly. - - Averaging 0.3 meters in length and weighing less than a half-kilo, - the 4-year-old adult salmon cease feeding and begin to migrate. Many - thousands swim the 100 kilometers from Flathead Lake to McDonald - Creek. Males appear in the creek first, arriving in late September, - and are soon followed by the females. - - Using her tail to dig a redd (a shallow nest depression), the female - deposits about 650 eggs. After fertilization by the male, the eggs - are covered over. The adults die within three weeks after spawning, - their bodies exhausted from the rigorous migration journey and the - weeks-long lack of sustenance. - - Egg fatalities are high, due to stream erosion and disturbance by - other spawning salmon. Hatching in late March, the fry work their - way out of the gravel and migrate downstream. - - Attracted to the 75,000-150,000 salmon concentrated in a 3-kilometer - stretch of shallow water, bald eagles begin gathering at McDonald - Creek in October. It is not known where the eagles come from or - where they go after the spawning run. Glacier has fewer than 20 - summer-resident bald eagles, and these are distributed among the - remote lakes of the North Fork area. - - In 1939, 37 bald eagles were counted along the creek. By 1969, 373 - were reported, representing approximately 10 percent of that year’s - estimated winter population for the contiguous United States. Since - 1960, the count has averaged 240 birds. (In 1977 there were 444.) - - Eagles feed by swooping down to pluck salmon from the water or by - wading out to grab a fish stranded on a shallow riffle. An eagle may - consume as many as six fish a day. Immature birds are not as adept - at catching fish and may harry adults or other immatures into - releasing their catch. - - [Illustration: From its vantage point, this mature bald eagle - examines the waters of McDonald Creek. Average weight is 5.7 - kilograms; average wingspan is 2.2 meters. Females are slightly - larger than males.] - - [Illustration: This immature bald eagle lacks the familiar white - head and tail of the adult birds. It will not acquire those markings - until it is several years old.] - - [Illustration: Breeding male and female kokanee salmon are easily - distinguishable; as spawning time approaches, they change - appearance. The dark gray backs turn red; heads become green, and - the males develop humped backs and hooked jaws.] - - [Illustration: Swooping upward with a fish, a mature eagle heads for - a convenient perch to consume its catch. A strategically located - tree may contain 30 birds.] - - A Triumph of Many Colors - - Grassland, meadow, tundra, or any other area in Glacier suitable for - plant growth and supplied with abundant sunlight produces an - extravagance of wildflowers. This display of various shapes and - colors is neither an accident nor a mere decoration of nature. Nor - would Earth’s recent explosion of mammal and bird species have been - possible without the evolution of flowering plants. - - Two hundred million years ago, early in the Age of Reptiles, - angiosperms (flowering plants) had not yet evolved. Plant - reproduction still relied on spores and cones. Then, during the - Cretaceous Period, the last sediments were being laid down in the - inland sea that covered most of Montana. (It was these sediments - that the ancient Precambrian rocks of Glacier’s mountains later - overrode, forming the Lewis Overthrust.) During this period the - evolutionary miracle occurred: flowering plants—grasses, vines, - shrubs, broadleaf trees, wildflowers—inherited the Earth. - - The timing was important. As Earth’s tropical climate gradually - changed to temperate extremes during this period, the domination of - cold-blooded dinosaurs ended and the moisture-demanding coniferous - forests that had covered the earth in green monotony began to - shrink. Angiosperms provided a solution to the ecological void: - grasses and forbs grew where trees no longer could. Most important, - relationships evolved between this new class of plants and the - relatively few species of insects then existing. - - Insects began to use the pollen of flowering plants; the - angiosperms, in turn, evolved bright petals and nectar that - exploited visiting insects for the plants’ own reproductive - purposes. This partnership allowed insects to diversify rapidly, - evolving new, specialized forms such as bees, moths, and - butterflies. As a result, predatory forms of insects and arachnids - also rapidly diversified. - - The most dramatic change, however, involved warm-blooded birds and - mammals, whose high rates of metabolism required high-energy fuels. - Unlike gymnosperm seeds, which contain no protective covering, - angiosperm seeds are surrounded by a fruit. The development of these - highly nutritious seeds, and the attendant explosion of insect - species, ensured survival of the newly evolved birds. - - As birds diversified into seed-eaters, insectivores, and carnivores, - mammals, then uncertain little ratlike creatures darting among the - feet of dinosaurs, began a rapid rise to dominance; grasslands - promoted an explosion of herbivorous and carnivorous species. - - The evolution of angiosperms, and the animal revolution it made - possible, came with amazing speed. Most significant, it was a vital - first step upon which the meteoric rise of man depended. - - [Illustration: Indian paintbrush is common at all elevations below - tundra. It may be white, yellow, orange, pink or red. The actual - flowers, inconspicuous and green, are surrounded by brilliantly - colored bracts. Semi-parasitic on other plants, paintbrush is - normally found growing in conjunction with other wildflowers; its - roots steal sustenance from neighboring plants.] - - [Illustration: Yellow stonecrop, widely distributed in forest and - scrub-forest zones, is one of the park’s few plants having succulent - leaves, an adaptation that helps it survive in such situations as - dry, rocky outcrops.] - - [Illustration: The Calypso orchid grows in the cool, shadowed forest - where light is dim. It lives in partnership with certain fungi that - exist about the orchid’s roots and seem to help nourish it.] - - [Illustration: Silky lupine, a legume, has nitrogen-fixing nodules - on its roots, thus allowing it to grow in nitrogen-poor soil. It is - widely distributed in grassland and forest communities.] - - Fire Succession: Key to Continuity - - Most of Glacier’s fires are lightning-caused. Strikes may flare up - immediately; or fires may smolder in the forest duff for days until - fanned into flame by wind. _Ground fires_ may race through the - forest understory, causing minor damage; or they may bridge the - understory and reach the canopy, thus becoming rapidly spreading - _crown fires_. Under certain conditions, uncontrollable infernos may - develop, generating terrific winds and heat. These rare - conflagrations are called _fire storms_. - - Every type of forest habitat has _climax vegetation_—trees and - shrubs that are best suited to the site and thus maintain themselves - indefinitely if not disrupted. - - After a major fire, habitat conditions are usually so altered that - the site must pass through several _seral stages_ before conditions - are such that climax vegetation can return. A _sere_ is a series of - plant communities that follow one another in orderly fashion until - climax conditions are again reached. - - [Illustration: Lightning fires occur most often during the hot, dry - weeks of late summer.] - - [Illustration: When the forest is dry, lightning often causes quick - flare-ups.] - - [Illustration: The forest may continue to burn for days after the - main conflagration has passed.] - - [Illustration: After a major fire, sun-loving grasses, shrubs, and - wildflowers quickly invade the former forest. Deer and wapiti - benefit from these new food sources.] - - [Illustration: Lodgepole pine, a pioneer species quick to take over - burned areas at lower elevations, grows rapidly. These trees are - five years old.] - - [Illustration: This is a Glacier National Park forest 80 years after - a major fire.] - -Sudden hammering made me jump. Above the forest darkness, a pileated -woodpecker leaned out from a high larch snag, braced against the trunk -by its specialized, stiff tail feathers. This was the first time I had -seen this big white-and-black bird, the “cock-of-the-woods.” There was -ample evidence of his work: the deep, oblong excavations in the trunk -and the pile of large wood chips at its base, both characteristic of -this species. Again he hammered, and I could see the chips falling. -After a little edge-work around the hole, he extracted a grub and flew -off, yammering against the advancing dark. - -Near a stream I stopped to sit down, to listen to the water and maybe -catch sight of some small animal. Across the narrow defile, from a slope -dense with young hemlock, came the buzzing note of a varied thrush. -Several notes followed, all on a different pitch, all drawn out, level -and clear; the quality was pure but songless, disjointed, deliberate, -like someone testing the reed of a strange woodwind. There seemed no -gladness in the heart of this thrush. The song was dark, haunting, -lonely. - -On the trail ahead I could make out a bird hopping rapidly along. After -passing the spot I could hear its song. There couldn’t be a hundred -meters between us, yet it seemed to be coming from a great distance. I -listened for as long as it would sing. I tried to hear it for what it -was, a male Swainson’s thrush proclaiming its territory. But the -ethereal, flute-like phrases seemed an evensong made not for man’s ears -but only for the forest itself. - -I hurried on after the bird had ceased. It was getting dark beneath the -trees, but I was beginning to be aware of creatures underfoot, the mad -dartings of shrew and vole, more imagined than seen. When a deer mouse -jumped away I got out my flashlight. Soon the beam caught a woodrat -sitting atop a fallen log. The light didn’t bother him in the least; as -I approached, he picked up his bushy tail in his forepaws. Whiskers -twitching, he looked more caricature than real. Then he bounded off the -log with graceful, arching hops, and disappeared into the night. - -Against a patch of sky that appeared in a clearing, I could make out -bats, circling and dipping like swallows. Locating a hovering moth, I -kept the light beam on it until it vanished into a furry streak of -silence. It was time to head back. - -By now it had become utterly dark within the trees, a moonless, -sightless, alien world, given over to the marble-black eyes of the small -night mammals and the creatures that hunt them. I thought of the -strange, unseen societies of the flying squirrels, the nocturnal -counterparts of red squirrels; of the great-horned owls, inspecting the -same ground the goshawks scanned during the day. Perhaps a foraging red -fox moved through the darkness nearby, or a coyote on night patrol. - -The flashlight beam probed ahead along the trail. The exposed roots were -given unnatural shading and they seemed to thicken and squirm as I -approached. On either side the tree trunks appeared to step backward -from the dim glow of the light. I felt lost in this night, thinking of -the great darkness in all the timbered ridges that ran westward from the -Divide. In this vast cathedral of crowded tree and peak, night was stood -on end, the stars shrunken to a circle overhead, as if seen from the -bottom of a well. Mouselike, shivering, insignificant in this -wilderness, I scurried back to find a fire and fill my empty senses with -its heat and snap and light, holding off the fright of night and -thinking of tomorrow’s sun. - - -Scrub-Forest - -The crowning beauty of Glacier—the high, cirqueheld meadows that scent -the wind with wildflower and waterfall—belongs to the zone of -scrub-forest. - -At Logan Pass you are introduced to the highlands. Here an exquisite -upland basin holds the Hanging Gardens, a wildflower-clothed gradient -laced with stair-step bogs and lines of wind-bent subalpine fir. In the -dawn sun, before the first engine noise, it shines unbroken, dewbright -and sagging like a spider web secured to the circle of surrounding -peaks. - -This is the region the hiker remembers best. The tall mountains wear -this zone close to the cliffs, and the trails encounter it near the -passes or follow it for long, level stretches, as along the Garden Wall. -I remember Preston Park and Fifty Mountain, the fire-touched bench of -Granite Park and the first sight of Sperry chalet, built on a brow of -rock at the upper reach of trees. But most of all I remember the -terrible waterfall that becomes Bowman Creek, the plunge of nearly a -kilometer that drains the magnificent upland bench called -Hole-in-the-Wall. - - - Hole-in-the-Wall - -September. The season is growing late, the meadow-rue dying and the -leaves of the wild strawberry failing at last. Everywhere the red -contagion of autumn surrounds the vital green. The lower valleys have -lost the whistle of ground squirrels. They sun themselves no longer -these late, mild days. Ripe, sluggish, and hawk-vulnerable, they sensed -the need of hibernation. - -It has been eight years since I last visited Hole-in-the-Wall, but I -retain its dimensions and hear its dozen waterfalls at will. Once you -have seen this basin you have a measure by which to judge the high -country and a thirst for the meadows at tree-line. - -In Glacier, treelimit ranges between 1,850 and 2,300 meters, depending -on local conditions. The upper limit of tree growth—rarely an even, -horizontal line—is generally an indistinct band running erratically -across a mountain’s face: a tension zone reflecting variations in wind -and sun exposure, degree of slope, snowpack accumulations, and the -presence of adequate soil and water. - -Subalpine fir, whitebark pine, and Engelmann spruce do not relinquish -easily their upward climb; where conditions become severe, their growth -is retarded and their stature dwarfed. Deformed and pruned by wind, -their leaders winter-killed when they outreach the protection of the -winter snowpack, trees become shrubs, forced to hug the ground. Size -belies age in these elfin forests, or krummholz, where the growing -season is painfully brief and progress is always uncertain. A twisted, -gnarled little bush, more snag than live branch, bearing a single cone -or two, may be senior by a century to the giants of its race in the -valley below, which yearly shower the ground with an abundant crop of -cones. - -This time I will come from Goathaunt, passing Lakes Janet and Francis, -reaching Brown Pass from the east, and camp in the spectacular garden -between Brown and Boulder Passes. - -Meadows and rock slides break the forest as the trail gains elevation -and distance through the valley. The spruce and fir thin out rapidly at -the valley head, the trail climbing the grassy slope to low, broad Brown -Pass. Below the pass is Thunderbird Pond, which receives the meltwater -from a glacier high on a shelf of Thunderbird Mountain and is bordered -by a low jungle of willow. In the water stands a bull moose, its heavy, -fully formed antlers ready for the season’s impending business. - -I was hoping again to see Cassin’s finches and Audubon’s warblers on the -pass; but the fir grove is quiet. Sitting down to rest and listen, I -become aware of a strange silence. No birds sing or flit among the -trees, no alarms pass back and forth among alert ground squirrels. There -is no wind—an odd condition for the Continental Divide. This place seems -to be holding its breath. High overhead, a veil of cirrus cloud arranges -long spears across the sky. - -Moving off the pass, along the dome of Mt. Chapman, I experience anew -the old excitement of this high country. Abruptly the gorge of Bowman -valley opens up, revealing the twisting blue snake of Bowman Lake far -down the narrow, cliff-imprisoned valley. Here again are the northern -titans—Numa, Peabody, Boulder, Thunderbird, and Rainbow; and Carter, -with its high glacier baring blue ice teeth to the sun. - -It is not the climb that makes your heart pound now; the trail is -suddenly narrow and cliff-defiant, cut by the plunging waters of -snowbanks far above. These are splendid peaks, unmatched in a land of -muscled, brutal earth. Even the air seems to retain the scent of glacier -work. - -At last the view of Hole-in-the-Wall, a staircase cirque excavated -between the gigantic spread ribs of Mt. Custer. The slopes of beargrass -are seed-spotted and gaunt now, the white fullness gone. Western -pasqueflowers have accomplished their magic transformation; known in -this season as old man’s beard, they nod their tufts of grizzled -seedhead silk in the wind. Red and yellow monkeyflowers bloom yet, -crowding along the many stream courses, and waterloving sedges and -mosses surround pools of collected water on the broad horseshoe tiers. - -A spur trail drops down into the campground on the last ledge. Through a -cleft in its lip plummets the gathered water of the basin. From the -valley below, the waterfall appears to be springing from a hole in the -headwall, giving this basin its name. Down, down, down, roars the water -where once a mighty glacier ground its teeth. - -I leave until later the making of camp; by now the sharp shadows of -Boulder Peak stab the valley forest and are beginning the upward assault -of Thunderbird. - -Around the basin headwalls, last winter’s snowbanks remain formidable. -Snow caves send out meltwater torrents. Glacier lilies and patches of -spring beauty line their fringes. Pasqueflowers bloom in pockets. Here, -among the asters of August, bloom also the first flowers of spring, -shooting up as the snowbanks shrink, making these spots of snow-free -ground a patchwork of May and July, August and June. The shrubs that -line the furious water are willows, still bud-swollen this tenth day of -September. The coming days will bring a sharp surprise. - -Winter will soon stop the melting of this snow. Could it be that I am -seeing the first year of a reawakening ice age? If so, each year the -snowfields would grow thicker and broader, connecting the shelves into -one ice mass again, lilies and willows entombed, the summer heat failing -to rescue them, until the ice at last began to slide, stripping the soil -and once more plucking at living rock. - -Then these dwarfed fir, which cling precariously to the cliffs and hide -behind the backs of boulders, would be in more danger than they were -from their recent antagonists. Engulfed by ice, they would know the -shearing wind no more. Their skeletons would rain down into the valley -below, signalling another long forest retreat. But they have waited out -the mountain ice before and would send their seeds again to this valley, -changed however it might be, as they have always done. - -Evening brings out two sleek mule deer does. As they graze, their large -ears stand erect, sorting out the lesser sounds from the ceaseless roar -of water. Both raise their heads and point their ears, statue straight, -at the scuttle of a porcupine. A noise among the rocks draws a backward -glance and focus of those ears. I would like the sensitivity of such -fine equipment, to hear what deer have always heard. - -Setting about the business of camp, I wonder about those animals that -watched me for a while, then moved off, having seen a tent go up before. -With the appearance of the moon the wind increases and they test the air -more often now. Do they have visions of cougar or grizzly with every -snap the wind delivers? - -In summer these high meadows see a surprising variety of animal life. -Briefly out of hibernation are marmots and the handsome golden-mantled -ground squirrels. Mice, voles, shrews, and woodrats run among the -shadows, feeding on the season’s feast of seeds and insects. A nightmare -for these are the fierce little weasels that haunt the rocks. - -Tracks of cougar and wolverine are sometimes seen, often teasingly -fresh; to glimpse either of these elusive predators is to taste the -finest wine of wilderness. - -Before the berry season, grizzlies grub the meadows for the tasty bulbs -of glacier lilies and the tubers of spring beauty; often distracted by -the scent of a ground squirrel in its burrow, they sometimes make a huge -excavation for a small reward. - -White-crowned sparrows sing in July from the low tops of the battered -trees, though their nests are on the ground below. Grey-crowned rosy -finches patrol the drier ground for seeds while water pipits hunt -insects in the wet areas. High above, a golden eagle scans the basin -again, circling slowly before following a ridge south to sight another -likely slope in its 10,000-hectare territory. - -The moon shines through the tent top. The wind, blowing more violently -now, shivers the nylon and interrupts the voice of the waterfall. I have -followed the pasqueflower run from the April prairies here to its -highest bloom near treeline. I think about the triangular seed pods of -the glacier lilies, colonies of steep-throated blue gentians, and the -season’s last glory of goldenrod. Indian paintbrush, from white to fire -red, blazes the slopes that light the fringes of sleep. - -I awake to a determined rain, the moon gone and the tent shuddering with -wind-blast. I try not to think of the steel-cold air, and slip into a -fitful sleep that seems an endless treadmill of rocky trail. - -Stiff and unrefreshed, I look out into the dawnless morning. The tip of -Thunderbird is detached from its base by grey clouds swirling at its -throat. A wave of sleet slants down, dancing on the rocks, chanting -triumph over the buried, bent, and broken flowers of yesterday. - -So I must make my escape, short of Boulder Pass. Unattainable now, -invisible above the cirque, that high pass grows in my memory. This -testament to what a glacier can do, to the struggle of trees and the -life-pioneers that invade such harsh places, is at my feet but shrouded -with snow. My hands grow stiff and numb in the blunt work of packing up. - -I had wished to see Kinnerly Peak again, rising from the western Kintla -valley, and walk along black ledges of the lava that floors the pass. -Beyond it grows a grove of subalpine larch, stately, seldom encountered, -the least common tree species in Glacier. Confined to this narrow zone -between forest and alpine, it reaches up tall and proud, impervious to -the gruelling climate that makes cowering shrubs of other trees. - -But all must wait another year, for this season comes down hard. And the -will of winter is to erase whatever summer had devised. - - -Tundra - -Porcelain-cold, the November sun dawns in the southeast sky. The ledges, -ice-encrusted, layered with sleet from a recent squall, whistle the cold -morning wind aside. Rattling down, a slide of rock plunges off the final -ledge, seconds passing before the hollow sounds of impact clatter back. -Like an apparition of winter itself, white beard bent sideways by the -wind, a mountain goat steps to the precipice edge. Looking out across -the vast white void, its long belly hair and pantaloons streaming with -the ceaseless wind, this strange animal, product of some unfathomable -ingenuity, hesitates but a moment; dropping down from step to invisible -step along the sheer rock face, fracturing the ice glaze as it goes, it -turns a wall and disappears. A nimble, eight-months-old kid follows. - -Blinking and twisting in the dull light, the shower of shattered ice -clinks softly downward against rock, fading away like the short summers -of this place. - -But while the wind chants winter, life has made a passage here, and also -waits, hidden in seed and root and den. - - -■ -The nanny and her kid have bedded down now, looking across the deep, -snowy basin below. Their ledge shines with the first spear of sunlight. - -Far below the pass that connects Mount Siyeh to the snow-giants Matahpi -and Going-to-the-sun, three male white-tailed ptarmigan emerge from -their night’s huddle within a snowbank and step out to peck at an -exposed mat of willow. Ptarmigan, the only birds on the winter tundra, -wear white plumage in this season, helping to camouflage them in the -snow, just as their mottled brown summer plumage makes them difficult to -detect among bare rocks. There are few predators here to hunt them now, -but they move with habitual slowness; quick movement can be fatal when -summer brings numerous eyes to scan the slopes. With legs and feet -heavily feathered and sharp claws to scratch for food beneath the snow, -the ptarmigan live at truce with winter. When blizzards rage between the -peaks, they nestle together in snow dens, beyond the reach of the winds. -Ptarmigan hens winter lower in taller willow thickets, but the males -prefer to take their winter as high as possible. - -Now they crouch behind the wind-deflecting rocks, dozing in the meager -warmth of the morning sun. - -Near the snowless summit crags, a flash of brown fur zigzags among the -rocks. That would be a pika. Only for a moment does it show itself, so -quickly does it move. - -Also called the rock rabbit, the diminutive pika belongs to the order of -hares and rabbits. Resembling a small guinea pig, this sturdy creature -spurns hibernation as a way to beat the challenge of winter. Instead, it -spends the summer laying in a store of hay for the lean season, -spreading cut grass to cure upon the rocks and tending its “haystacks,” -on which its survival hangs. - -Winter is a great peril to small mammals. Their small bodies, because of -a large surface area in relation to volume, retain heat poorly, and -their high metabolic fires consume calories quickly. Great amounts of -energy are required to sustain an active animal in rough terrain, -placing further demands on the animal’s capacity to survive the cold. -The pika may need to stack as much as 25 kilos of hay; to keep its -furnace burning during winter it will have to fuel its stomach almost -hourly. - -Small animals of cold climates often show distinctive body adaptations. -On the pika the small, rounded ears lie flat along the head, the tail is -inconspicuous, the legs are short; heat loss from exposed surfaces is -thus reduced. Fur insulates the soles of the pika’s feet while at the -same time providing good traction on steep rock faces. - -Hidden below these rocks are the hibernating marmots and the sleeping -ground squirrels. Beneath the snow the mice, shrews, and pocket gophers -struggle on with their lives. But above ground, directly confronting -this arctic climate, are the pika, the ptarmigan, and the mountain goat. - -A triumph of adaptation, the mountain goat faces the winter day without -benefit of either the pika’s den or the ptarmigan’s snow roost. - -The nanny and kid descend from their ledge to search out browse at -treeline with other members of a loose band—yearlings, young males, -other nannies with kids. At the fringes of the band a solitary adult -billy only grudgingly associates with other members of his kind; for -this is the season of rut. - -Not really goats at all, these relatives of the European mountaineering -chamois are insulated from the wind by coats of long, hollow-haired fur -overlying woolly underfur. They are stocky, stiff-legged, and -deliberate, able to negotiate the walls and pinnacles with their -superbly adapted hoofs. The unique design of these hoofs gives the -animal great traction and stability on precarious crags. Opening towards -the front, the cleft between the two hoofs spreads each outward as the -animal descends a slope, helping to grip the rocky surface. In addition, -the large, rough, and pliant sole of each foot conforms to the bare -rock, increasing traction. - -There is little need for the goat to leave its steep sanctuaries; it can -subsist on lichens and mosses if browse is not available. It depends on -the inaccessibility of the cliffs for its security. Accidents, -avalanches, and rockfall are greater enemies than predators. Golden -eagles sometimes attempt to knock newborn kids from ledges and a young -goat quickly retreats under its nanny when an eagle soars by. With the -protection of sharp spike horns and a terrifying terrain, adult goats -seldom fall victim to cougar or grizzly. - -It will be a long time before the snow releases this land and wapiti, -bighorn, grizzly, and cougar wander back into these high basins. In this -winter minimum of life, the spring songs of rosy finches, water pipits -and white-crowned sparrows seem an impossible extravagance. - - -■ -I am drawn to the spring tundra—to the vigor and tenacity of its sparse -life—where survival itself seems ceremony enough. But it is a strange -world, where a man is out of perspective. Here the plant cover is -carpet-high, and distance, for the lack of trees, tricks the eye. Here -the wind, snow, and sun quickly burn skin, and the intense light, -reflected from snowbanks, stabs at the eyes. Almost instantly, a -sandwich is sucked dry of its moisture. The desiccating wind probes the -ears until it seems at last to pierce your brain. Except for fearful -mountain walls the only shadow is your own. Animals seem somehow remote -and unknowable, as if seen through glass. A day on the tundra and you -feel the want of a company of trees. - -Yet once exposed, you acquire a craving for the look of tundra. Nowhere -else is there such an impatience for spring—the flowers rush into bloom; -the male water pipit soars, its skylark song crystal sharp in the thin -air. The nesting birds are restless, for sun-days and warm days are few, -precious, and quickly spent. Insects and spiders abound—flying about the -peaks or crawling among the rocks. - -Summer brings bands of bighorn rams up from the valley to explore the -highest meadows. Though not so sure-footed as the goats, they too have -hoofs adapted to climbing steep faces, and they walk the slopes not far -below the goats. - -Marmots, which whistle sharply when threatened, spend their days -sunbathing and grazing; they must fill out their now loose-hanging fur -coats with life-sustaining fat for the coming winter. - -Alpine animals are blessed with mobility and can choose their weathers, -retreating to burrow, den, or rock-harbor to escape the worst fury of -storms. But what about the plants, rooted forever in one spot, assaulted -by an untempered sun and a drying wind, and facing the almost daily -threat of freeze and storm? - -Alpine plants, through their design and growing habits, have adapted -themselves to the rigorous demands of this climate in many ways. Most -plants are perennial: there just aren’t enough days or nutrients -available for the growing of entire plants each year from seed. And they -have the ability to grow and carry on photosynthesis at temperatures -just above freezing, thus extending their season. In this zone, -temperatures are rarely above 15° C; the mean summer temperature is -about 10° C. But a flower such as the alpine buttercup, which is found -at treeline or above, can grow through several centimeters of snow; heat -given off during the plant’s respiration will create an opening through -which it can emerge. - -Plants have various adaptations to meet the demands of the alpine -environment. Yellow stonecrop, not restricted to this zone, is -nevertheless able to survive here because of its fleshy succulence and a -waxy covering that prevents water loss. On some plants, protective hairs -covering leaves and stems help retard the burning effects of wind and -sun. Often this pubescent foliage looks more grey than green, for the -soft hairs mute the color. - -Cushion growth is another alpine adaptation. The moss campion cushion, -covered with delicate pink flowers, grows to about one-third of a meter -across and only 3 to 5 centimeters high. Spreading out close to the -ground, the plant avoids the major violence of the wind and hoards -moisture like a sponge. - -The dryad, growing abundantly on the windy sweep of Siyeh Pass, shows -alpine adaptations in several ways. The energy of the mature plant is -channeled primarily into reproduction: its large flower, supported by a -short stem, matures quickly; and it produces many seeds, ensuring -germination of a few. An evergreen, it begins to synthesize water and -carbon dioxide into food as soon as the snow is gone; and its rolled -leaves prevent rapid evaporation. It grows as a low and woody mat that -year by year extends itself through the production of new shoots that -carpet the rock. Mat growth has the advantage of retaining dead plant -material and capturing wind-blown grains of soil, allowing the plant -slowly to enlarge its soil base. - -Compared to the forest, the heartbeat of the tundra is painfully slow. -Here a plant may grow for a quarter of a century before it has acquired -the reserves necessary for flowering. Contrasted with the progress on -the tundra, forest succession races by with dizzying speed. Yet -imperceptible as the change may be the alpine plant community also -passes from pioneer to climax. - -Beyond the limit of other plants, lichens thrive, encrusting rocks with -their rainbow colors. A lichen is actually a primitive and highly -successful association between a fungus and an alga, working together -for mutual benefit. The fungus protects the delicate alga, trapping and -holding moisture; the green alga, in turn, produces enough food to -sustain the needs of the fungus. - -Generating rock-disintegrating acids that help secure this partnership -to the rock, lichens, along with physical weathering, help break down -the rocks into soil particles. Collected in pockets by run-off or wind, -rudimentary soil is slowly invaded by cushion plants. After centuries of -colonization by these, while the meager soil is deepened and enriched -and moisture retention is increased, other plants move in, climaxing at -last in hardy grasses and sedges. As in the forest, pioneer species -change the environment to their detriment, creating a habitat better -suited to other species. - -Although it will progress with geologic slowness, the rocky ground of -Siyeh Pass—its plant cover presently scant and wind-rowed by frost-heave -and relentless wind—will in time develop grasses and sedges, the climax -vegetation of the alpine meadows. - - -■ -Simplicity rules the alpine zone. Here life is reduced to bare -essentials. Chief controlling force is climate; but the plants and -animals that live here are well adapted. Compared to the lower realms, -where both competition and predation are fierce, life here looks secure. - -There is a penalty to simplicity. In the lowland, the long food chains -and diversity of species, the long growing season, and the abundant food -supply give the forest an adjustment mechanism and healing power not -found on the critically balanced tundra. The greater the variety in a -plant and animal community, the greater the stability. So in the alpine -world there exists a paradox: the most durable life forms constitute the -most fragile community. - - -The Water Communities - -Snowfields begin again their summer-long melt. The alpine stream, vocal -again, collects its water from a thousand places. Miniature gorges drain -the meadow, gurgling with the sparkle and rush of meltwater in the -lengthening spring days. - -Gathering volume, the stream seems to hurry faster; at the first rock -staircase, it begins to sing. I follow the gully downward, drawn like -the water. There is excitement in the growing dash and roar, a wind-gust -sweeping spray into the air. A rainbow appears, holding steady to the -swirling cloud of spray, then doubles and abruptly disappears. - -At the first great plunge the water lunges outward over the lip. Like -glass at shattering, long shards lance out. But the wind feathers the -sharp edges as they fall. - -The close thunder of a waterfall beats at your head, and your mind must -shout to think. Here is water, a most amazing and most important -substance. Perhaps some of this same water was once part of the ancient -sea in which was laid down the mudstone of this ledge; was once drunk by -dinosaurs; has coursed the globe countless times; and has flowed in this -very stream before. In solid, liquid, or gaseous form, it goes through -its own cycle. Together with sunlight, water makes possible and -maintains all life on Earth. - - - Ouzel Music - -A glacier might cling to a winter snow a hundred years and turn it to -ice, a blue tool to rasp and pluck at rocks, before letting it go. -Lingering summer snowfields might delay its passage for a time. But the -water always wins at last, becoming, in one decisive instant, liquid -again, and beginning its long journey to the sea. Plants and dry air -will intercept some of its molecules, sending them back into the -atmosphere to bloom as fog and cloud; but as rain, snow, or dew, these -are soon commissioned to the land again. - -Water is so familiar to us that we seldom think about it. We know that -fish swim in the lower lakes, and we are vaguely aware of the -bewildering assortment of life-forms abounding in a pond. But life -begins in the streams. - -Even cups of cold meltwaters, scooped out of a rivulet only a few meters -away from its snowbank source, contain some life. Snow algae, which grow -on the snowbank surface, often sufficiently dense to give the snow a -distinctive red complexion, are released into the meltwater. In summer, -small invertebrate life can be discovered in the standing pools of even -the highest cirque. - -But conditions are not good for the development of complete aquatic food -chains in the streams and lakes of higher elevations. Alpine lakes, or -tarns, support little visible life. Often flanked by high ridges and -peaks, many tarns receive scant direct sunlight during the day. Since -these lakes occupy basins that capture tremendous amounts of snowfall, -the snowbanks persist in the mountain shadows, and summer makes little -progress in warming the water. Iceberg Lake, for example, is seldom free -of floating ice, and its temperature never rises above 4° C in summer, -even at the surface. - -Moving out of the cirque lakes, water is soon churning again, dashing -downward many hundreds of meters to the valleys below, in rapids, -cascades, and breathless waterfalls. Not surprisingly, few plants and -animals are adapted to life in fast-moving water. - -Algae can be found covering streambed rocks and stranded, water-polished -tree trunks. Securely attached by holdfasts, these small plant forms -survive the rigorous stream flow that would destroy the larger vascular -plants. Several species exist, from microscopic forms to branched -filamentous algae whose long hairlike strands wave in the current. - -A surprising number of insects live on the stream bottom, finding a -measure of protection from the current in the jumble of rocks. -Underwater beetles live under the gravel or among the debris at the -stream-edge, or cling to stones and sticks. Scurrying and creeping among -the rock-crannies are the larvae of stoneflies, mayflies, and -caddisflies. These and the small fish that venture up from lower lakes -are the food of the water ouzel, a creature that loves the places where -the waters thunder. - - -■ -The noise of the water is overpowering. A slip into this boiling rage -would mean quick death. Looking 10 meters across the dim, mist-slippery, -water-scoured canyon, I see a young water ouzel peering out of its -unique nest, on the lookout for its parents. Clouds of spray keep the -nest of living moss continually wet; but this bird is waterproofed with -an oily plumage and keeps its vigil at the nest opening. Peering into -the torrent below, then upstream and downstream, it awaits patiently the -delivery of the next meal. - -With the approach of one of the adults, three other heads crowd the -opening, begging yellow mouths agape. Flying low, the ouzel parent zeros -through the heavy spray, alighting on a slippery boulder below the nest -ledge. Preparing to fly up to the nest with its load of insect larvae, -the ouzel spots me across the water. At its sharp _jigic, jigic_ alarm, -the bills of the young snap instantly shut. Nervously the bird regards -my close presence, dipping its entire body rapidly up and down, as if -keeping time with the surging torrent. - -Discovering no danger, the dusky blue-grey bird bobs more slowly. The -other adult, returning from an upstream forage, alights on the same -rock, occasioning a new outcry from the fledglings. Each in turn, the -parent birds fly up to feed their young, beating their wings to maintain -their position at the perchless nest. Not pausing to regard me further, -they split the stream between them again, one flying upstream and one -down, to continue the hunt. Blinking and shaking the collected mist from -its bill, the single young sentry renews its watch. - - - In Shallow Waters - -Life abounds in the shallow lakes and ponds. Calm, protected John’s Lake -offers a fine example of how a complex aquatic plant-and-animal -community can exist in balance in a confined space. The water teems with -the microscopic algae, protozoans, and rotifers that sustain the barely -visible zooplankton. Dancing, flitting, hopping, and swaying through the -water, these zooplankton in turn support the larger plankton-eating -animals. - -Dragonflies and damselflies shoot past, crackling their wings, and perch -in the bog grass. Looking into the shallow water, you will see a wealth -of small animal life. A spotted frog swims into view, floating to the -surface beside a lily pad so that its eyes protrude above the water. - -The ribbonlike form of a leech swims across the bottom toward deeper -water. Looking closer, you see that the water swarms with bizarre -shapes—water boatmen propelling themselves with oarlike appendages, a -gliding mayfly nymph, then a predacious diving beetle surfacing, -grasping a bubble of air beneath its shiny brown wing plates and -disappearing downward again—the bubble’s edge shining silver—into the -brown bottom debris. Suddenly a whirligig beetle sets the surface to -spinning, wrinkling the view below. - -Everywhere in the water there is animal life, forms that are attached, -free-swimming, crawling on the bottom, and clinging to or swimming on -the surface film. The gray, slimy encrustation on a sunken log looks -like a covering of lichen but is really a freshwater sponge, a colonial -animal that feeds by filtering minute plankton from the water. Another -attached creature is the barely visible hydra; this twig-shaped -predator, related to marine jellyfish, captures water fleas and other -small animals in its several poisonous tentacles. - -Water beetles, backswimmers, water boatmen, and many other creatures -move about more or less freely in the water, propelling themselves along -with jerky movements. Suspended between surface and bottom are the -zooplankton, the tiny water fleas, cyclops, daphnia, and others, which -feed by filtering minute algae. On the bottom and below live scavenging -worms. Water striders skate on the surface film. - -Along the shore, frogs, salamanders, garter snakes, and water shrews are -hunting. Dabbling and diving ducks patrol about, tipping or submerging -for the bottom plants. Moose tracks circle the muddy shore. Because it -produces vegetation abundantly, John’s Lake sustains a great diversity -of animal life. - - - Beaver Ponds - -Fully 10 percent of all the present meadow area in the Rocky Mountains -is estimated to have been created by beaver, the only animal besides man -that engineers extensive changes in the environment to suit its own -needs. - -When beavers dam a stream, they set in motion another form of -succession. If the resulting backwater floods a forest area, the trees -are soon killed, creating a broad opening in the forest canopy. -Water-associated plants and shrubs quickly invade the pond and -shoreline, creating favorable habitat for waterfowl, moose, blackbirds, -amphibians, wading birds, warblers, marsh hawks, and a score of other -animals. - -After many years the water becomes shallow, filling in with silt and -plant debris. When the beavers abandon the site, the dam may rupture for -lack of maintenance and the pond will rapidly drain. Or it may continue -to hold, delaying for several more years its slow conversion to meadow. -Stimulated by the nutrient-rich mud, the water grasses, sedges, and -shrubs finally choke the water with their accumulating debris, -transforming the area into a bog. - -Gradually the ground firms as more humus is created and more silt is -trapped. The area becomes meadow, supporting grasses, sedges, and other -flowering plants. Trees begin to reinvade the drier ground, and -eventually the meadow reverts to forest. Centuries may be required to -see this cycle through, from forest to pond, to bog, to meadow, to -forest again. At each stage many of the animal inhabitants change: the -song of the western robin and the chatter of a red squirrel in the -original, pre-beaver forest give way to the croak of a heron; the heron -is replaced by the insect-and-berry-eating cedar waxwing; the waxwing is -followed by the tree-dwelling western robin and red squirrel. - - - Lakes Cold and Deep - -Seeming to skate on its own reflection, a spotted sandpiper comes in low -over the quiet water, wingtips almost touching the surface of the lake. -It alights at the shore and folds its wings. Amid the rounded rocks, -this plain but elegant little shorebird is all but swallowed up. -Teetering constantly on long legs, it sets off along the water’s edge, -pecking here and there, coming closer and closer, never forgetting to -stop and curtsy, as if acknowledging, while hurrying offstage, the -applause of an audience. - -As it draws near, several water striders skate away from the shore. A -stonefly, scuttling between two rocks, is deftly speared. So large a -morsel makes the bird pause and rough its feathers, then scamper into -the water to take a drink. Teetering again, it passes in front of me and -continues down the shore, where I soon lose sight of it rounding a rocky -point. - -I am sitting at the foot of Lake McDonald, watching the darkness gather -over the valley, seeing the last light slide upward to the tips of the -distant mountains. As daylight dissolves, this long fleet of familiar -peaks seems almost to glide toward darkness, slow and silent as sailing -ships. - -The sheet of motionless water stretches many kilometers away between -tree-covered moraines. The water is deep and cold. No emergent plants -line the barren shore. It would seem that no life, except for the single -gull that rests on the water far away, exists in this nearly -thousand-meter-high lake. - - -■ -Considering the great volume of Glacier’s large, deep lakes, the life -they support is indeed meager. A large part of the reason lies with the -nature of their shores, where almost no plants grow. A combination of -factors prevents the development of a lush shoreline growth. - -Contoured like bathtubs, these steep-sided lakes exhibit narrow or -non-existent shoreline shallows, which are vital for the production of -rooted plants. Strong wave action and extensive seasonal fluctuations in -the level of these natural reservoirs prevent the development of -emergent water plants in locations where they might otherwise be -expected. - -Since sunlight cannot penetrate to the bottom of these deep lakes, they -are deprived of bottom-anchored plants in midlake as well. As a result, -herbivorous animal life must depend almost wholly on algal growth. Wave -action inhibits the spread of free-floating algae by washing much of it -onto the shore. Deep lakes are also low in available oxygen, preventing -the development of bottom decomposers, which would rapidly release -nutrients as they break down the accumulating debris washed into the -lake. Without a steady supply of nutrients, plant growth is retarded. - -Since the food chain depends upon green plants, the ability of a lake to -support higher animals such as fish depends upon its ability first to -produce adequate plant growth. The production of one kilo of trout -requires that a lake produce about 1,000 kilos of plants to support 100 -kilos of herbivorous invertebrates, which are eaten by 10 kilos of -carnivorous insects, on which the trout feed. - -Compared to smaller shallow lakes, which teem with visible life, cold, -deep, nutrient-poor lakes such as McDonald appear to be watery deserts. -Yet because of their great volume—Lake McDonald contains 5 or 6 cubic -kilometers of water—these large lakes do sustain significant numbers of -fish. Of the 22 kinds of fishes found within the park, most are -coldwater species. Trout, whitefish, grayling, suckers, minnows, and -carp fill the roles of herbivore, carnivore, and scavenger. Agile, -highly mobile, and acutely sensitive, fish represent the most successful -total adaptation to the aquatic environment. - -Through the stocking of nonnative species, including plantings in -formerly fish-free lakes, the natural aquatic communities of many of -Glacier’s lakes and streams have been permanently modified. - -Aquatic food chains are not confined to the water. Ospreys, ducks, -mergansers, otter, mink, and many other semi-aquatic or terrestrial -birds and mammals utilize the plants and animals of the water. In fall, -a remarkable spectacle occurs along the outlet of Lake McDonald. -Attracted to the kokanee salmon concentrations, which run from Flathead -Lake to spawn and die in these clear, shallow waters, bald eagles -collect to exploit the vulnerable fish. In 1977, 444 eagles were counted -in one census. This food resource is also exploited by grizzlies, -coyotes, skunks, gulls, loons, and other animals. On occasion, even -white-tail deer have been observed swallowing salmon! - - [Illustration: Sunset] - - - - - Shooting Stars - - -This park is very special. The people who know it well feel proprietary -toward its mountains, scattered lakes, and glaciers. Perhaps it is the -arrangement of the land, an unsurpassed concentration of American -wilderness. Time and again I have thought, as I regarded some aspect of -this country, _yes, this is exactly right_—almost, it would seem, as if -some magic existed that could translate thought and emotion into rock -and bark. - -Glacier remains largely unexploited, bearing still the aspect of the -Earth the Indians knew for 500 generations—a land where it is yet -possible to feel a sense of discovery, sense that a single man matters. -On too many mountains, man has tarnished whatever he has touched; but -here the land has shed, as a fir sloughs snow, a long succession of -traders, trappers, explorers, hunters, surveyors, prospectors, loggers, -settlers, and tourists. - -You may walk the same trail a dozen times and not tire of the view. I -have given up wondering why. I know only that these are mountains a man -might grow old with, and that mountain-fever never diminishes but only -changes its look, as a forest does over many years. - -Repeatedly I have noticed that this park creates an instant bond between -strangers. A certain pause intrudes at the first mention of Glacier -National Park, and a look of distance comes, as Red Eagle becomes real -again, or the wind at Firebrand is remembered, or the flowers of -Fifty-Mountain converge once more upon the senses. - -Never are we quenched. If a goshawk rushes past, straining upward with -its squirming load of ground squirrel, forever afterward our blood -demands more. The sight of a wolverine running is not enough. Nor the -magnificent assemblage of bald eagles feasting on November salmon. More -days of this: mountain goats leaping impossible ledges, wave tracks from -a beaver reaching out on dawn water. There are messages here, loud as -kingfishers. The land has languages, stories to tell. - -But in wilderness there is no moral, save that it must continue. For all -our probings and plottings we discover no adequate interpretation of the -forces we find swirling about us. A larch you must touch to know; your -neck must feel the ache of too much looking up. Watch its treepoint -pirouette. Then, looking back at the world level, you will find that you -have lost all answers. We have learned the art of building bridges, -cataloging plants, predicting what a shrew might do. Of the essential -mystery, we know nothing. - -For nature assigns no “roles” to its creatures; there is no “reason” for -a forest fire, which burns mightily but with no intent. Life’s only -“purpose” is the feeding of life, and the beauty we see therein is but -its lack of guarantee: for the chipmunk and the weasel, and the man who -measures his life to theirs, no assurance of long days and tempered -seasons, abundant seeds, ample meat. In wilderness there is mystery yet, -unsimplified, not reduced, resplendent and immense. - -Whatever the conclusion of this planet, however many the acts to follow -in this consuming drama—mountains coming up, mountains going down, -forests, lakes, and seas skimming past like wind-driven scud clouds -before a storm—at least in the scant shadow of this present age there is -an achievement of sorts. For now, with this creature man, such things as -mountains can be loved. And men have memories to fill. - -Tomorrow I will look for shooting stars—purple spring flowers that point -their fire down, always down toward the center of the Earth, as if to -give in their brief term beneath the sun a tribute to this most -excellent mystery. - -Today I can say nothing more, neck-sore now from looking at larchtops -swaying with the wind of this splendid morning. - - [Illustration: Shooting star.] - - [Illustration: Mountain goats.] - - - - - Appendix - - -Mammals of Glacier National Park - -Distribution information was obtained from _Meet the Mammals of -Waterton-Glacier International Peace Park_, by Robert C. Gildart (see -Reading List). Nomenclature follows, for the most part, _a Field Guide -to Mammals_, by William H. Burt and Richard P. Grossenheider. - - Key to symbols: - E—occurs east of Continental Divide (spruce-fir forest; aspen; - bunchgrass meadows) - W—occurs west of Continental Divide - (redcedar-hemlock-lodgepole-fir-larch forest; some meadows) - A—occurs in alpine areas (above upper edge of continuous forest) - R—rare in Glacier National Park - - Shrews - Masked shrew, _Sorex cinereus_ - E, W, coniferous forests, meadows, pond and stream edges - Vagrant shrew, _Sorex vagrans_ - E, W, A, moist forests and grasslands, marsh and stream edges - Northern water shrew, _Sorex palustris_ - E, W, stream edges - - Bats - Little brown myotis, _Myotis lucifugus_ - E, W, coniferous forests, often around buildings, caves; nocturnal - Long-eared myotis, _Myotis evotis_ - E, W, A, R, coniferous forests, meadows; nocturnal - Long-legged myotis, _Myotis volans_ - E, W, A, coniferous forests, meadows; nocturnal - Big brown bat, _Eptesicus fuscus_ - E, W, coniferous forests; often around buildings, caves; nocturnal - Silver-haired bat, _Lasionycteris noctivagans_ - E, W, coniferous forests; meadows; nocturnal - Hoary bat, _Lasiurus cinereus_ - E, W, coniferous forests; mostly nocturnal - - [Illustration: Cougar] - - Cats - Bobcat, _Lynx rufus_ - E, open forests, brushy areas - Lynx, _Lynx canadensis_ - E, W, coniferous forests - Cougar, _Felis concolor_ - E, W, coniferous forests - - Raccoon, bears - Raccoon, _Procyon lotor_ - E, W, R, open forests, stream bottoms - Black bear, _Ursus americanus_ - E, W, A, forests, slide areas, alpine meadows - Grizzly, _Ursus arctos_ - E, W, A, forests, slide areas, alpine meadows - - [Illustration: Coyote] - - Canines - Red Fox, _Vulpes vulpes_ - E, grasslands, open forest - Coyote, _Canis latrans_ - E, W, A, forests, grasslands - Gray wolf, _Canis lupus_ - E, W, R, coniferous forests - - [Illustration: Wolverine] - - [Illustration: Longtail weasel] - - Mustelids - Striped skunk, _Mephitis mephitis_ - E, W, open forests, grasslands - Badger, _Taxidea taxus_ - E, W, grasslands - River otter, _Lutra canadensis_ - E, W, R, rivers, lakes - Wolverine, _Gulo gulo_ - E, W, A, coniferous forests, alpine meadows - Least weasel, _Mustela rixosa_ - E, R, open forests, grasslands - Shorttail weasel, _Mustela erminea_ - E, W, A, coniferous forests, meadows - Longtail weasel, _Mustela frenata_ - E, W, A, open forests, meadows - Mink, _Mustela vison_ - E, W, creek and lake edges - Marten, _Martes americana_ - E, W, A, coniferous forests - Fisher, _Martes pennanti_ - E, W, R, coniferous forests - - Lagomorphs - Pika, _Ochotona princeps_ - E, W, A, rockslides - Snowshoe hare, _Lepus americanus_ - E, W, coniferous forests - Whitetail jackrabbit, _Lepus townsendii_ - E, W, R, grasslands - - Squirrels - Hoary marmot, _Marmota caligata_ - E, W, A, rocky areas, alpine meadows - Richardson ground squirrel, _Spermophilus richardsonii_ - E, R, grasslands - Columbian ground squirrel, _Citellus columbianus_ - E, W, A, open woodlands, grasslands, alpine meadows - Thirteen-lined ground squirrel, _Spermophilus tridecemlineatus_ - E, R, grasslands - Golden-mantled squirrel, _Spermophilus lateralis_ - E, W, A, high, open forests; rocky areas - Least chipmunk, _Eutamias minimus_ - E, W, A, high, open forests; brushy, rocky areas; alpine meadows - Yellow pine chipmunk, _Eutamias amoenus_ - E, W, open forests; brushy, rocky areas - Redtail chipmunk, _Eutamias ruficaudus_ - E, W, open forests; brushy, rocky areas - Red squirrel, _Tamiasciurus hudsonicus_ - E, W, coniferous forests - Northern flying squirrel, _Glaucomys sabrinus_ - E, W, coniferous forests; nocturnal - - Pocket gophers - Northern pocket gopher, _Thomomys talpoides_ - E, W, A, meadows - - [Illustration: Beaver] - - Beaver - Beaver, _Castor canadensis_ - E, W, streams, lakes - - Voles and kin - Deer mouse, _Peromyscus maniculatus_ - E, W, A, forests, grasslands, alpine meadows - Bushytail woodrat, _Neotoma cinerea_ - E, W, A, rocky areas, old buildings - Northern bog lemming, _Synaptomys borealis_ - W, R, coniferous forests - Mountain phenacomys, _Phenacomys intermedius_ - E, W, A, coniferous forests, alpine meadows - Boreal redback vole, _Clethrionomys gapperi_ - E, W, coniferous forests - Meadow vole, _Microtus pennsylvanicus_ - E, W, open forests, meadows; along streams; marshy areas - Longtail vole, _Microtus longicaudus_ - E, W, coniferous forests, grasslands - Water vole, _Arvicola richardsoni_ - E, W, A, high-elevation stream and lake edges - Muskrat, _Ondatra zibethica_ - W, streams, lakes, marshy areas - Western jumping mouse, _Zapus princeps_ - E, W, A, grasslands, alpine meadows - - Deer - Wapiti (American elk), _Cervus canadensis_ - E, W, A, open forests, meadows - Mule deer, _Odocoileus hemionus_ - E, W, A, open forests, meadows, often at high elevations - Whitetail deer, _Odocoileus virginianus_ - E, W, coniferous forests, meadows, creek and river bottoms - Moose, _Alces alces_ - E, W, coniferous forests, lakes, slow streams, marshy areas - - [Illustration: Mountain goat] - - Bovids - Mountain goat, _Oreamnos americanus_ - E, W, A, high peaks and meadows - Bighorn, _Ovis canadensis_ - E, A, open mountainous areas - - -Reptiles and Amphibians of Glacier National Park - -Note: This check list is based upon actual specimens in the Park and -other collections, according to Dr. Royal Brunson, Montana State -University. - - Reptiles - Great Basin Garter Snake, _Thamnophis elegans vagrans_ - A large garter snake of mountainous areas, usually with large spots. - - Great Plains Red-sided Garter Snake, _Thamnophis ordinoides - parietalis_ - Dorsal stripes varying from yellow to blue or black. Usually found - near water. - - Hypothetical List: - Rubber Boa, _Charina bottae utahensis_ - May occur in rock slides or, possibly, in forested areas, on either - side of the Divide. - - Gopher Snake, _Pituophis catenifer sayi_ - May occur along eastern boundary (Great Plains). - - Yellow-bellied Blue Racer, _Coluber constrictor mormon_ - May occur on eastern boundary of Park along border of Great Plains. - - Painted Turtle, _Chrysemys picta_ - May occur in ponds and sluggish waters from Upper Sonoran Zone to - Canadian Zone. - - Western Skink, _Eumeces skiltonianus_ - May occur in Transition Zone along western border of Park. - - [Illustration: Northern Alligator Lizard] - - Northern Alligator Lizard, _Gerrhonotus coeruleus principis_ - May occur in Transition Zone along western border of Park. - - Amphibians - Tiger Salamander, _Ambystoma tigrinum melanostrictum_ - Ground color either black or bluish-black, with large spots or - blotches of yellow. - - Long-toed Salamander, _Ambystoma macrodactylum_ - Ground color black or dark brown; wide band of yellow extends from - back of head to tip of tail. - - Northwestern Toad, _Bufo boreas boreas_ - Widely distributed over entire Park. (Also known as Columbian, - Northern, or Western Toad.) - - [Illustration: Western Spotted Frog] - - Western Spotted Frog, _Rana pretiosa pretiosa_ - Widely distributed over entire Park. (Also known as Western or Pacific - Frog.) - - Green Frog, _Rana clamitans_ - One specimen, from Bowman Lake. (Chicago Natural History Museum) - - Tailed Frog, _Ascaphus truei_ - Should be fairly common, although it is not often taken. - - Pacific Tree-toad, _Hyla regilla_ - Small size and disks on fingers and toes identify this species. Common - throughout Park. - - -Fishes of Glacier National Park - -Classification and common scientific names are from: “A List of Common -and Scientific Names of Fishes from the United States and Canada,” -American Fisheries Society Publication No. 2, 1960. - - Key to symbols: - N Species native to at least one major drainage of the Park. - I Non-native species, having been introduced into Park waters by man. - S A species of sporting qualities and valued for recreational angling. - 1 Waterton Drainage - 2 Belly River Drainage - 3 Swiftcurrent Drainage - 4 St. Mary Drainage - 5 Two Medicine Drainage - 6 Middle Fork Flathead River Drainage (exclusive of McDonald Valley) - 7 McDonald Valley Drainage - 8 North Fork Flathead River Drainage - - [Illustration: Lake Trout] - - Family _Salmonidae_ (trouts, whitefishes, and grayling) - Lake Whitefish, _Coregonus clupeaformis_ (I) (1, 2, 3, 4, 7) - Pygmy Whitefish, _Prosopium coulteri_ (N) (7) - Mountain Whitefish, _Prosopium williamsoni_ (N) (S) (1, 2, 3, 4, 5, 6, - 7, 8) - Kokanee (Sockeye) Salmon, _Oncorhyncus nerka_ (I) (S) (3, 7, 8) - Cutthroat Trout, _Salmo clarki_ (N) (S) (1, 2, 3, 4, 5, 6, 7, 8) - Rainbow Trout, _Salmo gairdneri_ (I) (S) (1, 2, 3, 4, 5, 7) - Brook Trout, _Salvelinus fontinalis_ (I) (S) (1, 2, 3, 4, 5, 6, 7) - Dolly Varden, _Salvelinus malma_ (N) (S) (1, 2, 3, 4, 6, 7, 8) - Lake Trout, _Salvelinus namaycush_ (N) (S) (1, 2, 4, 5, 7, 8) - Arctic Grayling, _Thymallus arcticus_ (I) (S) (2, 8) - - Family _Esocidae_ (pikes) - Northern pike, _Esox lucius_ (N) (S) (1, 2, 3) - - [Illustration: Redside Shiner] - - Family _Cyprinidae_ (minnows and carps) - Longnose Dace, _Rhinichthys cataractae_ (N) (2, 3, 4, 5, 6, 7, 8) - Northern Pearl Dace, _Margariscus margarita_ (N) (3, 5) - Redside Shiner, _Richardsonius balteatus_ (N) (7, 8) - Streamline Chub, _Hybopsis dissimilis_ (N) (1, 3) - Northern Squawfish, _Ptychocheilus oregonensis_ (N) (7, 8) - - [Illustration: White Sucker] - - Family _Catostomidae_ (suckers) - White Sucker, _Catostomus commersoni_ (N) (1, 2, 3, 4, 5) - Largescale Sucker, _Catostomus macrocheilus_ (N) (6, 7, 8) - Longnose Sucker, _Catostomus catostomus_ (N) (1, 2, 3, 4, 5, 6, 7, 8) - - Family _Gadidaie_ (codfishes and hakes) - Burbot, _Lota lota_ (N) (S) (1, 4) - - Family _Cottidae_ (sculpins) - Mottled sculpin, _Cottus bairdi_ (N) (5, 6, 7, 8) - Spoonhead sculpin, _Cottus ricei_ (N) (1, 2, 3, 4) - - -Birds of Glacier National Park - - Key to symbols: - E—occurs on east side of the park (east of the Divide) - W—occurs on west side of the park (west of the Divide) - A—occurs in alpine areas - ab—abundant - c—common - u—uncommon - r—rare - i—introduced - a—accidental - - [Illustration: Common Loon] - - Loons - Common Loon E, W, ab - Arctic Loon? - Red-throated Loon? - - [Illustration: Western Grebe] - - Grebes - Red-necked Grebe E, W, c - Horned Grebe E, W, ab - Eared Grebe E, W, c - Western Grebe E, W, u - Pied-billed Grebe E, W, r - - Pelicans, Cormorants - White Pelican E, W, u - Double-crested Cormorant E, r - - [Illustration: Great Blue Heron] - - [Illustration: American Bittern] - - Herons, Bitterns - Great Blue Heron E, W, c - Black-crowned Night Heron a - American Bittern, W, r - - [Illustration: Mallard] - - [Illustration: Wood Duck] - - [Illustration: Ruddy Duck] - - Swan, Geese, Ducks - Whistling Swan E, W, ab - Trumpeter Swan E, W, r - Canada Goose E, W, c - Snow Goose E, W, c - Ross’ Goose E, W, r - Mallard E, W, ab - Gadwall E, W, r - Pintail E, W, c - Green-winged Teal E, W, c - Blue-winged Teal E, W, u - Cinnamon Teal E, W, u - European Widgeon E, W, c - American Widgeon E, W, ab - Northern Shoveler E, W, c - Wood Duck E, W, r - Redhead E, W, c - Ring-necked Duck E, W, u - Canvasback E, W, u - Lesser Scaup E, W, c - Greater Scaup? - Common Goldeneye E, W, c - Barrow’s Goldeneye E, W, ab - Bufflehead E, W, u - Harlequin Duck E, W, c - White-winged Scoter E, W, r - Ruddy Duck E, W, c - Hooded Merganser E, W, u - Common Merganser E, W, ab - Red-breasted Merganser, E, W, u - - [Illustration: Cooper’s Hawk] - - [Illustration: Marsh Hawk] - - Vultures, Hawks, Eagles - Turkey Vulture E, W, r - Goshawk E, W, c - Sharp-shinned Hawk E, W, u - Cooper’s Hawk E, W, u - Red-tailed Hawk E, W, c - Red-shouldered Hawk a - Swainson’s Hawk E, W, c - Rough-legged Hawk E, W, r - Ferruginous Hawk E, W, u - Golden Eagle, E, W, A, c - Bald Eagle, E, W, ab - Marsh Hawk E, W, ab - Osprey E, W, ab - Prairie Falcon E, W, A, r - Peregrine Falcon E, W, r - American Kestrel E, W, c - - [Illustration: Sharp-tailed Grouse] - - Grouse, Ptarmigans - Blue Grouse, E, W, ab - Spruce Grouse E, W, ab - Ruffed Grouse E, W, ab - Sharp-tailed Grouse E, r - White-tailed Ptarmigan A, c - Willow Ptarmigan ? - Ring-necked Pheasant E, W, r, i - Gray Partridge E, W, r, i - - Cranes - Sandhill Crane E, r - - [Illustration: American Coot] - - Rails, Coots - Sora E, W, r - American Coot E, W, ab - - [Illustration: Greater Yellowlegs] - - Shorebirds - Killdeer E, W, c - Black-bellied Plover E, r - Common Snipe E, W, c - Long-billed Curlew E, r - Upland Sandpiper E, r - Spotted Sandpiper E, W, A, ab - Solitary Sandpiper E, r - Willet, E, r - Pectoral Sandpiper E, r - Baird’s Sandpiper E, W, r - Lesser Yellowlegs, E, W r - Greater Yellowlegs E, W, r - American Avocet E, W, u - Northern Phalarope E, W, r - Wilson’s Phalarope E, W, u - Black Turnstone ? - Long-billed Dowitcher E, W, r - - [Illustration: Herring Gull] - - Gulls, Terns - Herring Gull E, W, r - California Gull E, W, ab - Ring-billed Gull E, W, c - Franklin’s Gull E, W, c - Bonaparte’s Gull E, u - Forster’s Tern E, W, u - Common Tern E, r - Caspian Tern a - Black Tern E, W, u - - [Illustration: Mourning Dove] - - Doves, Pigeons - Band-tailed Pigeon E, W, r - Mourning Dove E, W, c - Rock Dove E, W, r, i - - [Illustration: Great Horned Owl] - - Owls - Screech Owl E, W, r - Great Horned Owl E, W, ab - Snowy Owl E, W, u - Hawk Owl E, W, u - Pygmy Owl E, W, ab - Barred Owl E, W, c - Great Gray Owl E, W, u - Long-eared Owl E, W, r - Short-eared Owl, E, W, c - Boreal Owl E, W, r - Saw-whet Owl E, W, u - - [Illustration: Common Nighthawk] - - Nighthawks, Swifts - Common Nighthawk E, W, ab - Black Swift E, W, u - Vaux’s Swift E, W, ab - White-throated Swift W, A, r - - Hummingbirds - Broad-tailed Hummingbird E, W, r - Rufous Hummingbird E, W, A, ab - Calliope Hummingbird E, W, A, ab - Black-chinned Hummingbird E, W, r - - [Illustration: Belted Kingfisher] - - Kingfishers - Belted Kingfisher E, W, ab - - Woodpeckers - Common Flicker E, W, ab - Pileated Woodpecker E, W, ab - Red-headed Woodpecker E, W, r - Lewis’ Woodpecker E, W, c - Yellow-bellied Sapsucker E, W, ab - Williamson’s Sapsucker E, W, u - Hairy Woodpecker E, W, ab - Downy Woodpecker E, W, ab - Black-backed Three-toed Woodpecker E, W, ab - Northern Three-toed Woodpecker E, W, ab - - [Illustration: Ash-throated Flycatcher] - - Flycatchers - Eastern Kingbird E, W, ab - Western Kingbird E, W, u - Ash-throated Flycatcher a - Say’s Phoebe E, W, r - Willow Flycatcher E, W, c - Hammond’s Flycatcher E, W, ab - Olive-sided Flycatcher E, W, ab - Western Flycatcher E, r - Western Wood Peewee E, W, c - - Larks - Horned Lark E, W, A, ab - - [Illustration: Barn Swallow] - - Swallows - Violet-green Swallow E, W, A, ab - Tree Swallow E, W, ab - Bank Swallow E, W, ab - Rough-winged Swallow E, W, u - Barn Swallow E, W, u - Cliff Swallow E, W, A, ab - - [Illustration: Common Crow] - - Jays, Magpies, Crows - Gray Jay E, W, ab - Blue Jay E, W, r - Steller’s Jay E, W, ab - Black-billed Magpie E, W, ab - Common Raven E, W, A, ab - Common Crow E, W, ab - Clark’s Nutcracker E, W, A, ab - - Chickadees - Black-capped Chickadee E, W, ab - Mountain Chickadee E, W, ab - Boreal Chickadee E, W, r - Chestnut-backed Chickadee E, W, u - - Nuthatches, Creepers - White-breasted Nuthatch E, W, u - Red-breasted Nuthatch E, W, ab - Brown Creeper E, W, ab - - [Illustration: Winter Wren] - - Dippers, Wrens - Dipper E, W, A, ab - House Wren E, W, u - Winter Wren E, W, ab - Long-billed Marsh Wren a - Rock Wren E, W, u - - Catbirds, Thrashers - Gray Catbird E, W, u - - [Illustration: Mountain Bluebird] - - Thrushes, Bluebirds, Solitaires - American Robin E, W, A, ab - Varied Thrush E, W, ab - Hermit Thrush E, W, ab - Swainson’s Thrush E, W, ab - Veery E, W, c - Western Bluebird E, W, r - Mountain Bluebird E, W, A, ab - Townsend’s Solitaire E, W, A, ab - - Kinglets - Golden-crowned Kinglet E, W, ab - Ruby-crowned Kinglet E, W, ab - - Pipits - Water Pipit E, W, A, ab - - [Illustration: Cedar Waxwing] - - Waxwings - Bohemian Waxwing E, W, ab - Cedar Waxwing E, W, ab - - Shrikes - Loggerhead Shrike E, W, r - Northern Shrike E, W, r - - [Illustration: Starling] - - Starlings - Starling E, W, c, i - - [Illustration: Red-eyed Vireo] - - Vireos - Solitary Vireo E, W, ab - Red-eyed Vireo E, W, ab - Warbling Vireo E, W, ab - - Warblers - Black and White Warbler W, r - Tennessee Warbler E, W, r - Orange-crowned Warbler E, W, r - Nashville Warbler E, W, r - Yellow Warbler E, W, ab - Yellow-rumped Warbler E, W, ab - Townsend’s Warbler E, W, ab - Northern Waterthrush E, W, ab - MacGillivray’s Warbler E, W, ab - Common Yellowthroat E, W, ab - Wilson’s Warbler E, W, ab - American Redstart E, W, ab - Yellow-breasted Chat ? - - [Illustration: House Sparrow] - - Weaver Finches - House Sparrow E, W, r, i - - Blackbirds, Orioles - Bobolink E, r - Western Meadowlark E, W, u - Red-winged Blackbird E, W, ab - Northern Oriole E, W, r - Brewer’s Blackbird E, W, u - Rusty Blackbird E, W, r - Yellow-headed Blackbird E, r - Common Grackle E, r - Brown-headed Cowbird E, W, c - - [Illustration: Evening Grosbeak] - - Tanagers, Grosbeaks - Western Tanager E, W, ab - Evening Grosbeak E, W, ab - Pine Grosbeak E, W, ab - Black-headed Grosbeak E, W, r - - [Illustration: American Goldfinch] - - Finches, Sparrows, Buntings - Lazuli Bunting E, W, c - Lark Bunting E, W, r - Snow Bunting E, W, c - Cassin’s Finch E, W, A, ab - Gray-crowned Rosy Finch E, W, A, ab - American Goldfinch E, W, u - Common Redpoll E, W, c - Pine Siskin E, W, A, ab - Red Crossbill E, W, ab - White-winged Crossbill E, W, u - Rufous-sided Towhee E, W, u - Green-tailed Towhee E, W, r - Savannah Sparrow E, W, c - LeConte’s Sparrow E, W, u - Vesper Sparrow E, W, ab - Tree Sparrow E, W, r - Chipping Sparrow E, W, A, ab - Brewer’s Sparrow E, W, r - Harris’ Sparrow E, W, r - White-crowned Sparrow E, W, A, ab - Fox Sparrow E, W, A, ab - Lincoln’s Sparrow E, W, A, c - Song Sparrow E, W, ab - Dark-eyed Junco E, W, c - McCown’s Longspur E, c - Lapland Longspur E, W, c - Chestnut-collared Longspur E, c - - - - - Suggested Reading - - -Alexander, Taylor R. and George S. Fichter, _Ecology_ (a Golden guide). - Western Publishing Co., Inc., Racine, Wis. 1973. - -Alt, David D. and Donald W. Hyndman, _Rocks, Ice and Water, the Geology - of Waterton-Glacier Park_. Mountain Press Publishing Co., - Missoula, Mont. 1973. - -Baker, William, et. al., _Wildlife of the Northern Rocky Mountains_. - Naturegraph Co., Healdsburg, Calif. 1961. - -Borland, Hal, _The History of Wildlife in America_. National Wildlife - Federation, Washington, D.C. 1975. - -Brooks, Maurice, _The Life of The Mountains_. McGraw-Hill, New York. - 1967. - -Costello, David F., _The Mountain World_. Thomas Y. Crowell Co., New - York. 1975. - -Craighead, John J., et. al., _A Field Guide to Rocky Mountain - Wildflowers_. Houghton Mifflin Co., Boston. 1963. - -Dobie, J. Frank, _The Voice of the Coyote_. Little, Brown and Co., - Boston. 1950. - -Farb, Peter, _Face of North America_. Harper and Row, New York. 1963. - -Gildart, Robert C., _Meet the Mammals of Waterton-Glacier_. Glacier - Natural History Association, Inc. Thomas Printing, Inc., - Kalispell, Mont. 1975. - -McCormick, Jack, _The Life of the Forest_. McGraw-Hill, New York. 1966. - -Milne, Lorus and Margery Milne, _The Balance of Nature_. Alfred A. - Knopf, Inc., New York. 1960. - -Nelson, Alan G., _Wildflowers of Glacier National Park_. Nelson, Great - Falls, Mont. 1970. - -Peattie, Donald Culross, _A Natural History of Western Trees_. Bonanza - Books, New York. 1953. - -Ruhle, George C., _Roads and Trails of Waterton-Glacier Parks_. John W. - Forney, Minneapolis, Minn. 1972. - -Shea, David S., _Animal Tracks of Glacier National Park_. Special - Bulletin No. 11, Glacier Natural History Association, Inc., West - Glacier, Mont., 1969. - -Storer, John H., _The Web of Life_. Devin-Adair Co., Old Greenwich, - Conn. 1953. - -Zwinger, Ann H. and Beatrice E. Willard, _Land Above the Trees_. Harper - and Row, New York. 1972. - - [Illustration: WATERTON LAKES NATIONAL PARK—GLACIER NATIONAL PARK] - - Using Metrics - - As we go to press with this book, the United States is in the early - stages of conversion to the metric system of measurement, and though - we urge you to think metric—for most of the world does—we provide - this table to help you understand the measurements given in the - book. - - To convert from to multiply by - - Millimeters Sixteenth-inches 0.6301 - Centimeters Inches 0.3937 - Meters Feet 3.2808 - Kilometers Miles 0.6214 - Hectares Acres 2.4711 - Hectares Square miles 0.00386 - Grams Troy Ounces 0.0322 - Kilograms Pounds 2.2046 - Degrees—Celsius Degrees—Fahrenheit 1.8, and add 32 - - [Illustration: Temperature Conversion Chart] - - [Illustration: Length Conversion Chart] - - Drawings from David S. Shea, _Animal Tracks of Glacier National - Park_ - - [Illustration: red fox, - hind foot, in mud - 53 mm.] - - [Illustration: mule deer, - adult buck, in snow - 72 mm.] - - [Illustration: badger, - left front foot, in mud - 43 mm.] - - [Illustration: coyote, - hind foot, in snow - 63 mm.] - - About the Author - - Greg Beaumont’s interest in Glacier National Park dates from 1963, - when he was a summer employee at Lake McDonald Lodge. In 1966 he and - his wife were fire-control lookouts on Numa Ridge in the Bowman - Valley. Now a free-lance writer-photographer, he lives with his - family in Lincoln, Nebraska. - - National Park Service - U.S. Department of the Interior - - As the Nation’s principal conservation agency, the Department of the - Interior has responsibility for most of our nationally owned public - lands and natural resources. This includes fostering the wisest use - of our land and water resources, protecting our fish and wildlife, - preserving the environmental and cultural values of our national - parks and historical places, and providing for the enjoyment of life - through outdoor recreation. The Department assesses our energy and - mineral resources and works to assure that their development is in - the best interests of all our people. The Department also has a - major responsibility for American Indian reservation communities and - for people who live in Island Territories under U.S. administration. - - - - - Transcriber’s Notes - - -—Retained publication information from the printed edition: this eBook - is public-domain in the country of publication. - -—Corrected a few palpable typos. - -—Included a transcription of the text within some images. - -—In the text versions only, text in italics is delimited by - _underscores_. - - - - - - - -End of the Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -*** END OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - -***** This file should be named 55150-0.txt or 55150-0.zip ***** -This and all associated files of various formats will be found in: - http://www.gutenberg.org/5/5/1/5/55150/ - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - -Updated editions will replace the previous one--the old editions will -be renamed. - -Creating the works from print editions not protected by U.S. copyright -law means that no one owns a United States copyright in these works, -so the Foundation (and you!) can copy and distribute it in the United -States without permission and without paying copyright -royalties. 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Thus, we do not -necessarily keep eBooks in compliance with any particular paper -edition. - -Most people start at our Web site which has the main PG search -facility: www.gutenberg.org - -This Web site includes information about Project Gutenberg-tm, -including how to make donations to the Project Gutenberg Literary -Archive Foundation, how to help produce our new eBooks, and how to -subscribe to our email newsletter to hear about new eBooks. - diff --git a/old/55150-0.zip b/old/55150-0.zip Binary files differdeleted file mode 100644 index fb3bad6..0000000 --- a/old/55150-0.zip +++ /dev/null diff --git a/old/55150-8.txt b/old/55150-8.txt deleted file mode 100644 index 0f7472a..0000000 --- a/old/55150-8.txt +++ /dev/null @@ -1,4332 +0,0 @@ -The Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -This eBook is for the use of anyone anywhere in the United States and most -other parts of the world at no cost and with almost no restrictions -whatsoever. You may copy it, give it away or re-use it under the terms of -the Project Gutenberg License included with this eBook or online at -www.gutenberg.org. If you are not located in the United States, you'll have -to check the laws of the country where you are located before using this ebook. - -Title: Many-Storied Mountains - The Life of Glacier National Park - -Author: Greg Beaumont - -Release Date: July 19, 2017 [EBook #55150] - -Language: English - -Character set encoding: ISO-8859-1 - -*** START OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - - - - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - - - - - - - *GPO:1978-261-215/3 - For sale by the - Superintendent of Documents, - U.S. Government Printing Office, - Washington, DC 20402. - Stock Number 024-005-00709-1. - - Library of Congress Cataloging In Publication Data - - Beaumont, Greg, 1943- - Many-storied mountains. - - (Natural history series) - 1. Natural history--Montana--Glacier National Park. - 2. Glacier National Park. I. Title. II. Series: Natural history series - (Washington, D.C.) - OH105 M9B43 500.9'786'52 78-606071 - - - - - Many-storied Mountains - The Life of Glacier National Park - - - Written and - photographed by - Greg Beaumont - - 1978 - Natural History Series - Division of Publications - National Park Service - U.S. Department of the Interior - - [Illustration: The landform of Glacier National Park is a monument - to the power of moving ice. This view from Stoney Indian Pass is - startlingly different from the scene of a million years ago, when - the glaciers of the Pleistocene were sculpturing the land. Only the - higher peaks would then have been visible above the blanket of ice - that flowed like a slow-moving river down into the Mokowanis Valley - and out into the Great Plains beyond.] - - -About This Book - -This natural history of the mountain wilderness called Glacier National -Park is not a guidebook, but provides an overview of the ecology of the -region. At the same time, it is a personal statement, revealing one -individual's response to this rugged, delicate land. - -For their consistent cooperation and helpfulness, I wish especially to -thank Chief Naturalist Ed Rothfuss and his capable staff. Technical and -field assistance came from many; for special thanks, I would like to -single out Art Sedlack, Francis Singer, Bert Gildart, Walt Martin, Craig -Kuchel, and Danny On. The manuscript profited greatly from the criticism -of Douglas Chadwick, to whom I am deeply grateful. - - --G.B. - - -The National Park Service Division of Publications gratefully -acknowledges the financial support given this book project by the -Glacier Natural History Association, Inc., West Glacier, Mont. - - - - - Contents - - - Song of the High Peaks 1 - Cycles and Seasons 5 - Bedrock: The First Story 6 - The Rising of the Sun and the Running of the Deer: A Glacier - Year 39 - Plant-and-Animal Communities 43 - Over Going-to-the-Sun Road 44 - Groves and Grasslands: The Prairie Sea 46 - The Forest 70 - Scrub Forest 105 - Tundra 109 - Water Communities 114 - Shooting Stars 121 - Appendix 125 - Pictorial Features - The Mountains of Glacier 10 - The Forests of Glacier 48 - The Vital Predator 78 - Protective Coloration 84 - _Ursus arctos horribilus:_ The Vulnerable King 88 - Bald Eagles and Kokanee Salmon: A Recent Gathering 92 - A Triumph of Many Colors 96 - Fire Succession: Key to Continuity 100 - - -Illustrations by Celia Strain/Morgan-Burchette Assoc. - - [Illustration: Soaring eagle] - - - - - Song of the High Peaks - - -April again and the wind turns on the Great Plains. Wedges of geese, -high and determined, began this storm of spring, their voices sharp as -the morning frost. Sicklebills cry to claim the land, sandhill cranes -wheel and talk overhead, and everywhere the killdeer shout. -Pasqueflowers push the bleak soil aside, beginning the westward rush -that I must join, seeking again the sight of mountains. - -In Glacier National Park the land is folded up. On the east, Chief -Mountain, Curly Bear, and Rising Wolf break the prairie's hold. When the -early French fur trappers saw these peaks glistening in the distance -with summer-long snows and perpetual ice, they named this region "the -land of shining mountains." But for all the ice and snow that reflect -the summer sun, the park's present glaciers are but snowflakes compared -to the mighty rivers of ice that carved this land. Glaciation, the -magnificent sculptor, left its bold signature everywhere, and this park -honors with its name the force that shaped it. - -But the essential excitement of this land is more than cliff face, -spire, and sudden storm. It comes to you when you realize that here is -an aggregation of dramatically differing life zones, where a day's walk -can easily take you from prairie and forest to treelimit and tundra; -where a dense forest of redcedar and hemlock, similar to the rain -forests of the Pacific coast, exists a score of kilometers from the -great prairie sea. - -Or it comes when you discover that these mountains--young and sharp with -shadows, snow-jeweled and newly gowned with forests--are chiseled from -the oldest unaltered sedimentary rocks on earth. - -I come from the prairie and love its broad strokes; I've learned to hear -the singing in the grass and to see those long, slow seasons soar the -level horizons like gliding hawks. But here I learned to match my days -against a wild earth, and in me grew the mysterious need to know a -mountain from its every side. Mountains that wear the dawn like yellow -hats, repeated in the named and nameless lakes. Mountains that stretch -the storms between them and balance rainbows ridge to ridge. - -I must see again the secret forest places, where the paleflowered -wood-nymphs hover like a breath, and know once more the endless meadows -painted camas blue. - -I need the perfect freedom of this land, to be able to say, _today I -will climb Siyeh_: to stand, for a time, on the rugged shoulders of this -upright earth. - - [Illustration: The sharp spire of little Matterhorn and the broad - face of Mt. Edwards loom above Going-to-the-Sun Road in the upper - McDonald Valley. During warm days in spring the valleys of the park - resound with the thunder of avalanches.] - - [Illustration: Twilight view.] - - - - - Cycles and Seasons - - -Bedrock: The First Story - -On the trail that connects the Logan Pass visitor center to Hidden Lake -overlook there is a shallow pond. Near Hidden Pass, it collects its -meltwater from the Continental Divide and sends it down the shallow -gorge that drains the Hanging Gardens; as a waterfall it plunges into -the upper St. Mary Valley where it becomes Reynolds Creek; joined by -other tributaries, it continues its long journey to Hudson Bay. - -The surface of this pond is seldom still, for the wind treats it like a -sea. Because the water is shallow, the wave action wrinkles the bottom -mud into ripple patterns, mimicking the churning waves. - -I like to come here early in the morning. Sometimes, arriving before the -wind awakes, I catch reflections of the surrounding mountains. Beyond -the low bench of Logan Pass the Garden Wall begins, running northward -with the Divide. In the eastern valley the pitched peak of -Going-to-the-Sun hunkers in the morning light like a tensed warrior. To -the south, the incisor Bearhat, beautiful cloud cutter of Hidden Lake -Valley, juts above the nearby saddle of the pass. But over this place, -standing as fresh monuments to an age of ice, tower the cliffs of -Clements and the pyramid Reynolds. - -I am sitting on a wedge of red rock. Its surface exhibits a wrinkled -pattern identical to the ripples in the soft mud of the shallow pond. -The distance is not great; with a stick I could reach out and touch the -mud. Yet this represents a gulf no bird can fly, for between the ripples -of this rock and the ripples of this mud lie billions of vanished -mornings, a constellation of years. - -These red, green, tan, white, black and purple bands of rock that layer -Glacier's mountains comprise the oldest unaltered sedimentary rocks on -Earth. They were laid down in Precambrian time, more than a billion -years ago, when life was just beginning, as the deposits of an inland -sea. - -For millions of years, sand, mud and carbonates washed into the ancient -sea, compressing the lower layers into mudstones and limestones, -building up a sediment thickness that may have been as much as 10,000 -meters (_see_ metric conversion table on page 136). - -When we look at the sharp contours of Glacier's mountains, we see the -evidence of uplift, overthrust and glaciation. But on the geologic clock -these are recent events, a mere eyeblink of time ago. For the vast -majority of years, the rocks lay undisturbed and level beneath the sea -and land. - -To understand better the tremendous time scale these rocks represent, we -need a way to visualize the vast collection of years. If we were to make -a movie of these geologic events, we would first need to determine how -many years each minute should represent. Since the Pleistocene lasted -about 3,000,000 years (its four ice ages sculpting the present muscle of -this land), let us make each minute portray a million years. To -chronicle these rocks we will then need a film 60 hours long! - -Not until the fifty-seventh hour of our film will the Mesozoic lowlands -begin to bulge with the coming Rocky Mountain chain. During the long -preceding hours we would have seen little else but sea--withdrawing, -advancing, deep and shallow; yellow, green, and brown with great -colonies of algae. Unseen below the water, lava has spilled out -occasionally on the sea bottom; once, it intruded between the rock -layers below, forming the conspicuous, 60-meter-thick band of black -diorite that we see today on many mountain faces in Glacier. - -During this time of initial uplift an amazing process is going on deep -underground. A major fault has developed, fracturing the buckled layers -of rock. A vast mountain plate begins to slide eastward, over-riding and -submerging the rock layers to the east and opening the wide trench that -is today the North Fork Valley. Known as the Lewis Overthrust, this -gigantic earth-force has created an unusual situation: ancient rock -strata lying atop recent rock strata. - -Now less than 3 minutes of film remain. The arrival of the ice is -imminent. We look at the landscape of featureless mountains and wonder -at the dramatic difference that this last 3 million years will make. We -do not see the familiar forests and lakes, the savage peaks, and the -broad, deep valleys of this present land. These mountains are gentle, -arid, and shallow-valleyed. The vague outlines are there; we recognize -the general alignments of the drainage systems, the bloated domes from -which sharp peaks will be cut. The mountains are connected to one -another by blunt ridges and smooth saddles, and the shadows they cast -are dull, dunelike. - -Suddenly the ice is there, filling the landscape, with only the -mountaintops protruding. Four times in these last 3 minutes of film the -ice sheets advance and retreat, each time leaving an altered landscape. -Strange lakes and forests fill the gaps between the glacial invasions. -Then we see the mountains we now know come into being rapidly, as if the -land were being hacked into shape by giant cleavers. - -After this flicker of Pleistocene time, the film ends, the forests -return, and familiar lakes shine beneath the sun again--these lakes and -forests we had thought to be timeless. - - -[_] -Up springs the morning wind from Hidden Valley, making the nearby alpine -fir branches whiz with its passing and shattering the perfect reflection -of Bearhat Peak on the pond. From where I sit, it is a short distance to -Hidden Pass; so I leave the pond and walk to the overlook to see again -the fine basin quarried by an ancient glacier. - -Hidden Lake, deep, far below, so blue, fits into its cliffed, crooked -valley like a polished boomerang. Closely ringed by ridge and -peak--distant Sperry Glacier and pointed Gunsight peering up from the -southern jumble, and broad Bearhat impossibly close--this lovely lake is -almost lost amid such sharp proclamations of rock. Its outlet gorge -gives a narrow view across the angled, hidden valleys of Avalanche and -McDonald, past the pyramid of Stanton, to the low, faraway undulations -of the Whitefish Range. - -Glaciation is a cruel master of mountains, biting deeply into their bulk -and leaving sheer, spectacular contours when the glaciers disappear. The -landforms here attest to their power, everywhere exhibiting the effects -of glaciation. - -In eating back the mountain headwall, alpine glaciers formed rounded -depressions, called cirques. Unlike the narrow clefts left by running -water, these broad, deep basins look as though they were made by -ice-cream scoops gouging into the rock. Hidden, Ptarmigan, Iceberg, and -Avalanche Lakes sit in well-developed cirque basins, and many mountains -are dimpled by the beginnings of other cirques--the conspicuous -amphitheater on the south shoulder of Heaven's Peak, for example. - -Occupying all major drainage systems, glaciers modified the contour of -the valleys, changing them from their narrow, stream-cut V-shapes into -broad U-shapes. Into these wide main valleys, waterfalls plunge from -higher, smaller valleys. Like rivers, flowing glaciers have tributaries. -Lacking the ice mass and cutting power of the main glaciers, these -tributary ice fingers could not bite as deeply into the bedrock. When -the ice melted, hanging valleys were left stranded high above the main -valley floor. Hidden Lake sits in one of these hanging valleys, and from -it Hidden Creek plunges 750 meters into Avalanche Basin toward McDonald -Creek. - -On my many previous visits to this pass I have been too busy enjoying -the wildflowers, the weather, or the scenery to realize what an open -textbook of glaciation is everywhere displayed. - -I stand here on a small saddle of a pass. Wherever glaciers met, passes, -or cols, were created. A high, notched pass like this one (or -Swiftcurrent or Gunsight) reveals recent connections. Broad, lower -passes, such as Logan, resulted where the ice early overran the mountain -ridge and had a chance to work longer. - -Where two glaciers worked on opposing sides of a ridge and failed to -meet, they formed an arte--a thin, steep-walled remnant resembling a -saw blade. Another ice age would probably consume the park's many thin -artes, such as the Garden Wall and Ptarmigan Wall; but it would also -create new ones from existing ridges. - -Further testimony to the sculpting power of ice is presented by Mt. -Reynolds, looming to the east. The most dramatic feature of a glaciated -landscape is the pyramid-shaped mountain called a horn--and Reynolds is -a perfect example. Horns were formed when three or more glaciers cloaked -the mountain, excavating its sides toward its core and gradually -transforming its original domed shape into a sheer-sided peak. Glacier -has many remarkable horns, from the sleek spire of St. Nicholas in the -south to exquisite Kinnerly in the northern Kintla valley. - -Sperry Glacier stares back at me from the flank of Gunsight. Glaciers -found in the park today are not remnants of the last ice phase, which -ended here about 8,000 years ago, but are newly formed, having come into -existence some 4,000 years ago. They reflect a cooling trend in the -present climate. - -Shrinking steadily from their period of greatest extent in the middle of -the last century, these modern glaciers finally stabilized in the late -1940s and since then have shown only a slight increase in area. - -Movement distinguishes glaciers from icefields, and the movement of ice -is a force on as well as a feature of a landscape. A glacier excavates -by abrading and plucking at the rock. Alternately melting and freezing, -ice at the headwalls plucks out blocks of rock. Ultimately the rocks are -deposited along the sides or at the feet of the glacier as moraine -debris. But as they move in the grip of the ice, they constantly abrade -the rock surfaces they encounter. Polished rock beds of past glaciers -show striations--grooves gouged by rock fragments imbedded in the moving -ice. - -Flow rate of a glacier depends upon the thickness of the ice and the -degree of slope. Under tremendous pressure, ice becomes plastic, like -thick taffy. Unlike kilometer-thick continental glaciers, which may move -a hundred meters a day, small alpine glaciers seldom progress more than -two or three centimeters per day. - -Although a glacier moves, it gets nowhere if in a state of -equilibrium--when annual melting equals annual accumulation. Snow mass -gained at the sun-shielded headwall is usually lost as melt at the -exposed snout. Glaciers such as Sexton or Weasel Collar, whose snouts -perch on cliff edges, also lose mass by calving. Thunder you hear on a -late-summer day near such a glacier may actually be the sound of ice -pushed off from the lip of a cliff. - -Walking back to the visitor center, I suddenly stop where the trail -skirts the steep moraine of Mt. Clements. From the opposite side of the -moraine five mountain goats have appeared. Spotting me on the trail -below, they also halt. But before I can get to my camera they are off in -a stiff-legged gallop, running in single file along the crest of the -moraine to the distant safety of the mountain face. - -Moraines are ridges of rock debris piled up along the edges and -terminuses of glaciers. Like a bracelet lying against the wall of this -mountain, the circle of steeply piled debris marks the extent of a -small, recently vanished glacier. Ghost of the power that once resided -here, a stagnant icefield lies beneath the confining walls of the -moraine. The recent accumulation of these rock fragments is a mighty -accomplishment, attesting to the force of moving ice. - - _continued on p. 38_ - - [Illustration: The Mountains of Glacier - - Lying astride the Continental Divide in the Northern Rockies, - Glacier is above all else a mountain park. The special beauty of its - lakes, streams, and forests derives from the microclimates and - varied topography and soil produced by mountain-building and - mountain-eroding forces.] - - [Illustration: Overthrust Mountains - - 1 A hypothetical block of the Earth's crust in the region of Glacier - National Park as it existed more than 60 million years ago. The two - layers shown actually represent many strata of sedimentary rocks. - - 2 Lateral pressure begins to force the rock layers to buckle. - - 3 A large fold has been created, forcing the rock strata to double - over and overturning some layers. A break, or _fault_, is forming at - the plane of greatest stress. - - 4 The break has been completed and the strata west of the fault have - slid eastward, up and over the rocks east of the fault. - - 5 The Glacier landscape today. Throughout the millions of years - during which the folding, faulting, and overthrusting have been - taking place, the process of erosion has continued; a thousand - meters of stratified rocks have been worn away, so that only a - remnant of the overthrust layers can be seen today. Because - Glacier's eastern slope represents the eroded face of the overthrust - block, the mountain range rises precipitously from the prairie, with - no foothills breaking the abrupt transition from open prairie to - mountain valley.] - - [Illustration: The peaks in this photograph (a view to the northwest - from Marias Pass) are remnants of the overthrust block, which moved - eastward. The dividing line between the light-colored rocks and the - gray talus slopes beneath them is the Lewis Overthrust Fault.] - - [Illustration: Glaciation - - 1 This is how the landscape in this region might have appeared - before the onset of the Pleistocene, millions of years ago. Note the - stream-eroded, V-shaped valleys. The climate at that time was dry. - - 2 Glaciers began to form high on the peaks, crept downward, and - joined to form larger glaciers. - - 3 After many centuries of glaciation, tributary glaciers have cut - back into the peaks, forming basins called _cirques_. Thick - glaciers, moving rapidly and carrying rock fragments, have abraded - the main valleys' floors and sides, widening and deepening the - valleys into characteristic U-shapes.] - - V-shaped Valley - Tributary Glacier - Unglaciated Peak - Headwall - Meltwater Stream - Nose of Glacier - Crevasse - - [Illustration: 4 In the present landscape, free of all but remnant - glaciers, small lakes called _tarns_ occupy many of the cirque - basins; and waterfalls plunge into the main valleys from higher, - shallower, tributary valleys, called _hanging valleys_. _Alluvial - cones_--recent accumulations of rock debris--have begun to build - along the valley walls. In the main valley, a _moraine_ (a deposit - of rock materials left by the retreating glacier) has formed a dam - that holds back a large lake. - - During all this time, all parts of the terrain not buried under ice - and snow have been weathered and eroded by nonglacial forces. Thus - the contours of the jagged peaks and sheer cliffs have been - softened.] - - Unglaciated V-shaped Valley - U-shaped Valley - Hanging Valley - Cirque - Tarn - Alluvial Cone - Moraine - Morainal Lake - - [Illustration: Glacial landforms can be identified in this view of - the Mokowanis Valley.] - - [Illustration: A Divided Climate - - Because of an eastward flow of cool, moist Pacific air masses, the - climate of northwestern Montana, including the western portion of - Glacier National Park, differs from that of other portions of - Montana. As a result of increased precipitation, Glacier's western - valleys support a rich flora, more typical of the Pacific Northwest. - - West - - Moist Pacific air - - As the moisture-laden Pacific winds are pushed up the windward - slopes of Glacier's mountains, the air cools and water vapor - condenses, forming fog or clouds. Rain or snow begins to fall as the - air continues to rise and cool. By the time the air mass reaches the - crest and flows down the leeward slopes, most of the moisture has - been lost. - - Western slopes average about 70 cm. of precipitation at elevations - between 900 and 1,100 m. Upper elevations average 200 to 250 cm., - mostly in the form of snow; and 300 to 500 cm. is common. - - East - - Dry chinook winds - - Eastern slopes, under the influence of Continental air masses, - receive less annual precipitation. West Glacier's annual average is - 66.5 cm. Babb, a small town east of the park, averages 49.3 cm. - Frequent high winds east of the Divide further reduce moisture - through evaporation. - - Exposed to Arctic air masses flowing down from Canada, locations - east of the Divide also suffer more severe winter conditions than do - protected western valleys. Average January temperature is -5C at - West Glacier, -8 at Babb. - - Moreover, 80 percent of the winter days in the western portion of - the park are overcast, a condition almost identical to that of - Seattle, Wash. This serves to moderate winter temperatures and to - minimize evaporation.] - - [Illustration: Moss campion and mountain forget-me-not colonize a - fellfield. Fellfields are rocky alpine sites that are slightly less - than 50% bare rock, interspersed with such plant pioneers as cushion - plants, mosses, and lichens.] - - [Illustration: High lakes generally occupy cirque basins. These - depressions in the valley bedrock, quarried by glaciers, are deepest - near the headwall where ice thickness was greatest. Cold and deep, - and ice-free only weeks each year, tarns cannot support vascular - plants or vertebrates. Iceberg Lake, shut off from the sun most of - the year by the encompassing 1,000-meter walls of Mt. Wilbur and the - Ptarmigan Wall, is never completely free of ice.] - - [Illustration: Lake McDonald, 16 kilometers long, 2 kilometers wide, - and 134 meters deep, is the largest lake in the park. Its basin is - the classic U-shaped glacial valley. Forested lateral moraines on - either shore gently rise 600 meters above lake level. - Going-to-the-Sun Road snakes along the eastern shore, and Logan Pass - lies near the center of the photograph, behind the peaks of the - Lewis Range.] - - [Illustration: Subjected to the drying and shaping effects of wind - both winter and summer, this Douglas-fir, growing in the prairie - community near St. Mary, will attain neither the symmetrical shape - nor the great size of the Douglas-firs growing in moister, more - sheltered sites on the western slopes of the Continental Divide.] - - [Illustration: Freeze-and-thaw cycles continually fracture and - loosen rocks along joints, making them subject to removal by the - actions of water, gravity, and avalanche. The resulting fans of rock - debris (talus cones) indicate the extent of erosion since the - withdrawal of the Pleistocene glaciers.] - - [Illustration: Although moving water is an agent of erosion--the - primary destructive force of mountain masses--it also permits life. - Even small watercourses, such as this freshet, abound with plant and - invertebrate life.] - - [Illustration: Going-to-the-Sun Mountain, towering above the St. - Mary Valley, from the trail to Siyeh Pass. The coniferous forest at - its base and the alpine tundra plants at its summit are closely - juxtaposed in space; but if these two communities grew at the same - elevation they would be separated by thousands of kilometers. Hiking - from St. Mary Lake up to Siyeh Pass is going, in effect, from - Montana to the Arctic Circle; but here the life zones are compressed - and sharply divided rather than extended and overlapping.] - - [Illustration: Setting moon and snow shelf near the summit of - Heavens Peak. Note stratification of Precambrian sediments.] - - [Illustration: Western redcedars line the shores of Lake McDonald. - Because of prevailing air currents from the Pacific coast, winters - in the protected western valleys are moist and comparatively mild, - and this deep body of water freezes over an average of only one - winter in four.] - - [Illustration: Moose often follow the spring snowmelt upwards to the - headwaters of drainages. This bull will remain at Thunderbird Pond, - at the base of Brown Pass, until autumn, when it will return to its - Waterton Valley wintering ground.] - - [Illustration: Because of the high reproductive capacity of insects - and small mammals, if all their offspring survived the earth's plant - life would be consumed within one year. This is prevented by natural - controls such as predation and parasitism. The American kestrel - ("sparrow hawk") feeds primarily on large insects and on small - rodents such as the meadow vole here.] - - [Illustration: Gray jays are found in the deep coniferous forests of - the park. In some parks gray jays, or "camp robbers," loiter about - campgrounds and picnic areas begging or stealing food. In Glacier, - however, they are seldom noticed as they search out seeds, berries, - and insects.] - - [Illustration: A generalized predator, the coyote will eat almost - anything, from berries to carrion. When man eliminated most of the - coyote's enemies and competitors, including the wolf, grizzly, and - cougar, it enlarged its range to fill the void. Intelligent and - social, the coyote thrives despite man's persecution. Although most - numerous in the prairie community, it ranges up to timberline.] - - [Illustration: The spruce grouse is a year-round resident of the - spruce/fir and lodgepole communities. It forages on the ground for - seeds and insects, in winter turning to needles. Several other - species of grouse occupy different habitats in Glacier.] - - [Illustration: Chipmunks are found in every community, from prairie - to tundra, in Glacier. Each of the park's three very similar species - has its preferred habitat. The diurnal counterpart to nocturnally - active mice, which have the same diet of seeds, berries and - occasional insects, chipmunks adapt easily to the presence of people - and become nuisances if encouraged by handouts. Feeding rodents is - dangerous and is harmful to them. By altering their diets and - blunting their cautious instincts, daily exposure to "free lunches" - makes the animals less fit to face the harsh realities of their - natural environment.] - - [Illustration: Unlike whitetail deer, which remain in lowland areas - all year, mule deer range upward into high meadows during the - summer. The bucks, especially, are wanderers and travel together. - Velvet antlers, worn during the time of summer sociability, presage - the autumn contests to come.] - - [Illustration: The checkerspot butterfly belongs to the most diverse - group of animals on the planet--the insects, whose importance can - hardly be overestimated. They not only help recycle nutrients in the - living community and provide an abundant food base for other - lifeforms, but are instrumental in pollinating most of the earth's - terrestrial plants.] - - [Illustration: Alpine vegetation must be able to survive freezing - temperature during the growing season, since winter conditions are - possible even in summer. Early bloomers, such as the glacier lily, - endure repeated snowfalls during the unstable weather conditions of - June.] - - [Illustration: Unlike mountain goats, these bighorn rams will desert - the alpine zone at the approach of winter; they will join other - bighorns congregating in the lower valleys.] - - [Illustration: In November bighorn sheep rams end their summer-long - isolation from the ewes, move down from the higher slopes, and begin - a bloodless but taxing ritual of strength and endurance to determine - the harem master. The sharp reports of clashing horns may carry for - kilometers, and the contests continue for weeks until the dominant - ram emerges. (Note the Many Glacier hotel complex in the valley - below.)] - - [Illustration: Hummingbirds, like shrews and other small-bodied, - warm-blooded animals, exist at the theoretical thresh-hold of life. - Because of their small size, body volume is not large enough in - relation to surface area to prevent a rapid loss of body heat. To - compensate for this, metabolic rates must be high; food is rapidly - processed and used up. Thus, since fat reserves are not practical on - such small animals, they must eat at frequent intervals. - - Two species of hummingbirds--the rufous and the calliope--are found - in Glacier. Pictured is a female rufous (which weighs about the same - as a dime) landing on its lichen decorated nest to feed its two - young on a protein-rich mixture of nectar and small insects.] - - [Illustration: The insect-eating yellowthroat prefers moist - habitats. Unlike many of its treetop-dwelling relatives, this tiny - (10-11 cm.) warbler is usually seen near or on the ground.] - - [Illustration: Bands of bighorn ewes and lambs do not summer as high - as the rams and are often encountered in the scrub-forest zone. Note - the gnarled limber pine in the foreground of this photograph taken - on the south face of Altyn Peak.] - -Reaching the mountain wall, the goats scramble upward to a ledge, -sending scree streams pouring from several clefts. Encountering a -narrow, steep snowbank, they do not hesitate but continue across the -slope. Above the rock fingers of this peak the gathering clouds grow -black. A sudden crack of thunder hurries me down the trail. - -Although geologically young, the Rocky Mountains in Glacier are composed -of soft sedimentary rocks that are easily assailed by the many agents of -weathering and erosion. If not rejuvenated by continual uplift, these -magnificent peaks will glimmer but briefly in the long memory of the -planet. - -Already the sharp countenance of this land is being softened by the -ongoing forces of erosion. Chief among these is water, which attacks the -mountains everywhere. In addition, frost action continually exploits -rock fractures, breaking down blocks of rock into talus and scree. -Avalanche and rockfall sweep down the slopes. Layers of softer rock -erode quickly, undercutting more resistant rock and creating overhangs -which gravity, in time, will collapse. - -The lashing rain catches me on this sun-and-storm-contested pass. Ice, -gravity, wind, and especially water--all attack a land that dares the -clouds. - - -The Rising of the Sun and the Running of the Deer: A Glacier Year - -As if to make up for the days-long darkness of this last blizzard, the -peaks today wear snow plumes--long, graceful trails of white, curving up -into an ice-blue sky. Yesterday the snow-mad wind raced through the -forest. Today the motionless trees are cloaked in heavy, glistening -robes, the leafless aspen and young larch bent down. - -Moderate snowfall helps many plants and animals survive the winter. For -ground dwellers it provides insulation from the wildly fluctuating -winter temperatures encountered east of the Divide, protecting the -hibernators and providing cover for the many small mammals that remain -active during the winter. Wind-swept ground freezes deep; but under a -mantle of snow life-sustaining heat is trapped, permitting many animals -to survive and allowing the work of decomposers to continue. - -But this has been a winter of too much snow and too many temperature -extremes. The heavy snowpack has forced the sharp-hoofed deer to yard up -in great numbers; unable to range freely in deep snow, they are forced -into smaller and smaller confines where their numbers allow them to -break and maintain trails. But in time they exhaust the food supply. -Younger deer, unable to reach the increasingly higher browse line, -starve first. Then the does, heavy with unborn fawns, grow weak and fall -to predators. So the imprisoned herds dwindle quickly this year, -sometimes less than a kilometer from plentiful browse. - -Deep snow is also death for many seed-eating birds. As they are unable -to scratch for food, their body furnaces quickly fail, and during a -night of cold wind their fluffed corpses drop into the snow. - -Exposed to the noon sun, the snow surface thaws; when refrozen, it is -restructured to crystalline ice. If snow repeatedly thaws and freezes, -an ice barrier is formed, shutting off vital air exchange. Plants are -then subject to rot, and micro-animal life is smothered. Travel beneath -the snow is made more difficult for mice and shrews and they are -deprived of food and cover. Under such conditions their numbers rapidly -decline. - -But while many starve in a winter of deep snow, others benefit. The -exposed traffic of small mammals is to the owl's advantage. Foxes and -coyotes more easily run down rabbits and hares on crusted snow. Deer -and, to a lesser extent, wapiti and moose--their hoofs punching through -the snowpack--swiftly tire in deep snow and become helpless before -cougar or wolf, whose lighter weight is supported by the crust. - -Grim as this winter's toll becomes, enough will survive to begin the -process of renewal in spring. Last winter, a season of light snow, was a -time of hardship for predators. The deer remained strong, the wapiti -remote on high, windswept ridges, and the small mammals hidden. - -Only the water ouzel, winter after winter, seems not to notice the -hardships of the season. Lord of his small world of open water, he sings -in February, wading and swimming his diminished stream to find a -never-failing supply of water insects and small fish. It is a voice of -spring--glad, wild, continual as the moving water--an incongruous song -in this winter-shrouded land. - -But with the growing stature of the sun, the grip of winter softens. The -firs and spruce send their loads of snow sliding to the ground. Streams -begin to sing again and soon the lakes increase, the booming of -splitting ice breaking the silence of the valleys. Avalanches thunder -down the steeper slopes, carrying trees to the swollen streams. Rivers -hiss and rage, speeding the debris along. A spring that comes too -suddenly will bring flood to lower elevations. - -Snow geese thread through the valleys, and ground squirrels tunnel up -through snow to find invasions of birds returning from the south. Soon -the three-petaled wakerobins appear, chasing the snowline up the ridges. -Glacier lilies and Calypso orchids are next, and with the shooting stars -spring arrives. - -The melting snow releases a new group of animals to populate the -winter-thinned land. Up come chipmunks. Bears reappear. Young red -squirrels, helpless and blind, squirm in their nest holes. Hidden dens -rustle with pups and kits. Soon warm days will bring them out and the -business of learning to cope with their world will begin. - -All life responds irresistibly to the growing strength of the Sun. -Cottonwood, willow, and maple come into flower and unfold new leaves; -green needle clusters spot the limbs of larches that in winter had -seemed lifeless snags among the other conifers. Beneath the soil of -prairie, meadow, and forest, in the mud of lakes and ponds, other life -stirs; armies of insects, spiders, crustaceans, amphibians, and fish -will strive to complete their life cycles against the formidable odds of -a predatory world. - -Spring reaches higher up the mountains, the lowlands passing into -summer. Wapiti and mountain sheep follow the rising tide of succulent -browse up to the high meadows. In forest, grove, and meadow and along -the stream new fledglings appear--thrush, vireo, hummingbird, waxwing, -harlequin duck, bluebird, osprey, and flicker--as holes, nests, and -cavities brim with begging mouths. - -In the alpine meadows, where snow overlaps the spring and winter follows -hard behind the summer, the growing season is short and the climate -unstable. Sensing the stronger light, flowers push up impatiently -through the snow and hasten into bloom. Pikas and marmots scurry and -sunbathe among the rocks of scree slopes. - -Summer matures in ripening huckleberries, and the bears that grazed the -spring grasses now gorge themselves fat. Dry days of August bring -probing lightning, threatening the forests with fire. - -Sweeps of beargrass reach their climax now in the highest meadows. In -dizzy succession wildflowers set seed. Fat and sluggish, marmots and -ground squirrels disappear beneath the rocks. The golden eagle must -search longer each day to find prey within its vast domain. - -Autumn lingers in the valleys and on the flanks of low ridges. The -morning sun glints on hoarfrost, firing the yellow leaves of larch, -aspen, birch, maple, and cottonwood, and shines on the blood-red berries -of mountain-ash. Soon a night of killing frost will bring down the -corpses of insects and spiders by the millions. The reptiles and -amphibians, being cold-blooded animals, seem out of place in this -long-wintered land. Unable to maintain body temperatures appreciably -above their surroundings, they are the first to seek the protection of -hibernation, collecting in dens or burying themselves beneath the ooze -of pond bottoms. - -Songbirds gather and leave the valleys. The harsh cries of jays sound -ominous now in the forest. Only the chickadees seem to ignore the long -tree shadows; their ceaseless conversations carry through the leafless -underbrush as they busily search for seed. - -Velvet has gone to bone, and in these final noon-warm days the rut runs -through the land. It begins in the valleys in September with the -joustings of deer and moose and the buglings of bull wapiti puncturing -the forest silence. By November the higher meadows ring with the -collisions of bighorn rams who compete for ewes by smashing together -their massive, curled horns. On high slopes mountain goat billies -posture and swagger; head to tail, they circle, threatening each other -with dagger-like horns. - -From Flathead Lake, 100 stream kilometers to the south, kokanee salmon -return to spawn in the clear, cold shallows of McDonald Creek. Gathering -bald eagles surround the stream, again and again lifting vulnerable fish -from pool and riffle. Perched by the hundreds along the stream course, -their white heads and tails glistening against the dark trees, they -stand out like lanterns strung for a banquet. - -Now the stinging wind comes down from the peaks and shuts the lakes. -Life slows or sleeps. Ptarmigan, snowshoe hare, and longtail weasel, all -wearing winter white, seek shelter and food in a silent land where -spring and yellow lilies seem forever lost. - - -[_] -All life faces one ultimate challenge: to survive or not, to reproduce -or fail, to bring one's kind to tomorrow's sun or vanish forever. This -land is harsh. To survive in nature demands skill in the individual, -excellence in the species, and a chance from the environment. - - [Illustration: The mink, a solitary predator associated with - low-elevation watercourses, preys on anything it can catch and - subdue.] - - - - - Plant-and-Animal Communities - - -Over Going-to-the-Sun Road - -I like to begin with St. Mary, a lake the whitecaps love to run. From -the far passes the several winds gather and collect, arranging long -lines of white waves for the race downlake. Past the purple scree of -Mahtotopa and Little Chief they go, white as the headdress of -Going-to-the-Sun Mountain, colliding, collapsing along the promontory -snares about the Narrows. Onward they press, spreading out and setting -sail for the straight rush to the final shore where a line of -cottonwoods sings with a sound like applause. - -Across the lake the timbered ridge starkly contrasts the finger of -prairie that claims the north shore. This is a flower-glad place, a -meeting-ground for mountain and prairie plants. Along the road the -grassland holds the conifers back, allowing only scattered clumps of -aspens. - -Finally, at Rising Sun, beneath the shadow of Goat Mountain, the prairie -ends and wind-seasoned Douglas-firs announce the coming forest. - -There's excitement now, with the prairie heat gone, the wind scent raw -with fir and high meadows, honed by waterfall and tall, dank rock. Our -mountain thirst is never extinguished, and a road that tightens down to -cliff face and sudden turn brings back to our blood the ancient need to -go to the highest place. - -There is sword-edged Citadel, and the snow-flanked spike of Fusillade -holding court like a queen in this valley of peaks; then the dome of -Jackson and the Gunsight notch. Our eyes are kept high, transfixed at -last by looming Heavy Runner and the distant promise of Reynolds. - -Looking for mountain goats, we scan the walls around the sweep of Siyeh -Bend, catching a glimpse of the trail that crosses the scree to hidden -Piegan Pass. - -Beargrass heads lean out above the road like old men conferring on the -view. The purple trumpets of penstemon crowd the rocks, and spots of -Indian paintbrush lead like a blood-trail to the higher slopes. - -Intoxicated now, feeling the fresh full force of the wind from Logan -Pass, we race on. We hardly notice the struggle of the forest in -Reynolds Creek far below, how it thins and loses strength in its own -hard climb. We sweep past it on the broad magnificence of this pass. - -Level but a moment, the road dips to a shelf on the headwall above Logan -Creek and swings over the great sculptured cliff of the Garden Wall. For -several kilometers this masterpiece of a road glides down a constant -grade, squeezed between rock face and space, twisting into tight -drainages--a road for storm lovers, wet with spray and snow-seep, its -quick turns concealing sudden winds. - -Mighty, snow-robed Heaven's Peak appears, taking our attention from the -Pass-group mountains and the hanging valley that spills Birdwoman Falls. -Northward is the great array of peaks encircling distant Flattop, -jumbles of mountains and glaciers. How are we to notice the forest far -below? - -Not until we have passed the Loop and are moving past the blackened -snags of a recent burn do we realize the stature of this forest. The -long road down will take us into a valley much deeper than any on the -eastern side. Near Avalanche Creek are trees we have seen nowhere else -in the park--giant western redcedars, western hemlocks with their -nodding tops, monstrous black cottonwoods with bark so deeply furrowed -that it looks hewn by hatchet. - -We take a long ride down the valley, past the low pyramid of Mt. -Stanton, final peak in the Livingston Range. Near the outlet end of Lake -McDonald, birch and aspen again appear in numbers, and the road enters a -crowded stand of lodgepole pine. - -Our memories cluttered with mountains, waterfalls, and snowfields, we do -not quite realize the significance of this 80-kilometer journey. We have -crossed the boundaries of several different plant-and-animal -communities, spanning a range of climate that would be encountered on a -5,000-kilometer north-south journey at sea level. - -At first glance the various trees, wildflowers, and animals seem -randomly distributed, scattered about like the distant mountains. But -mountainous terrain represents an organized high-rise approach to life. -From the lowest, most protected valley to the highest wind-and-ice-cut -summit, the life-forms align themselves, each according to its own -climatic tolerance. - -Here too can be seen the great cycles of nature: fire and regrowth, the -building of soil and its erosion, the incessant duel of the eaters and -the eaten. - -In the following sections we will spend some time in these various -communities, from prairie to tundra. - - -Groves and Grasslands: The Prairie Sea - -There is something about spring on the prairie that gets me up before -dawn. I like to watch the seasons change their guard over the landscape, -from the wintry cold of pre-dawn dark to the spring-scented morning air -to the hot summer-foretaste of the noon May sun. - -Hoarfrost surrounds these patches of pasqueflowers, blue goblets on -downy stems. On this windless night, frost has formed everywhere, -reclaiming for a time its vast winter range, sparkling over the green -handiworks of spring. - -But the god of the growing grasslands is the sun, and it now proclaims -itself, stretching out to make the mountains shine. With its assault the -frost collapses, becoming bright beads on grass tip and leaf joint by -which a beetle might refresh itself. - -Spring is best perceived ant-level, at its ground beginnings, where the -bright yellow-green tips of new grass shoots reclaim the winter-blighted -land. I look closely at a drag line of spider silk; a necklace of -dewdrops slides down, collects to a moment's greatness, in which I -briefly see a curved horizon, the morning sunburst, and myself, before -it falls away. - -Getting up from my prone position, my belly damp from the prairie earth, -I startle a whitetail jackrabbit; bounding high, it zigzags off. The -commotion disturbs a distant badger, which faces about from its diggings -to confront danger in whatever form it might take. It swings its snout -to scent the air. Somewhat uncertainly, it returns to the business of -hunting, then hesitates, swings about once more and waits, myopic, -patient. - -Satisfied at last, the spurt of the now distant rabbit lost in its -brain, the creature snorts a defiance at the mystery and resumes its -morning gopher hunt. - -Overhead a marsh hawk skims past, its flight erratic as a butterfly's. -Far away a magpie rattles at the passing hawk and takes flight, briefly -flashing black and white. - - -[_] -It is easy to see only pieces in the natural puzzle--a badger throwing -dirt, horned larks dipping into wind, black ants dragging the rosette of -a dead spider--and be satisfied with the scattered scenes. But at last, -to make it meaningful, we must complete the picture. There is that -special joy in discovering larger schemes: green plants utilizing -sunlight; a rabbit building its days at the plants' expense; the falcon -tearing the rabbit meat for its young; magpies picking at the fallen -falcon; and then, in the end, all returning to the earth. - -Here on the prairie, as in every plant-and-animal association, the -ancient drama repeats itself over and over; the distant tundra is a -drastically different stage with different actors, but the cycle is the -same. Life depends upon the interaction of all its many forms. Unseen -bacteria are as necessary to the land as green grass; the meadow vole -and the coyote are as much a part of the prairie as the grasses. - -The secret of life rests in the wonder of photosynthesis. Only green -plants can manufacture food from the earth's raw minerals. This is the -vital first step upon which the great pyramid of animal and plant life -is built. Using energy from the sun, green plants combine water and -carbon dioxide to synthesize sugar, and give off oxygen as a by-product. -The caterpillar takes its energy from the plant tissue, converting to -protein the sugar and minerals in its body. The caterpillar is then food -for a spider or other predator. A yellow warbler may take the spider and -in turn be ambushed by the prairie falcon. Thus the energy produced by -the plant travels through the food chain. When the prairie falcon dies, -scavengers--including insects and other invertebrates, birds, and -mammals--redistribute its wealth among themselves; the rest is -decomposed by bacteria. Thus, eventually, the nutrients on which the -plants depend return to the soil. - -When we look at any living organism, whether it is plant, herbivore, -carnivore, parasite, scavenger, or decomposer, we are soon made aware of -its associations with other living things, each puzzle piece leading us -to another and another. We begin to see a picture whole--the fox, meadow -mouse, grasshopper, bunchgrass, and sparrow hawk--all interlocked. - -Geologically speaking, grasslands are a recent development. As the Rocky -Mountains were being uplifted, the prevailing warm, moist climate began -to change. The rising mountain mass intercepted moisture-laden winds -that blew in from the Pacific, creating a rain shadow that lengthened -eastward as the mountains rose higher. A continental climate, -characterized by severe winters and dry, wildfire summers gradually took -shape, extinguishing the great forests that had grown across the -continent's interior. Herbaceous plants, which had been evolving amid -the forests, inherited the land. - -Unlike trees, grasses die back to the ground each winter, hoarding their -life-germ beneath the protecting soil. Growing not from the tip but from -the joints, grasses regenerate quickly after fire or grazing. Suspension -of the normal metabolic processes enable the grasses to go dormant and -thus survive periods of severe heat and drought. - -Although the great prairie sea washes up against Glacier's eastern -boundary, with estuaries probing into the mountain valleys on the drier, -south-facing slopes, the grassland community comprises less than 5 -percent of the land area of Glacier National Park. This includes the -puddles of prairie west of the Divide that interrupt the dense -coniferous forests along the North Fork of the Flathead River. - -From the pasqueflowers that bloom in early May to the asters and -goldenrod of September, these summer-long gardens of grasses and flowers -lean with the wind. Here are timothy, oatgrass and the -bunchgrasses--rough fescue, bluebunch fescue, and bluebunch wheatgrass. -Among the grasses bloom bitterroot, blue camas, lupine, gaillardia, -balsamroot, cinquefoil, sticky geranium, and wild rose. - - _continued on p. 68_ - - [Illustration: The Forests of Glacier - - From the lush redcedar-hemlock forest in the McDonald Valley to the - subalpine fir, whitebark pine, and Engelmann spruce struggling for - existence near treeline, the forests of Glacier reflect the - conditions of temperature, exposure, soil, and drainage prevailing; - and each forest has its characteristic association of understory - trees and shrubs, herbaceous ground cover, and vertebrate and - invertebrate animal life.] - - [Illustration: Life Zones - - Many physical and climatic factors determine the range of Glacier's - plant-and-animal communities. Boundaries between communities are - seldom sharply defined, but rather merge together in broad zones of - transition. - - With elevation gain, average daily temperature drops at the rate of - 5 per 900 meters. Precipitation, wind velocity, and evaporation - loss increase. Soil thins. These factors, along with others such as - fire frequency, north or south exposure, and availability of - moisture, combine to determine the range of each community. - - In the forest community below 1,800 meters, Douglas-fir, lodgepole - pine, and western larch predominate. In the valleys, Engelmann - spruce and subalpine fir are found. The somewhat lower and much - better watered western valleys of the park support western redcedar - and western hemlock. - - Treeline is the upper limit to which the tolerances of trees to - environmental conditions permit them to grow. Because there are so - many controlling factors (wind, temperature, exposure to sunlight, - snow cover, etc.) treeline in the diagram is only approximate. In - Glacier it averages 2,000 meters. Avalanche chutes or sheer cliff - walls may suppress it to below 1,500 meters; on protected slopes it - may be as high as 2,150 meters. - - At the eastern edge of the park below 1,200 meters, the forest gives - way to the prairie community, composed mostly of soft-stemmed plants - adapted to the conditions of low precipitation that prevail here in - the rainshadow of the mountain range. Clumps of aspen, found in the - prairie in sheltered spots, occur here in the transition zone - between prairie and forest.] - - [Illustration: A Mountain Profile - - This diagram represents the eastward-facing slope of a hypothetical - mountain near the eastern boundary of Glacier National Park. Its - life communities are somewhat different from those of mountain - slopes at the western edge, chiefly because of the differential in - annual precipitation. - - Illustration: Here, above approximately 2,750 meters, in a realm of - ice, snow, and barren rock, there is little life. - - Alpine tundra - - Below 2,750 meters and above 2,000 meters, depending on other - factors such as exposure to sun and wind and steepness of terrain, - exists the alpine tundra community, with vegetation similar to that - of the vast, essentially level, treeless zones of the Arctic. - - Scrub-forest - - Roughly between 1,800 and 2,000 meters, the dominant vegetation is - scrub-forest. Trees here are stunted; except in sheltered spots they - are more or less prone rather than upright. Net growth is slow, not - only because of the short growing season but also because of the - pruning effect of icy mountain winds. Very few tree species can - survive in this harsh habitat. - - Coniferous forest - - In the forest community below 1,800 meters, Douglas fir, lodgepole - pine, and western larch predominate. In the valleys, Engelmann - spruce and subalpine fir are found. The somewhat lower and much - better watered western valleys of the park support western redcedar - and western hemlock. See page 54 - - Prairie - - At the eastern edge of the park below 1,200 meters, the forest gives - way to the prairie community, composed mostly of soft-stemmed plants - adapted to the conditions of low precipitation that prevail here in - the rainshadow of the mountain range. Clumps of aspen, found in the - prairie in sheltered spots, occur here in the transition zone - between prairie and forest.] - - [Illustration: The Forest Community - - A forest is organized vertically like an apartment house or office - building, with layers corresponding to stories. The _canopy_ is the - branches and foliage of tall trees that form a roof over the - community. Below the canopy are the _understory_ trees: young - individuals of the canopy species; and small, shade-tolerant trees - that will never become part of the canopy. Beneath the understory - branches is the _shrub layer_, occupied by knee-high-to-man-high - woody plants; beneath that is the _herb layer_, where most of the - ferns, wildflowers, grasses, and smaller woody plants grow. The - _forest floor_ is the zone of mosses, mushrooms, creeping plants, - and forest litter (leaves, twigs, needles, feathers, bits of bark, - animal droppings, etc.). The forest has a "basement," too, - interlaced by plant roots, mycelia of fungi, and tunnels of myriad - animals. - - Each layer of the forest has its characteristic animal species, but - most forage over more than one level. Some nest in one story and - feed in another. The red squirrel races back and forth from the - forest floor to the highest branches. - - The forest community also has a socio-economic organization. Every - animal (and plant) takes up space and consumes a portion of the - available nutrients. Each has a place in the community food - chain--as, for example, _herbivore_, _carnivore_, or _scavenger_. - Each directly or indirectly affects all the other organisms. - - The Forest Community - - The role of a species in the community, like the job and social - function of a person, is its _niche_. Similar species of animals - have different niches, thus lessening competition for food and - living space. Thrushes hunt close to the ground; vireos and kinglets - hunt among the branches; flycatchers snap up airborne insects. The - flicker feeds upon insects, excavates nesting holes that are later - occupied by other species such as squirrels and owls, and is preyed - upon by the great horned owl; its niche is _insect exterminator / - food for carnivores / homebuilder_. The great horned owl, hunting - mammals, birds, and reptiles by night, preys on species different - from those hunted by the goshawk, and thus occupies a parallel - niche. When it dies, its remains, like those of other animals, are - decomposed and return to the soil.] - - Canopy - Great Horned Owl - Yellow-bellied Sapsucker - Understory - Flying Squirrel - Shrub Layer - Ruffed Grouse - Herb Layer - Red Squirrel - Western Toad - Forest Floor - Shorttail Weasel - Scavenging Insects - Deer Mouse - Garter Snake - Soil Layer - Ground Squirrel - Earthworm - Masked Shrew - - [Illustration: Sun, Green Plants, and Animals - - The sun is the source of energy for any plant-and-animal community. - Green plants draw nitrogen and minerals from the soil, and in a - process called photosynthesis use sunlight to convert raw materials - (carbon dioxide and water) into carbohydrates (sugar, starch, - cellulose), giving off oxygen as a by-product. Besides burning - oxygen, animals depend on plants for food. - - Green Plants, trees and shrubs, grasses and sedges, wildflowers, - ferns, mosses, algae and lichens--are fed upon by animals, which are - unable to manufacture their own food. - - The Redback Vole, like other rodents, pikas and hares, seed-eating - birds, grazing and browsing hoofed animals, and herbivorous insects, - derives its energy from the seeds and other parts of green plants - that it eats. - - The Garter Snake, feeding upon the vole, is dependent upon plants - even though it does not eat them. - - The Great Horned Owl, preying upon the garter snake, is one more - step removed from the green plants--but still dependent on them. - - Scavengers such as carrion beetles feed upon the carcass of the owl; - the remains are then attacked by Decomposers, primarily bacteria, - that break down the animal tissues into basic organic compounds. - - The Soil, enriched by the minerals and carbon and nitrogen compounds - added to it by the decomposers (and by other processes such as fire) - supports new green plant growth. - - Thus energy derived from the sun flows through the ecosystem in a - food chain. A plant-and-animal community is a complex, interlocking - web of such food chains.] - - Sun - Green Plants - Redback Vole - Garter Snake - Great Horned Owl - Scavengers, Decomposers - Soil - - [Illustration: A Pyramid of Numbers - - Necessarily, the number of plants in an ecosystem far exceeds the - number of plant eaters, and the number of prey species must exceed - the number of predators. During its lifetime, a golden eagle will - consume a vast number of lesser animals. The combined mass of prey - animals necessary to sustain an eagle greatly outweighs the eagle - itself. Ecologists refer to this proportional relationship of mass - between each link in the food chain as the _pyramid of numbers_. - - The diagram represents a numbers pyramid for the alpine zone. - Because of its limiting environment, the alpine zone supports a - lesser plant mass than the forest zone. As a result, the carrying - capacity of the alpine is less than that of the forest. - - 1 Kilo - - _Tertiary_ (third-order) _consumers_ are the predators (Golden - Eagle, Swainson's Hawk, etc.) that feed upon other predators. - Because of the 90% loss of energy at each level of the food chain, - there will be very few hawks and eagles in comparison to the numbers - of marmots. - - 10 Kilos - - _Secondary consumers_ are the predators (weasels, shrews, - carnivorous insects and birds, etc.) that eat herbivores. The - animals at this level of the pyramid are often--though not - always--larger than the animals they feed upon. But they are much - less numerous, because it takes many prey animals to sustain one - predator. - - 100 Kilos - - _Primary consumers_ (plant eaters, or herbivores) convert plant - tissue into animal flesh. In the process about 90% of the energy - stored as plant food is lost, mostly as heat energy. In the alpine - community the herbivores include pikas, marmots, ground squirrels, - and ptarmigan, as well as herbivorous insects. - - 1,000 Kilos - - _Producers_ are the green plants at the base of the food pyramid, - manufacturing food for the animals of the alpine community. The - _biomass_ (total weight) of each level of the food chain is ten - times (more or less) the weight of the stage above it: 1,000 kilos - of green plants will produce only 100 kilos of primary consumers.] - - [Illustration: Great horned owls are the nocturnal equivalent of - Cooper's hawks and goshawks in the low-elevation forests of the - park. Large and powerful, they are capable of taking prey as big as - skunks. This young bird, disturbed on its day roost, clacked its - bill and fluffed its feathers in a menacing manner.] - - [Illustration: The only sizable mature stand of ponderosa pine found - within the park is along the North Fork truck trail. A scattering of - old ponderosas growing at the lower end of Lake McDonald suggests - that at one time ponderosa forests were more extensive in this - region than at present.] - - [Illustration: A black bear near treelimit. Bears will eat almost - anything, from ants to carrion, grass to garbage. Color phases - include brown and blonde bears. Unlike the larger, more aggressive - grizzly, which ranges out onto the plains, black bears are strictly - forest creatures.] - - [Illustration: The water ouzel, or dipper, a creature of fast - mountain water, is admirably outfitted to cope with its demanding - environment. Stubby wings, chunky body, short tail, and oily plumage - allow it to walk under water, where it scavenges for aquatic insect - larvae and small fish. In flying up- and down-stream, ouzels never - shortcut but follow the winding streamcourse. - - As long as there is open water, the dipper suffers no hardship from - the mountain winter. Then, when the land is shut down and lakes are - frozen over, this little bird carries on in its mountain-stream - habitat, plunging into the cold water to find food, and pausing - occasionally to sing.] - - [Illustration: Ouzels construct their nests of living moss on cliff - faces or ledges where constant spray keeps the moss moist. At - fledging, the four young of this nest in Avalanche Gorge tumbled one - by one into the torrent below, to be collected by the adults in - quieter water downstream. Within a day they appeared to have - mastered the underwater gymnastics and were feeding on their own.] - - [Illustration: From their lowland wintering grounds, wapiti move up - to higher elevations in spring. Summer range in the park is - abundant, but winter range is limited; as a result, wapiti have a - tendency to increase their populations beyond the carrying capacity - of available winter range. In a severe winter many starve. But in a - balanced ecosystem such loss is not waste, for the carrion helps - sustain scavengers; it is an important initial food source for bears - emerging from hibernation.] - - [Illustration: Cedar waxwings nest in moist areas of low valleys - where fruits and berries are abundant. Although they also subsist on - insects (which they can capture on the wing), their weakness for - fruit is so pronounced that the birds will sometimes gorge - themselves until rendered incapable of flight.] - - [Illustration: The Columbian ground squirrel is found at all park - elevations, from prairie to alpine meadow. Hibernation occupies - almost three-quarters of its five-year lifespan. Unlike other park - ground squirrels, it lives in colonies. Although not as tightly - structured as a prairie dog town, the association is beneficial to - all members in that danger is readily detected.] - - [Illustration: The tundra community is encountered above Preston - Park on the Siyeh Pass trail. Mt. Reynolds, a classic example of a - horn, dominates the distant Logan Pass area.] - - [Illustration: Camas blooms in the prairie community along the Red - Eagle road. An important staple, camas bulbs were gathered as food - by Indians.] - -Conspicuous also are many insects--including grasshoppers; flies; ants, -wasps and bees; butterflies and moths; bugs; and beetles--which fulfill -important roles as herbivores, carnivores, and scavengers while also -acting as pollinators for flowering plants and providing an abundant -food source for other animals. - -Below the ground are the tunnels. Burrowing is an important means of -survival on the open prairie, and life underground is extensive. Some of -the animals are rarely seen--the northern pocket gopher, for example, -with a diet of underground insects, grubs, worms, and roots, spends most -of its life tunneling just below the surface. Others, like the badger, -leave their burrows during the day to dig for rodents. Most conspicuous -of the burrowing animals in the park's grasslands is the Columbian -ground squirrel. Its alert upright stance has earned it the nickname -"picket pin." When danger approaches from the air or on land, its shrill -alarm whistle passes the warning to others of its kind. - -Where prairie and forest meet, a never-ending struggle for dominion is -waged. The isolated patches of prairie that dot the North Fork Valley -near Polebridge hold the great forest of the park's northwest region at -bay. - -This broad valley, floored with coarse glacial outwash and terraced -downward to the deep channel of the North Fork River, presents a graphic -battleground between grass and tree. Lining the upper terraces, from -which they glower down on the dry, well drained grass flats like a line -of warriors, are the Douglas-fir, western larch, and ponderosa pine. -Seedling trees continually invade the prairie. But most perish early, -their shallow roots no match for the extensive root systems of the -fast-growing, moisture-greedy grasses. If encouraged by a series of wet -summers, however, the young lodgepoles quickly gain stature. They had -made significant inroads at Big Prairie when the disastrously dry summer -of 1967 killed most of these 15-year-old pioneer trees. - -These North Fork grasslands and the immediately surrounding lodgepole -pine forests are an important spring range. Deer, wapiti, and -grizzly--and, in the wetter areas, moose--graze or browse here. And -here, low on the western slopes of the Livingston Range, are the park's -only stands of ponderosa pine, a tree that prefers warm, dry habitats. -As a result, at low elevations it often merges with the prairie -community. - -Groves of aspen colonize the eastern prairies in areas where there is -sufficient water and protection from wind. These aspen parklands are -important havens for animals. Wherever two differing communities -interact, a phenomenon known as "edge effect" occurs. Here wildlife -exists in abundance; the animals that favor forest cover mingle freely -with those that prefer open areas. Aspen groves--supporting grasses, -herbs, and shrubs beneath their thin canopies--are favored haunts for -grouse, varying hare, deer, and wapiti, all of which find among the -trees abundant food, shelter and concealment. Populations of insects, -small mammals, and birds, which are high for the same reasons, attract a -wide range of predators. - -Isolated aspen groves are characteristically dome-shaped. Because aspens -are capable of reproducing themselves vegetatively, the grove slowly -expands outward from the parent tree. As a result, most of these groves -are either exclusively male or exclusively female. - -Since quick-growing aspens provide a bountiful food source for beaver, -streams near these trees are often dammed by the rodents flooding -lowlands and creating additional habitat in the form of willow flats. -Another "edge effect" is established, attracting animals found near -water. Waterfowl, marsh birds, moose, mink, muskrat, skunks, amphibians, -and many others find such areas to their liking. - - -[_] -Before the appearance of the white man, these eastern prairies were a -paradise for animals. Once, on the summit of Rising Wolf, light-headed -from the climb and the view of endless prairie, I fancied that I saw -that vast, undisturbed animal panorama spread before me. - -Principally there were the bison, darkening the uneven land. Pronghorn -bands flashed white on ridgetops, and moose moved through the long -fingers of willow that extended eastward with the rivers. Caribou and -wolves inhabited the shadows. Among vast cities of prairie dogs, swift -fox and grizzly roamed. There were the clamorings of sandhill crane, and -white clouds of trumpeter swans. - -This land, endowed with a wealth of wild grass, wore its wilderness -well. - - -The Forest - -On Gunsight Pass, the rain lancing down, I found a sharpedged rock that -split the continent in two. On both sides the rain rivulets ran down, a -fraction of an inch determining the stream's destination: Pacific or -Atlantic. - -The Continental Divide is a mighty barrier, a line of consequence that -does more than determine watersheds. Its effect in Glacier is dramatic, -as a look at the forests will reveal. - -Obstructing the eastward flow of the moisture-laden Pacific winds, the -Divide extracts a heavy annual tribute of precipitation from the air -mass, forcing it to rise up the mountain chain, where it cools and -condenses. Chief benefactors are the low western valleys, which respond -with a lush growth of Pacific coastal-type forests. - -The eastern valleys, however, deprived of abundant annual moisture and -exposed to the wind and temperature ravages of the prairie's continental -climate, support a dramatically different kind of forest. Here Engelmann -spruce and subalpine fir are the climax trees, contrasted with such -trees as the western redcedar and western hemlock of the mild and moist -McDonald valley. - -Elevation exerts an additional restriction on the distribution of tree -species. Since climatic conditions vary with change in elevation--lower -temperatures resulting in shorter growing seasons, and increased wind -exposure resulting in greater loss of moisture through evaporation--we -would expect to find the forest composition change as we ascend a -mountain slope. In Glacier, eastern valleys average 240 meters higher -than western, and thus even if they had more moisture they would not -sustain the redcedars and hemlocks. All plants have range limits, some -narrow, some broad; and they excel where their particular set of -preferences as to moisture, soil, sunlight, and wind exposure are best -met. On sites that do not meet their optimum requirements, they face -being crowded out by species better adapted to the prevailing -conditions. - -Physical features of the land determine vegetation also. Certain trees -prefer the moist areas along a streambed--the great black cottonwoods, -for example. And on steep hillsides, avalanches prevent the growth of -climax trees, permitting instead only shrubby, pliant -growth--mountain-ash, mountain maple, alder, menziesia. - -Forest communities are named for their dominant tree species. Thus, an -area in which Douglas-fir dominates is called a "Douglas-fir forest." -Glacier does have forests in which Douglas-fir is the climax species; -these are chiefly dry areas, below 1,800 meters, with south and west -exposures. But we usually associate the park with its Engelmann -spruce-subalpine fir forests, found extensively between 1,200 and 2,100 -meters, and with the western redcedar-western hemlock forests in the -McDonald valley. - -Because forests mature slowly and change is usually imperceptible, we -are tempted to think of them as static and eternal. But since a forest -is a community of living things, it responds to changes in the -environment. Subtle physical or climatic changes, such as a rising or -falling water table or a slight increase or decrease in annual -precipitation, will favor some species of trees and hinder others, -eventually altering the composition of the forest. - -Other changes are more dramatic. Most notable of these is fire. - - - From Fire to Forest - -Heat lightning, glimmering soundless behind the western peaks. Then the -first low rumble. At first the flashing had been from cloud to cloud, -but now, as the storm nears, the first ground-spears appear, lighting up -the night. Here is a big storm, many-celled, engulfing more and more -territory beneath its angry bulk. Lightning dances into the dry August -forest. In their towers the lookouts stay awake. - -Close strike and a flare-up! The ridge snag burns like a Roman candle, -sending bright embers down. Valley, ridge, and peak blink on and off -with blue light as the storm roars like night-firing artillery. - -Passing overhead, the low cloud belly brings a sudden lash of rain. But -it is not enough: tomorrow will mean long hours of fire watch. - -The next day dawns clear, a morning of heavy dew. The ridge strikes did -not ignite the forest. Inspecting the storm path, aircraft and lookouts -find no evidence of fire. - -But two days later, in a morning of high wind, thin smoke plumes rise -upward. Smoldering in the thick duff of the forest floor, a lingering -hot spot explodes with the fanning wind. It quickly spreads from a -hectare to ten while the quadrants are called in and the hot-shot crews -dispatched; then to a hundred, bringing in the smoke jumpers and -mobilizing the vast fire-control network. A thousand hectares, perhaps -ten thousand might burn this week of big fires. - -In the resulting skeleton forest, the scene of devastation is almost -overpowering: life seems forevermore excluded from this blackened ruin. -But fire is nothing new to forest communities. We may think fire demonic -because it takes from our life span this block of mature forest, a sight -we will never again see in this place. But nature does not operate in -terms of human time scales. This forest is simply pushed back closer to -its starting point, to begin again its long progression toward a climax -vegetation cover. - - - Forest Succession - -Through a series of complex vegetation stages, each characterized by -different herbs, trees, and shrubs, the forest slowly returns to the -type of vegetation best suited to the physical and climatic conditions -of the site; this is called a climax community. The fact that most of -Glacier's forests are in some stage of recovery from fire accounts in -part for the mosaic of forest cover found here. - -The forest of Huckleberry Mountain on the Camas Creek road was consumed -in the 1967 fire. By 1969, among the charred, lifeless trunks of the -former forest, lush grass and sunloving fireweed, thistle, and -paintbrush were growing. And by 1974 lodgepole pine seedlings along the -road were a meter or two high. Lodgepole is a fast-growing tree that -requires full sun to germinate. Forest fire is necessary for the -regeneration of these trees: the intense heat causes the tightly closed -cones to open, releasing the seeds that will establish the forest. So -young pines developed among fireweed, spiraea, willow, and mountain -maple shrubs. - -The lodgepole forest near the western entrance to the park has been -developing since 1929, when fire destroyed the redcedar-hemlock forest -in the area between Apgar and West Glacier. Beneath the scattered spires -of old larch that survived the burn, the lodgepoles have now grown up, -forming a canopy that shades the forest floor. Because lodgepole live -only about 80 years and will not germinate in shade, this forest will -not exist long. Shade-tolerant Douglas-fir, white pine, Engelmann spruce -and western redcedar seedlings are now taking hold. But the physical -characteristics of this area--the climate, terrain, and soil--are -ultimately most favorable for western redcedar and hemlock; and unless -other disruptions intervene, this area will eventually again become a -dense redcedar-hemlock forest. - -But this will not happen quickly. The soil after hundreds of years of -collecting debris will again become rich and moist. Young hemlocks will -germinate on and near decaying logs. When old larches, firs, and pines -fall, the slow-growing redcedars and hemlocks will take their places in -the canopy. - -Forest succession is a more complicated story than this; it is a -fascinating study involving herbs, shrubs, small and large trees, and -animal populations. From location to location it will vary; only in its -broad outlines is it predictable. It is based on the observation that, -given time, a forest--or any other plant community--will progress until -it reaches climax--that is, the stage that will perpetuate itself. - - -[_] -How then are we to think about fire? Increasingly, experts are concerned -not so much with fire suppression as with fire management. For -suppression has at least three disadvantages: it allows the accumulation -of unburned fuels that can result in "fire storms" when they are finally -ignited; an undiversified climax forest is more vulnerable to disease -than is a mixed forest; and a dense forest canopy discourages shrub -growth, an important food source for deer, wapiti, moose, and smaller -animals. - -As the well-being of the deer herd depends on the predators that thin -its numbers, so the long-term well-being of the forest depends on fire -to rejuvenate it periodically. We must realize that wilderness is -identified with fire, landslide, avalanche, windfall, and flood. Nature -not only has learned to cope with these agents of change--she depends -upon them for maintaining the delicate balances between landscape and -life. There is in the business of nature, after all, more than the -pleasing of man's eye. - - - Spruce Morning - -Of all times to get a rock in my boot! I had just started out, the -morning was still cool in this eastern valley, and the heavy pack was -not yet biting into my shoulders. Sitting down beside the trail, I -leaned the pack against the base of an old spruce and began unlacing. - -I could hear the scratching of the red squirrel descending to -investigate, but I didn't look up until it let go with long indignant -chatter at finding its territory invaded. I plunked out the pebble and -began relacing my boot. Cautiously the squirrel came down, pausing -frequently to scold, its lower jaw quivering with rage and exposing -yellow rodent teeth. Neighboring squirrels joined in and soon the trees -danced with flicking tails. - -Down the squirrel came, almost to the ground, then raced back up the -tree, stopping at each lateral branch to deliver a vocal broadside. -Finding no danger to themselves, the other squirrels soon quit the -uproar and went about their morning business. I was beginning to suspect -that I was committing some graver offense than the mere exercise of -squatters' rights--perhaps I threatened its cache of fir cones. Then -into the corner of my vision shot another form, streaking soundless as a -shadow; the squirrel also saw it--but too late. With a thin terrified -squeak, the rodent started to go higher; but the pine marten was above -it. The squirrel quickly reversed itself, sending bits of bark showering -down. - -As the squirrel leaped from the tree in desperation, the marten overtook -it in mid-air; they came down together. Clamping the limp creature -firmly in its jaws, the marten strode up the incline of a fallen spruce. -Before it hopped off onto a shelf of higher ground to disappear, it -looked briefly back at me. I fancied I could read, fixed in its eyes, a -certain recognition of my having distracted its prey. - -A breeze made me shiver, snapping me back from that swift vision of -luxuriant fur, that blinding grace which flashed its orange throat-patch -through the trees, and I realized I was sweating. For a moment I had -been that squirrel, eyes wide with terror, seeing fate bear down, and -powerless before the natural order of things. - -The incident got the other squirrels singing again; but the confidence -was gone, and soon it was quiet. What dreams do squirrels dream, I -wondered, looking around. I saw that place more clearly then, having -been caught between a marten and its prey. I saw each spruce: its age, -its condition, the onslaughts it had borne; the beargrass coming up in -an opening; and down the trail a meadow that was yellow, white, and red -with sulphur plant, mariposa, and Indian paintbrush. Bees, flies, -spiders, and butterflies worked that little garden tucked among the -crowding trees. Countless forms of life beneath the soil and bark, in -tunnel, crevice, hole, and pocket, working unseen to sustain their -lives, and somehow, when all were added up, maintaining the forest as -well. - -A flicker called, its loud _Klee-yer_ breaking the forest hush. Birds, -mammals, plants, insects--all hide together here, their lives so -skillfully embroidered that no loose thread exists that my mind might -grasp to unravel and understand the work. - -The forest had once been a place that obstructed my view, a great blank -to stride through, a few hours of necessary blur before the high lake or -pass was reached. Now I was quite content to remain awhile beneath these -great-boled trees. - - -[_] -A forest, like the mountains themselves, supports various levels of -life. The floor and substratum are a great processing plant where -bacteria, fungi, and insects work, decomposing the plant and animal -litter, recycling dead and discarded tissue back to simpler organic -compounds, gases, and minerals, thereby providing sustenance for growing -plants. As spiders, shrews, wrens, and thrushes seem to know, there is -good hunting on the forest floor. - -Just above the forest floor is the herb layer, a seasonal layer of -growth including flowers, mushrooms, grasses, and other small plants. - -Above that grows the shrub layer, then the understory of young trees -awaiting their chance to take a place in the forest's canopy high above. -From the swaying canopy, exposed to the full force of sun and wind, to -the dim, moist floor, the forest provides a wide range of habitat. - -Relatively few animals live in the treetops. The almost incessant motion -makes nesting too hazardous for birds. Red squirrels venture up to cut -cones in the canopy, but store their booty and make their nests farther -down. - -In the mid-range between canopy and understory, goshawks and Cooper's -hawks nest. Woodpeckers, nuthatches, and sapsuckers forage on the tree -trunks and nest in cavities they excavate or appropriate. Red squirrels -and the nocturnal flying squirrels create a major traffic here, along -with the martens and owls that hunt them. - -The understory and shrub layers house the greatest numbers of nesting -birds. Here the effects of storm and rain are minimized and protective -cover is greatest. Vireos, thrushes, warblers, hummingbirds, bluebirds, -flycatchers, and others can be found among the tangle of this sometimes -impenetrable layer. - -The most populated area, the forest floor, supports an astonishing -abundance of organisms. Below the busy traffic of mice, shrews, and -larger animals is a bewildering array of insects and other -invertebrates. The attrition rate in the litter of the forest floor--a -continual battleground difficult to comprehend--is enormous. The smaller -the organism, the greater its numbers are likely to be. This humus-rich, -moist soil teems with bacteria, and a handful will contain surprising -numbers of small spiders, pseudo-scorpions and almost microscopic mites. - -Each year some two to three thousand kilograms, dry weight, of falling -material litter an average hectare of forest. All this plant and animal -waste--twigs, leaves, limbs, fallen trees, feathers, hair, feces, and -carcasses--is processed by the armies of decomposers that thrive on the -forest floor. With the aid of larger creatures that break up the plant -and animal tissue, most microscopic bacteria are able to decompose from -a hundred to a thousand times their own weight every day. - -Few trees die of old age in the forest. The seedling mortality rate is -necessarily high, since far greater numbers of seeds germinate each year -than can reach maturity. Of those that do, many fall victim to the -ever-present dangers of disease, insect infestation, windfall, stream -erosion, and fire. Insects alone present a formidable threat to trees, -for they have evolved every means of attack--chewing and mining leaves, -boring into twigs, eating cambium and heartwood, sucking sap, triggering -galls. If the insect world did not police itself, aided by spiders, -insectivorous birds and other animals, forests and other plantlife would -quickly fade before the chewing, boring, sucking horde. - - -[_] -Through the trees the light on Citadel shows the morning slipping by. As -I start to get up I see a garter snake sliding out into the dusty trail, -seeking the sun-warmed earth. Moving slowly, alert for danger, it probes -the air frequently with its sensitive tongue. But against the -lightcolored duff its dark shape offers a fine target, begging attack. A -chipmunk, watching from a nearby lookout stump, twitches its tail -nervously over its back, curious--perhaps suspicious--at the sight of a -snake. Very slightly the snake's head goes up, its tongue flickering. -For a few seconds reptile and rodent regard each other. Then the -chipmunk drops back soundlessly into its hollow stump, and the snake -lowers its head onto warm ground. - -Some day soon, a sparrowhawk or weasel will interrupt the snake's -morning sun-bath. The snake will fuel bird or mammal for a time, as -mice, fledgling birds, and insects now sustain the snake. The chipmunk -too, rummaging nearby, lives in shadows of talon and tooth. - -Until that time of sharp encounter, each has its own niche, a way of -life, a shaft of sun, and food enough. - - - A Walk in the Redcedar Forest - -Climax! The word takes on a true significance here, among these -broad-based trees. When you enter this forest the road noise does not -follow far--as, when you walk into a cave and turn a corner, sound and -light are left behind. There is a surprising spaciousness, a feeling of -openness in a mature western redcedar forest. With scant understory and -the canopy so far above and everywhere complete, it seems like some -vast, high-ceilinged catacomb, pillared by the huge, shaggy-barked -cedars and the deeply scored trunks of the black cottonwoods. The floor -is strewn with fallen giants in magnificent disarray, uplifted roots -still grasping fractured rock. - -A rainy day is a good time to walk a cedar trail, when the dull light -seems to shine from the wet moss, making the underleaves of devil's-club -and Rocky Mountain maple glow. Wind and rain, like light, penetrate with -difficulty the latticework of this canopy; thin lines of fog develop -over the bogs. The air is fresh with growing plants, snow-cold still -when the first spring flowers appear. - -Fiddleheads of unfolding lady ferns line the trail in May, pushing up -from the hub of last year's leveled, lifeless fronds. Beds of trillium -shine their white, three-pointed flowers like flashlights in the dark -recesses. Unlike the small, hidden calypso orchid, which bears its -purple spikes and yellow throat low above the moss, the trilliums make -no secret of spring growth. They are bold, handsome plants, broad-leaved -and tall, with waxy white petals that tinge to purple in their -month-long bloom. - -Moss covers everything. Boulders are green and weightless-looking, -resilient and topped with miniature forests of cedar seedlings. Ancient -fallen trees are disguised with blankets of moss, sprouting hemlock here -and there. The rich greens that characterize Glacier's summers seem to -begin here amid the moisture-glossed leaves of twinflower, bunchberry -and bead-lily. - -Later, the spiders will spin thousands of kilometers of gossamer -filament among the trees. The orb-weavers will hang their webs high and -low, suspended in every opening. Walking through the forest then, you -will see shafts of sunlight whirling in the higher webs until they seem -like tops set spinning among the treetrunks. - -Indianpipes, the "ghost flowers" that need no light to grow, will break -through the forest soil. Like mushrooms, with fruiting bodies that are -nourished by underground mycelia, these saprophytes absorb their -nutrients from a fungus that covers their roots. - -Receiving an average of about 18 centimeters more annual precipitation -than forests east of the Divide, Glacier's redcedar-hemlock community -hoards its moisture. Its dense growth and the surrounding mountain walls -inhibit the circulation of drying winds. Mosses and ferns transpire -their moisture, which you can feel; place your hand close, and you will -sense a coolness like the air exuding from an ice cave. Draped from the -tree limbs are long filaments of squawhair and goatsbeard, black and -grey lichen strands that flourish in the damp air. - -Except for the black bear, few large animals inhabit the deep forest. -Grizzlies find better forage in meadows or along the forest edge. Since -shade discourages shrubby undergrowth, deer and wapiti will search -elsewhere for browse. In summer, wapiti, grizzlies, and mule deer bucks -tend to wander up into high meadows. - -Contrasted to the noisy, conspicuous birds of the prairie--meadowlarks -and bobolinks--birds of the forest seem elusive and secretive. Although -numerous, the varied thrushes, Townsend's solitaires, and Swainson's -thrushes are seldom seen; but when approached, they fly silently off and -are swallowed by the forest shadow. - -There seems to be serenity in a mature forest, as though the struggle -for life is somehow suspended, the needs of the animals here less -urgent, muffled. The towering redcedar forest seems to be no battlefield -at all, but rather a monument to what Earth can do. - - - The Perpendicular Night - -Behind Avalanche campground a trail leads back toward Lake McDonald -Lodge. I decided to follow it one June evening, to experience the -sensation of the deep forest changing into night. With the nearby -mountain wall intercepting the sun, dusk comes early to this valley. On -the prairie, night passes across the landscape in an even line, -forthright as a waxing tide; you can almost feel the globe in its -turning from the sun. There is reassurance in the night's coming, its -steady purple doming over the sky. - -But here darkness seems to sprout from the earth. It collects beneath -the hemlock clumps, bridges the creekbottoms. It seems to flit from -place to place. You look about, uneasy, trying to catch it here or -there, but always miss its infiltrations. It captures the narrow -clearings when you look away; pockets of tree-darkness join together, -forcing the light upward until the tree-tops seem impossibly bright and -distant. - -Through the trees I could see a dozen fires dance in the growing shadow, -wood-smoke and camp sounds filling the air. Turning uptrail, I felt a -reluctance to leave the presence of those fires--a senseless feeling, -but strong. A growing forest-dread impelled me almost physically -backward to those circles of firelight. I felt the need to be near a -fire, to be reassured by heat and light. Fire was our greatest friend, -our greatest weapon. With it we beat the long ages of ice and held the -forest gloom away. There was no harm here, only silence; yet the longer -I walked, with beard-moss hanging down like daggers all around, the more -I craved the comradeship of fire. - - _Continued on p. 104_ - - The Vital Predator - - The merciless law of predation might at first thought seem cruel; - but the predator plays a vital part in maintaining the balance of - the biotic community. Without the controlling factor of predation, - prey species quickly enlarge their populations. If plant eaters are - not checked, the resulting excess population exceeds the carrying - capacity of the range. Food supply rapidly diminishes. In a damaged - range, competition and stress result, usually culminating in a - massive die-off through starvation and disease. - - Ironically, predators thus provide a service to their prey. First to - fall to the predator are the old, the diseased, the unwary, and the - young. By removing many young and old deer from a typical herd, - cougars lessen competition among the deer for choice range, thus - tending to keep herbivore numbers at parity with the land's carrying - capacity. Only the strongest and wariest deer survive, ensuring that - the fittest will continue the species. When man upsets this delicate - balance--destroying predators in the hope of increasing numbers of - game animals--the result is ecological disaster. In the 1930s, in a - misguided attempt to "preserve" the whitetail deer herds of the - park's North Fork area, many coyotes and cougars were exterminated. - In 1935 alone, 50 cougars were killed. Relieved of the pressure of - predation, the deer flourished. In a few years, however, the - normally adequate range was severely overbrowsed. Suffering also - from this imbalance were wapiti ("elk") and moose, ungulates that - share the winter range with deer. - - Some predators are more specialized than others. The Canada lynx, - for example, has oversize feet, an adaptation that helps it move - across deep snow without breaking the surface. As a result, it is an - efficient predator of the snowshoe hare, another large-footed - animal. Relying on this adaptation, the lynx feeds almost - exclusively on snowshoe hares. Consequently, its numbers inevitably - fluctuate with the 10-year "boom and bust" cycle of the snowshoe. - - The coyote, on the other hand, is a generalized predator, exploiting - whatever prey is currently abundant. Should mice or ground squirrels - be in short supply, it will subsist on anything from grasshoppers to - berries until favored prey again becomes available. (Animals that - normally eat both plant and animal food are referred to as - omnivores.) Generalized predators are thus better equipped to - survive temporary ecological imbalances, maintaining their numbers - at relatively consistent levels from year to year. - - Carnivores all, the animals on these pages illustrate various - adaptations for capturing prey. - - [Illustration: The population of the Canada lynx, which is widely - distributed in Glacier's coniferous forests, fluctuates in cycles. - The lynx is abundant or scarce depending on the population condition - of its chief prey, the equally cyclic snowshoe hare.] - - [Illustration: The cougar, which feeds primarily on deer, requires a - large territory. Because of its strength, stealth, and speed, - American folklore has given this wary cat a false reputation as a - man-stalker.] - - [Illustration: The red fox depends largely on a well-developed sense - of smell to locate its prey; it also relies on its keen eyesight, - speed, and agility to capture mice, hares, birds, and whatever else - it can run down or surprise.] - - [Illustration: To feed its demanding young, the Swainson's thrush - hunts for insects along the forest floor and in the dense - underbrush. This thrush relies on its secretive behavior to protect - its nest near the ground from detection by other predators.] - - [Illustration: Armed with enlarged forelegs, the crab spider waits - on or near flowers to ambush visiting bees, flies, or other insects. - Its venom produces a quick kill, allowing it to attack insects many - times its own size.] - - [Illustration: The spotted frog is a large-mouthed predator that not - only eats water striders and other insects but also gulps down - smaller frogs and small fish.] - - Protective Coloration - - To escape extermination, each species must in some manner foil its - enemies. Protective coloration is one of the more common adaptations - helping to do this. Most animals resemble their environment to some - extent. The conspicuous markings of some, like the bitter-tasting - monarch butterfly or the striped skunk, seem to function as a - warning to prospective predators that it is in their best interest - to look elsewhere for a meal. - - Some animals, such as the white-tailed ptarmigan and the snowshoe - hare, have seasonal changes in plumage or pelage, wearing white in - winter and brown in summer. Even predators, such as longtail and - shorttail weasels, benefit from seasonal camouflage. Protective - coloration makes them less noticeable to prey species and to larger - predators. - - Many insects, too, change coloration with the season. Bright green - grasshoppers of early summer become more brown with each molt, - matching the changes in the surrounding vegetation. - - _Obliterative shading_ is especially important to animals that - frequent more than one habitat. Seen from above, turtles match their - dark background; from below, because of their lighter underbody - shading they blend into the bright skylight. - - _Disruptive coloration_ aids in breaking up an animal's outline. - Butterflies and moths commonly have disruptive wing markings. The - distinctive shapes of eyes can be concealed. Eye coloration may - mimic body color--as in the green katydid--or the eye may continue - disruptive body markings. - - Ground-nesting birds are especially vulnerable to attack. Their eggs - tend to be heavily blotched with earthy colors, making them less - conspicuous. Chicks also carry these disruptive colorations on natal - down. - - Most mammals, with coats of brown or gray, are inconspicuous when - motionless. Deer fawns are endowed with speckled coats, mimicking - the sun-flecked forest floor; this disruptive coloration, coupled - with absence of scent and their instinctive "freezing" behavior, - makes it difficult for predators to detect them. - - The whitetail deer not only uses its white "flag" to warn others in - the herd of danger; it also allows a pursuing predator to use it as - a target. When the tail is suddenly dropped--abruptly obliterating - the bright white patch--the deer seems to disappear into its dim - surroundings. - - Since overly conspicuous animals are prone to predation, natural - selection favors development of appropriate camouflage. - - [Illustration: For such ground-dwelling birds as the white-tailed - ptarmigan, camouflage is an important survival adaptation. The - ptarmigan changes its plumage to match its surroundings: it is white - in winter, speckled in summer. Moving slowly and refraining from - flight, it is less likely than more-active birds to be detected by - sharp-eyed, motion-conscious predators.] - - [Illustration: Birds that when hatched are covered with down and are - able to move about freely are called _precocial_. They are less - dependent upon their parents than are _altricial_ young, which are - naked and helpless when they hatch; but they must rely heavily on a - resemblance to their surroundings for survival during their first - flightless weeks. This spruce grouse chick, which blends into its - sunflecked forest-floor habitat, is an example of a precocial bird.] - - [Illustration: The bold disruptive pattern of the killdeer chick's - plumage helps this precocial bird avoid detection in its - open-prairie environment. This adaptation, coupled with the chick's - instinct to freeze at the approach of danger, ensures that enough - young will survive to perpetuate the species.] - - _Ursus arctos horribilus_: The Vulnerable King - - At the apex of the food pyramid, this great beast is unquestionably - the king of Glacier's biotic community. Yet the long-range future of - the grizzly bear is uncertain. With the grizzly exterminated from - most of its former range--which once extended into the midcontinent - and south into Mexico--its numbers have dwindled in proportion to - its diminished range. Present concentrations in the contiguous - United States remain in and around Yellowstone and Glacier National - Parks. Probably fewer than 200 of these magnificent creatures live - in Glacier National Park. - - Grizzlies are easily distinguished from the more common black bear. - In addition to larger size and heavier build, grizzlies have a - characteristic shoulder hump; long, conspicuous claws; and a broad, - concave face that gives them a "dished-in" appearance. Fur is - usually brown; like the fur of the black bear, however, color may - range from black to yellowish. Light tipped hairs make the fur - appear frosted, giving rise to the nickname, "silvertip." - - Grizzlies, popularly considered arch predators, are more accurately - described as omnivores. Carrion, grasses, cow parsnip, and several - species of berries, bulbs, and tubers make up a grizzly's diet, - along with insects, small mammals, and an occasional ungulate that - it can catch. As a result, grizzlies play several roles in the - biotic community, functioning as herbivore, scavenger, and predator. - - Ranging widely in all life zones, grizzlies follow the spring - snowmelt up to the alpine meadows, returning to lower elevations to - hibernate from November until April. One to three cubs are born in - midwinter during hibernation. Since the maternal bond lasts two - years, a sow will accept a mate only every other year. Mortality of - subadults is high, resulting principally from competition among the - bears themselves. As with most animals, range--habitat--appears to - be the limiting factor of grizzly populations. - - The grizzly is normally shy and fearful of man--but highly - unpredictable. Wounded or sick bears, sows defending cubs, young - adults, and bears that have become conditioned to human scent are - the most dangerous. As humans continue to encroach on grizzly - territory, odds of confrontation also increase. Recent fatalities - and personal injuries inflicted by grizzlies pose a vexing problem - to the National Park Service, which is charged with visitor safety - on the one hand and protection of the park's remaining grizzly - population on the other. Continuing study of grizzly ecology and - increasingly enlightened bear management programs will, it is hoped, - allow man and bear to co-exist in a wilderness both require. - - [Illustration: Grizzlies are fond of succulent spring grasses.] - - [Illustration: Traversing all life zones in the park, the grizzly is - a true opportunist, eating anything from ants and berries to - wapiti.] - - [Illustration: Seldom will a grizzly exceed 225 kilograms in - Glacier. This is a young adult.] - - Bald Eagles and Kokanee Salmon: A Recent Gathering - - In 1916 the kokanee salmon, a small, land-locked form of the Pacific - coast species, was planted in the Flathead drainage. With the first - planting augmented by additional stockings, the fish thrived in - cold, deep Flathead Lake, and, to a lesser extent, in Lake McDonald. - The salmon fed almost exclusively on zooplankton. - - By the mid-1930s, salmon runs were becoming established. The outlet - of Lake McDonald provides an ideal spawning site for the salmon. The - fast-flowing water is clear, cold, and shallow, and the creek bed is - gravelly. - - Averaging 0.3 meters in length and weighing less than a half-kilo, - the 4-year-old adult salmon cease feeding and begin to migrate. Many - thousands swim the 100 kilometers from Flathead Lake to McDonald - Creek. Males appear in the creek first, arriving in late September, - and are soon followed by the females. - - Using her tail to dig a redd (a shallow nest depression), the female - deposits about 650 eggs. After fertilization by the male, the eggs - are covered over. The adults die within three weeks after spawning, - their bodies exhausted from the rigorous migration journey and the - weeks-long lack of sustenance. - - Egg fatalities are high, due to stream erosion and disturbance by - other spawning salmon. Hatching in late March, the fry work their - way out of the gravel and migrate downstream. - - Attracted to the 75,000-150,000 salmon concentrated in a 3-kilometer - stretch of shallow water, bald eagles begin gathering at McDonald - Creek in October. It is not known where the eagles come from or - where they go after the spawning run. Glacier has fewer than 20 - summer-resident bald eagles, and these are distributed among the - remote lakes of the North Fork area. - - In 1939, 37 bald eagles were counted along the creek. By 1969, 373 - were reported, representing approximately 10 percent of that year's - estimated winter population for the contiguous United States. Since - 1960, the count has averaged 240 birds. (In 1977 there were 444.) - - Eagles feed by swooping down to pluck salmon from the water or by - wading out to grab a fish stranded on a shallow riffle. An eagle may - consume as many as six fish a day. Immature birds are not as adept - at catching fish and may harry adults or other immatures into - releasing their catch. - - [Illustration: From its vantage point, this mature bald eagle - examines the waters of McDonald Creek. Average weight is 5.7 - kilograms; average wingspan is 2.2 meters. Females are slightly - larger than males.] - - [Illustration: This immature bald eagle lacks the familiar white - head and tail of the adult birds. It will not acquire those markings - until it is several years old.] - - [Illustration: Breeding male and female kokanee salmon are easily - distinguishable; as spawning time approaches, they change - appearance. The dark gray backs turn red; heads become green, and - the males develop humped backs and hooked jaws.] - - [Illustration: Swooping upward with a fish, a mature eagle heads for - a convenient perch to consume its catch. A strategically located - tree may contain 30 birds.] - - A Triumph of Many Colors - - Grassland, meadow, tundra, or any other area in Glacier suitable for - plant growth and supplied with abundant sunlight produces an - extravagance of wildflowers. This display of various shapes and - colors is neither an accident nor a mere decoration of nature. Nor - would Earth's recent explosion of mammal and bird species have been - possible without the evolution of flowering plants. - - Two hundred million years ago, early in the Age of Reptiles, - angiosperms (flowering plants) had not yet evolved. Plant - reproduction still relied on spores and cones. Then, during the - Cretaceous Period, the last sediments were being laid down in the - inland sea that covered most of Montana. (It was these sediments - that the ancient Precambrian rocks of Glacier's mountains later - overrode, forming the Lewis Overthrust.) During this period the - evolutionary miracle occurred: flowering plants--grasses, vines, - shrubs, broadleaf trees, wildflowers--inherited the Earth. - - The timing was important. As Earth's tropical climate gradually - changed to temperate extremes during this period, the domination of - cold-blooded dinosaurs ended and the moisture-demanding coniferous - forests that had covered the earth in green monotony began to - shrink. Angiosperms provided a solution to the ecological void: - grasses and forbs grew where trees no longer could. Most important, - relationships evolved between this new class of plants and the - relatively few species of insects then existing. - - Insects began to use the pollen of flowering plants; the - angiosperms, in turn, evolved bright petals and nectar that - exploited visiting insects for the plants' own reproductive - purposes. This partnership allowed insects to diversify rapidly, - evolving new, specialized forms such as bees, moths, and - butterflies. As a result, predatory forms of insects and arachnids - also rapidly diversified. - - The most dramatic change, however, involved warm-blooded birds and - mammals, whose high rates of metabolism required high-energy fuels. - Unlike gymnosperm seeds, which contain no protective covering, - angiosperm seeds are surrounded by a fruit. The development of these - highly nutritious seeds, and the attendant explosion of insect - species, ensured survival of the newly evolved birds. - - As birds diversified into seed-eaters, insectivores, and carnivores, - mammals, then uncertain little ratlike creatures darting among the - feet of dinosaurs, began a rapid rise to dominance; grasslands - promoted an explosion of herbivorous and carnivorous species. - - The evolution of angiosperms, and the animal revolution it made - possible, came with amazing speed. Most significant, it was a vital - first step upon which the meteoric rise of man depended. - - [Illustration: Indian paintbrush is common at all elevations below - tundra. It may be white, yellow, orange, pink or red. The actual - flowers, inconspicuous and green, are surrounded by brilliantly - colored bracts. Semi-parasitic on other plants, paintbrush is - normally found growing in conjunction with other wildflowers; its - roots steal sustenance from neighboring plants.] - - [Illustration: Yellow stonecrop, widely distributed in forest and - scrub-forest zones, is one of the park's few plants having succulent - leaves, an adaptation that helps it survive in such situations as - dry, rocky outcrops.] - - [Illustration: The Calypso orchid grows in the cool, shadowed forest - where light is dim. It lives in partnership with certain fungi that - exist about the orchid's roots and seem to help nourish it.] - - [Illustration: Silky lupine, a legume, has nitrogen-fixing nodules - on its roots, thus allowing it to grow in nitrogen-poor soil. It is - widely distributed in grassland and forest communities.] - - Fire Succession: Key to Continuity - - Most of Glacier's fires are lightning-caused. Strikes may flare up - immediately; or fires may smolder in the forest duff for days until - fanned into flame by wind. _Ground fires_ may race through the - forest understory, causing minor damage; or they may bridge the - understory and reach the canopy, thus becoming rapidly spreading - _crown fires_. Under certain conditions, uncontrollable infernos may - develop, generating terrific winds and heat. These rare - conflagrations are called _fire storms_. - - Every type of forest habitat has _climax vegetation_--trees and - shrubs that are best suited to the site and thus maintain themselves - indefinitely if not disrupted. - - After a major fire, habitat conditions are usually so altered that - the site must pass through several _seral stages_ before conditions - are such that climax vegetation can return. A _sere_ is a series of - plant communities that follow one another in orderly fashion until - climax conditions are again reached. - - [Illustration: Lightning fires occur most often during the hot, dry - weeks of late summer.] - - [Illustration: When the forest is dry, lightning often causes quick - flare-ups.] - - [Illustration: The forest may continue to burn for days after the - main conflagration has passed.] - - [Illustration: After a major fire, sun-loving grasses, shrubs, and - wildflowers quickly invade the former forest. Deer and wapiti - benefit from these new food sources.] - - [Illustration: Lodgepole pine, a pioneer species quick to take over - burned areas at lower elevations, grows rapidly. These trees are - five years old.] - - [Illustration: This is a Glacier National Park forest 80 years after - a major fire.] - -Sudden hammering made me jump. Above the forest darkness, a pileated -woodpecker leaned out from a high larch snag, braced against the trunk -by its specialized, stiff tail feathers. This was the first time I had -seen this big white-and-black bird, the "cock-of-the-woods." There was -ample evidence of his work: the deep, oblong excavations in the trunk -and the pile of large wood chips at its base, both characteristic of -this species. Again he hammered, and I could see the chips falling. -After a little edge-work around the hole, he extracted a grub and flew -off, yammering against the advancing dark. - -Near a stream I stopped to sit down, to listen to the water and maybe -catch sight of some small animal. Across the narrow defile, from a slope -dense with young hemlock, came the buzzing note of a varied thrush. -Several notes followed, all on a different pitch, all drawn out, level -and clear; the quality was pure but songless, disjointed, deliberate, -like someone testing the reed of a strange woodwind. There seemed no -gladness in the heart of this thrush. The song was dark, haunting, -lonely. - -On the trail ahead I could make out a bird hopping rapidly along. After -passing the spot I could hear its song. There couldn't be a hundred -meters between us, yet it seemed to be coming from a great distance. I -listened for as long as it would sing. I tried to hear it for what it -was, a male Swainson's thrush proclaiming its territory. But the -ethereal, flute-like phrases seemed an evensong made not for man's ears -but only for the forest itself. - -I hurried on after the bird had ceased. It was getting dark beneath the -trees, but I was beginning to be aware of creatures underfoot, the mad -dartings of shrew and vole, more imagined than seen. When a deer mouse -jumped away I got out my flashlight. Soon the beam caught a woodrat -sitting atop a fallen log. The light didn't bother him in the least; as -I approached, he picked up his bushy tail in his forepaws. Whiskers -twitching, he looked more caricature than real. Then he bounded off the -log with graceful, arching hops, and disappeared into the night. - -Against a patch of sky that appeared in a clearing, I could make out -bats, circling and dipping like swallows. Locating a hovering moth, I -kept the light beam on it until it vanished into a furry streak of -silence. It was time to head back. - -By now it had become utterly dark within the trees, a moonless, -sightless, alien world, given over to the marble-black eyes of the small -night mammals and the creatures that hunt them. I thought of the -strange, unseen societies of the flying squirrels, the nocturnal -counterparts of red squirrels; of the great-horned owls, inspecting the -same ground the goshawks scanned during the day. Perhaps a foraging red -fox moved through the darkness nearby, or a coyote on night patrol. - -The flashlight beam probed ahead along the trail. The exposed roots were -given unnatural shading and they seemed to thicken and squirm as I -approached. On either side the tree trunks appeared to step backward -from the dim glow of the light. I felt lost in this night, thinking of -the great darkness in all the timbered ridges that ran westward from the -Divide. In this vast cathedral of crowded tree and peak, night was stood -on end, the stars shrunken to a circle overhead, as if seen from the -bottom of a well. Mouselike, shivering, insignificant in this -wilderness, I scurried back to find a fire and fill my empty senses with -its heat and snap and light, holding off the fright of night and -thinking of tomorrow's sun. - - -Scrub-Forest - -The crowning beauty of Glacier--the high, cirqueheld meadows that scent -the wind with wildflower and waterfall--belongs to the zone of -scrub-forest. - -At Logan Pass you are introduced to the highlands. Here an exquisite -upland basin holds the Hanging Gardens, a wildflower-clothed gradient -laced with stair-step bogs and lines of wind-bent subalpine fir. In the -dawn sun, before the first engine noise, it shines unbroken, dewbright -and sagging like a spider web secured to the circle of surrounding -peaks. - -This is the region the hiker remembers best. The tall mountains wear -this zone close to the cliffs, and the trails encounter it near the -passes or follow it for long, level stretches, as along the Garden Wall. -I remember Preston Park and Fifty Mountain, the fire-touched bench of -Granite Park and the first sight of Sperry chalet, built on a brow of -rock at the upper reach of trees. But most of all I remember the -terrible waterfall that becomes Bowman Creek, the plunge of nearly a -kilometer that drains the magnificent upland bench called -Hole-in-the-Wall. - - - Hole-in-the-Wall - -September. The season is growing late, the meadow-rue dying and the -leaves of the wild strawberry failing at last. Everywhere the red -contagion of autumn surrounds the vital green. The lower valleys have -lost the whistle of ground squirrels. They sun themselves no longer -these late, mild days. Ripe, sluggish, and hawk-vulnerable, they sensed -the need of hibernation. - -It has been eight years since I last visited Hole-in-the-Wall, but I -retain its dimensions and hear its dozen waterfalls at will. Once you -have seen this basin you have a measure by which to judge the high -country and a thirst for the meadows at tree-line. - -In Glacier, treelimit ranges between 1,850 and 2,300 meters, depending -on local conditions. The upper limit of tree growth--rarely an even, -horizontal line--is generally an indistinct band running erratically -across a mountain's face: a tension zone reflecting variations in wind -and sun exposure, degree of slope, snowpack accumulations, and the -presence of adequate soil and water. - -Subalpine fir, whitebark pine, and Engelmann spruce do not relinquish -easily their upward climb; where conditions become severe, their growth -is retarded and their stature dwarfed. Deformed and pruned by wind, -their leaders winter-killed when they outreach the protection of the -winter snowpack, trees become shrubs, forced to hug the ground. Size -belies age in these elfin forests, or krummholz, where the growing -season is painfully brief and progress is always uncertain. A twisted, -gnarled little bush, more snag than live branch, bearing a single cone -or two, may be senior by a century to the giants of its race in the -valley below, which yearly shower the ground with an abundant crop of -cones. - -This time I will come from Goathaunt, passing Lakes Janet and Francis, -reaching Brown Pass from the east, and camp in the spectacular garden -between Brown and Boulder Passes. - -Meadows and rock slides break the forest as the trail gains elevation -and distance through the valley. The spruce and fir thin out rapidly at -the valley head, the trail climbing the grassy slope to low, broad Brown -Pass. Below the pass is Thunderbird Pond, which receives the meltwater -from a glacier high on a shelf of Thunderbird Mountain and is bordered -by a low jungle of willow. In the water stands a bull moose, its heavy, -fully formed antlers ready for the season's impending business. - -I was hoping again to see Cassin's finches and Audubon's warblers on the -pass; but the fir grove is quiet. Sitting down to rest and listen, I -become aware of a strange silence. No birds sing or flit among the -trees, no alarms pass back and forth among alert ground squirrels. There -is no wind--an odd condition for the Continental Divide. This place -seems to be holding its breath. High overhead, a veil of cirrus cloud -arranges long spears across the sky. - -Moving off the pass, along the dome of Mt. Chapman, I experience anew -the old excitement of this high country. Abruptly the gorge of Bowman -valley opens up, revealing the twisting blue snake of Bowman Lake far -down the narrow, cliff-imprisoned valley. Here again are the northern -titans--Numa, Peabody, Boulder, Thunderbird, and Rainbow; and Carter, -with its high glacier baring blue ice teeth to the sun. - -It is not the climb that makes your heart pound now; the trail is -suddenly narrow and cliff-defiant, cut by the plunging waters of -snowbanks far above. These are splendid peaks, unmatched in a land of -muscled, brutal earth. Even the air seems to retain the scent of glacier -work. - -At last the view of Hole-in-the-Wall, a staircase cirque excavated -between the gigantic spread ribs of Mt. Custer. The slopes of beargrass -are seed-spotted and gaunt now, the white fullness gone. Western -pasqueflowers have accomplished their magic transformation; known in -this season as old man's beard, they nod their tufts of grizzled -seedhead silk in the wind. Red and yellow monkeyflowers bloom yet, -crowding along the many stream courses, and waterloving sedges and -mosses surround pools of collected water on the broad horseshoe tiers. - -A spur trail drops down into the campground on the last ledge. Through a -cleft in its lip plummets the gathered water of the basin. From the -valley below, the waterfall appears to be springing from a hole in the -headwall, giving this basin its name. Down, down, down, roars the water -where once a mighty glacier ground its teeth. - -I leave until later the making of camp; by now the sharp shadows of -Boulder Peak stab the valley forest and are beginning the upward assault -of Thunderbird. - -Around the basin headwalls, last winter's snowbanks remain formidable. -Snow caves send out meltwater torrents. Glacier lilies and patches of -spring beauty line their fringes. Pasqueflowers bloom in pockets. Here, -among the asters of August, bloom also the first flowers of spring, -shooting up as the snowbanks shrink, making these spots of snow-free -ground a patchwork of May and July, August and June. The shrubs that -line the furious water are willows, still bud-swollen this tenth day of -September. The coming days will bring a sharp surprise. - -Winter will soon stop the melting of this snow. Could it be that I am -seeing the first year of a reawakening ice age? If so, each year the -snowfields would grow thicker and broader, connecting the shelves into -one ice mass again, lilies and willows entombed, the summer heat failing -to rescue them, until the ice at last began to slide, stripping the soil -and once more plucking at living rock. - -Then these dwarfed fir, which cling precariously to the cliffs and hide -behind the backs of boulders, would be in more danger than they were -from their recent antagonists. Engulfed by ice, they would know the -shearing wind no more. Their skeletons would rain down into the valley -below, signalling another long forest retreat. But they have waited out -the mountain ice before and would send their seeds again to this valley, -changed however it might be, as they have always done. - -Evening brings out two sleek mule deer does. As they graze, their large -ears stand erect, sorting out the lesser sounds from the ceaseless roar -of water. Both raise their heads and point their ears, statue straight, -at the scuttle of a porcupine. A noise among the rocks draws a backward -glance and focus of those ears. I would like the sensitivity of such -fine equipment, to hear what deer have always heard. - -Setting about the business of camp, I wonder about those animals that -watched me for a while, then moved off, having seen a tent go up before. -With the appearance of the moon the wind increases and they test the air -more often now. Do they have visions of cougar or grizzly with every -snap the wind delivers? - -In summer these high meadows see a surprising variety of animal life. -Briefly out of hibernation are marmots and the handsome golden-mantled -ground squirrels. Mice, voles, shrews, and woodrats run among the -shadows, feeding on the season's feast of seeds and insects. A nightmare -for these are the fierce little weasels that haunt the rocks. - -Tracks of cougar and wolverine are sometimes seen, often teasingly -fresh; to glimpse either of these elusive predators is to taste the -finest wine of wilderness. - -Before the berry season, grizzlies grub the meadows for the tasty bulbs -of glacier lilies and the tubers of spring beauty; often distracted by -the scent of a ground squirrel in its burrow, they sometimes make a huge -excavation for a small reward. - -White-crowned sparrows sing in July from the low tops of the battered -trees, though their nests are on the ground below. Grey-crowned rosy -finches patrol the drier ground for seeds while water pipits hunt -insects in the wet areas. High above, a golden eagle scans the basin -again, circling slowly before following a ridge south to sight another -likely slope in its 10,000-hectare territory. - -The moon shines through the tent top. The wind, blowing more violently -now, shivers the nylon and interrupts the voice of the waterfall. I have -followed the pasqueflower run from the April prairies here to its -highest bloom near treeline. I think about the triangular seed pods of -the glacier lilies, colonies of steep-throated blue gentians, and the -season's last glory of goldenrod. Indian paintbrush, from white to fire -red, blazes the slopes that light the fringes of sleep. - -I awake to a determined rain, the moon gone and the tent shuddering with -wind-blast. I try not to think of the steel-cold air, and slip into a -fitful sleep that seems an endless treadmill of rocky trail. - -Stiff and unrefreshed, I look out into the dawnless morning. The tip of -Thunderbird is detached from its base by grey clouds swirling at its -throat. A wave of sleet slants down, dancing on the rocks, chanting -triumph over the buried, bent, and broken flowers of yesterday. - -So I must make my escape, short of Boulder Pass. Unattainable now, -invisible above the cirque, that high pass grows in my memory. This -testament to what a glacier can do, to the struggle of trees and the -life-pioneers that invade such harsh places, is at my feet but shrouded -with snow. My hands grow stiff and numb in the blunt work of packing up. - -I had wished to see Kinnerly Peak again, rising from the western Kintla -valley, and walk along black ledges of the lava that floors the pass. -Beyond it grows a grove of subalpine larch, stately, seldom encountered, -the least common tree species in Glacier. Confined to this narrow zone -between forest and alpine, it reaches up tall and proud, impervious to -the gruelling climate that makes cowering shrubs of other trees. - -But all must wait another year, for this season comes down hard. And the -will of winter is to erase whatever summer had devised. - - -Tundra - -Porcelain-cold, the November sun dawns in the southeast sky. The ledges, -ice-encrusted, layered with sleet from a recent squall, whistle the cold -morning wind aside. Rattling down, a slide of rock plunges off the final -ledge, seconds passing before the hollow sounds of impact clatter back. -Like an apparition of winter itself, white beard bent sideways by the -wind, a mountain goat steps to the precipice edge. Looking out across -the vast white void, its long belly hair and pantaloons streaming with -the ceaseless wind, this strange animal, product of some unfathomable -ingenuity, hesitates but a moment; dropping down from step to invisible -step along the sheer rock face, fracturing the ice glaze as it goes, it -turns a wall and disappears. A nimble, eight-months-old kid follows. - -Blinking and twisting in the dull light, the shower of shattered ice -clinks softly downward against rock, fading away like the short summers -of this place. - -But while the wind chants winter, life has made a passage here, and also -waits, hidden in seed and root and den. - - -[_] -The nanny and her kid have bedded down now, looking across the deep, -snowy basin below. Their ledge shines with the first spear of sunlight. - -Far below the pass that connects Mount Siyeh to the snow-giants Matahpi -and Going-to-the-sun, three male white-tailed ptarmigan emerge from -their night's huddle within a snowbank and step out to peck at an -exposed mat of willow. Ptarmigan, the only birds on the winter tundra, -wear white plumage in this season, helping to camouflage them in the -snow, just as their mottled brown summer plumage makes them difficult to -detect among bare rocks. There are few predators here to hunt them now, -but they move with habitual slowness; quick movement can be fatal when -summer brings numerous eyes to scan the slopes. With legs and feet -heavily feathered and sharp claws to scratch for food beneath the snow, -the ptarmigan live at truce with winter. When blizzards rage between the -peaks, they nestle together in snow dens, beyond the reach of the winds. -Ptarmigan hens winter lower in taller willow thickets, but the males -prefer to take their winter as high as possible. - -Now they crouch behind the wind-deflecting rocks, dozing in the meager -warmth of the morning sun. - -Near the snowless summit crags, a flash of brown fur zigzags among the -rocks. That would be a pika. Only for a moment does it show itself, so -quickly does it move. - -Also called the rock rabbit, the diminutive pika belongs to the order of -hares and rabbits. Resembling a small guinea pig, this sturdy creature -spurns hibernation as a way to beat the challenge of winter. Instead, it -spends the summer laying in a store of hay for the lean season, -spreading cut grass to cure upon the rocks and tending its "haystacks," -on which its survival hangs. - -Winter is a great peril to small mammals. Their small bodies, because of -a large surface area in relation to volume, retain heat poorly, and -their high metabolic fires consume calories quickly. Great amounts of -energy are required to sustain an active animal in rough terrain, -placing further demands on the animal's capacity to survive the cold. -The pika may need to stack as much as 25 kilos of hay; to keep its -furnace burning during winter it will have to fuel its stomach almost -hourly. - -Small animals of cold climates often show distinctive body adaptations. -On the pika the small, rounded ears lie flat along the head, the tail is -inconspicuous, the legs are short; heat loss from exposed surfaces is -thus reduced. Fur insulates the soles of the pika's feet while at the -same time providing good traction on steep rock faces. - -Hidden below these rocks are the hibernating marmots and the sleeping -ground squirrels. Beneath the snow the mice, shrews, and pocket gophers -struggle on with their lives. But above ground, directly confronting -this arctic climate, are the pika, the ptarmigan, and the mountain goat. - -A triumph of adaptation, the mountain goat faces the winter day without -benefit of either the pika's den or the ptarmigan's snow roost. - -The nanny and kid descend from their ledge to search out browse at -treeline with other members of a loose band--yearlings, young males, -other nannies with kids. At the fringes of the band a solitary adult -billy only grudgingly associates with other members of his kind; for -this is the season of rut. - -Not really goats at all, these relatives of the European mountaineering -chamois are insulated from the wind by coats of long, hollow-haired fur -overlying woolly underfur. They are stocky, stiff-legged, and -deliberate, able to negotiate the walls and pinnacles with their -superbly adapted hoofs. The unique design of these hoofs gives the -animal great traction and stability on precarious crags. Opening towards -the front, the cleft between the two hoofs spreads each outward as the -animal descends a slope, helping to grip the rocky surface. In addition, -the large, rough, and pliant sole of each foot conforms to the bare -rock, increasing traction. - -There is little need for the goat to leave its steep sanctuaries; it can -subsist on lichens and mosses if browse is not available. It depends on -the inaccessibility of the cliffs for its security. Accidents, -avalanches, and rockfall are greater enemies than predators. Golden -eagles sometimes attempt to knock newborn kids from ledges and a young -goat quickly retreats under its nanny when an eagle soars by. With the -protection of sharp spike horns and a terrifying terrain, adult goats -seldom fall victim to cougar or grizzly. - -It will be a long time before the snow releases this land and wapiti, -bighorn, grizzly, and cougar wander back into these high basins. In this -winter minimum of life, the spring songs of rosy finches, water pipits -and white-crowned sparrows seem an impossible extravagance. - - -[_] -I am drawn to the spring tundra--to the vigor and tenacity of its sparse -life--where survival itself seems ceremony enough. But it is a strange -world, where a man is out of perspective. Here the plant cover is -carpet-high, and distance, for the lack of trees, tricks the eye. Here -the wind, snow, and sun quickly burn skin, and the intense light, -reflected from snowbanks, stabs at the eyes. Almost instantly, a -sandwich is sucked dry of its moisture. The desiccating wind probes the -ears until it seems at last to pierce your brain. Except for fearful -mountain walls the only shadow is your own. Animals seem somehow remote -and unknowable, as if seen through glass. A day on the tundra and you -feel the want of a company of trees. - -Yet once exposed, you acquire a craving for the look of tundra. Nowhere -else is there such an impatience for spring--the flowers rush into -bloom; the male water pipit soars, its skylark song crystal sharp in the -thin air. The nesting birds are restless, for sun-days and warm days are -few, precious, and quickly spent. Insects and spiders abound--flying -about the peaks or crawling among the rocks. - -Summer brings bands of bighorn rams up from the valley to explore the -highest meadows. Though not so sure-footed as the goats, they too have -hoofs adapted to climbing steep faces, and they walk the slopes not far -below the goats. - -Marmots, which whistle sharply when threatened, spend their days -sunbathing and grazing; they must fill out their now loose-hanging fur -coats with life-sustaining fat for the coming winter. - -Alpine animals are blessed with mobility and can choose their weathers, -retreating to burrow, den, or rock-harbor to escape the worst fury of -storms. But what about the plants, rooted forever in one spot, assaulted -by an untempered sun and a drying wind, and facing the almost daily -threat of freeze and storm? - -Alpine plants, through their design and growing habits, have adapted -themselves to the rigorous demands of this climate in many ways. Most -plants are perennial: there just aren't enough days or nutrients -available for the growing of entire plants each year from seed. And they -have the ability to grow and carry on photosynthesis at temperatures -just above freezing, thus extending their season. In this zone, -temperatures are rarely above 15 C; the mean summer temperature is -about 10 C. But a flower such as the alpine buttercup, which is found -at treeline or above, can grow through several centimeters of snow; heat -given off during the plant's respiration will create an opening through -which it can emerge. - -Plants have various adaptations to meet the demands of the alpine -environment. Yellow stonecrop, not restricted to this zone, is -nevertheless able to survive here because of its fleshy succulence and a -waxy covering that prevents water loss. On some plants, protective hairs -covering leaves and stems help retard the burning effects of wind and -sun. Often this pubescent foliage looks more grey than green, for the -soft hairs mute the color. - -Cushion growth is another alpine adaptation. The moss campion cushion, -covered with delicate pink flowers, grows to about one-third of a meter -across and only 3 to 5 centimeters high. Spreading out close to the -ground, the plant avoids the major violence of the wind and hoards -moisture like a sponge. - -The dryad, growing abundantly on the windy sweep of Siyeh Pass, shows -alpine adaptations in several ways. The energy of the mature plant is -channeled primarily into reproduction: its large flower, supported by a -short stem, matures quickly; and it produces many seeds, ensuring -germination of a few. An evergreen, it begins to synthesize water and -carbon dioxide into food as soon as the snow is gone; and its rolled -leaves prevent rapid evaporation. It grows as a low and woody mat that -year by year extends itself through the production of new shoots that -carpet the rock. Mat growth has the advantage of retaining dead plant -material and capturing wind-blown grains of soil, allowing the plant -slowly to enlarge its soil base. - -Compared to the forest, the heartbeat of the tundra is painfully slow. -Here a plant may grow for a quarter of a century before it has acquired -the reserves necessary for flowering. Contrasted with the progress on -the tundra, forest succession races by with dizzying speed. Yet -imperceptible as the change may be the alpine plant community also -passes from pioneer to climax. - -Beyond the limit of other plants, lichens thrive, encrusting rocks with -their rainbow colors. A lichen is actually a primitive and highly -successful association between a fungus and an alga, working together -for mutual benefit. The fungus protects the delicate alga, trapping and -holding moisture; the green alga, in turn, produces enough food to -sustain the needs of the fungus. - -Generating rock-disintegrating acids that help secure this partnership -to the rock, lichens, along with physical weathering, help break down -the rocks into soil particles. Collected in pockets by run-off or wind, -rudimentary soil is slowly invaded by cushion plants. After centuries of -colonization by these, while the meager soil is deepened and enriched -and moisture retention is increased, other plants move in, climaxing at -last in hardy grasses and sedges. As in the forest, pioneer species -change the environment to their detriment, creating a habitat better -suited to other species. - -Although it will progress with geologic slowness, the rocky ground of -Siyeh Pass--its plant cover presently scant and wind-rowed by -frost-heave and relentless wind--will in time develop grasses and -sedges, the climax vegetation of the alpine meadows. - - -[_] -Simplicity rules the alpine zone. Here life is reduced to bare -essentials. Chief controlling force is climate; but the plants and -animals that live here are well adapted. Compared to the lower realms, -where both competition and predation are fierce, life here looks secure. - -There is a penalty to simplicity. In the lowland, the long food chains -and diversity of species, the long growing season, and the abundant food -supply give the forest an adjustment mechanism and healing power not -found on the critically balanced tundra. The greater the variety in a -plant and animal community, the greater the stability. So in the alpine -world there exists a paradox: the most durable life forms constitute the -most fragile community. - - -The Water Communities - -Snowfields begin again their summer-long melt. The alpine stream, vocal -again, collects its water from a thousand places. Miniature gorges drain -the meadow, gurgling with the sparkle and rush of meltwater in the -lengthening spring days. - -Gathering volume, the stream seems to hurry faster; at the first rock -staircase, it begins to sing. I follow the gully downward, drawn like -the water. There is excitement in the growing dash and roar, a wind-gust -sweeping spray into the air. A rainbow appears, holding steady to the -swirling cloud of spray, then doubles and abruptly disappears. - -At the first great plunge the water lunges outward over the lip. Like -glass at shattering, long shards lance out. But the wind feathers the -sharp edges as they fall. - -The close thunder of a waterfall beats at your head, and your mind must -shout to think. Here is water, a most amazing and most important -substance. Perhaps some of this same water was once part of the ancient -sea in which was laid down the mudstone of this ledge; was once drunk by -dinosaurs; has coursed the globe countless times; and has flowed in this -very stream before. In solid, liquid, or gaseous form, it goes through -its own cycle. Together with sunlight, water makes possible and -maintains all life on Earth. - - - Ouzel Music - -A glacier might cling to a winter snow a hundred years and turn it to -ice, a blue tool to rasp and pluck at rocks, before letting it go. -Lingering summer snowfields might delay its passage for a time. But the -water always wins at last, becoming, in one decisive instant, liquid -again, and beginning its long journey to the sea. Plants and dry air -will intercept some of its molecules, sending them back into the -atmosphere to bloom as fog and cloud; but as rain, snow, or dew, these -are soon commissioned to the land again. - -Water is so familiar to us that we seldom think about it. We know that -fish swim in the lower lakes, and we are vaguely aware of the -bewildering assortment of life-forms abounding in a pond. But life -begins in the streams. - -Even cups of cold meltwaters, scooped out of a rivulet only a few meters -away from its snowbank source, contain some life. Snow algae, which grow -on the snowbank surface, often sufficiently dense to give the snow a -distinctive red complexion, are released into the meltwater. In summer, -small invertebrate life can be discovered in the standing pools of even -the highest cirque. - -But conditions are not good for the development of complete aquatic food -chains in the streams and lakes of higher elevations. Alpine lakes, or -tarns, support little visible life. Often flanked by high ridges and -peaks, many tarns receive scant direct sunlight during the day. Since -these lakes occupy basins that capture tremendous amounts of snowfall, -the snowbanks persist in the mountain shadows, and summer makes little -progress in warming the water. Iceberg Lake, for example, is seldom free -of floating ice, and its temperature never rises above 4 C in summer, -even at the surface. - -Moving out of the cirque lakes, water is soon churning again, dashing -downward many hundreds of meters to the valleys below, in rapids, -cascades, and breathless waterfalls. Not surprisingly, few plants and -animals are adapted to life in fast-moving water. - -Algae can be found covering streambed rocks and stranded, water-polished -tree trunks. Securely attached by holdfasts, these small plant forms -survive the rigorous stream flow that would destroy the larger vascular -plants. Several species exist, from microscopic forms to branched -filamentous algae whose long hairlike strands wave in the current. - -A surprising number of insects live on the stream bottom, finding a -measure of protection from the current in the jumble of rocks. -Underwater beetles live under the gravel or among the debris at the -stream-edge, or cling to stones and sticks. Scurrying and creeping among -the rock-crannies are the larvae of stoneflies, mayflies, and -caddisflies. These and the small fish that venture up from lower lakes -are the food of the water ouzel, a creature that loves the places where -the waters thunder. - - -[_] -The noise of the water is overpowering. A slip into this boiling rage -would mean quick death. Looking 10 meters across the dim, mist-slippery, -water-scoured canyon, I see a young water ouzel peering out of its -unique nest, on the lookout for its parents. Clouds of spray keep the -nest of living moss continually wet; but this bird is waterproofed with -an oily plumage and keeps its vigil at the nest opening. Peering into -the torrent below, then upstream and downstream, it awaits patiently the -delivery of the next meal. - -With the approach of one of the adults, three other heads crowd the -opening, begging yellow mouths agape. Flying low, the ouzel parent zeros -through the heavy spray, alighting on a slippery boulder below the nest -ledge. Preparing to fly up to the nest with its load of insect larvae, -the ouzel spots me across the water. At its sharp _jigic, jigic_ alarm, -the bills of the young snap instantly shut. Nervously the bird regards -my close presence, dipping its entire body rapidly up and down, as if -keeping time with the surging torrent. - -Discovering no danger, the dusky blue-grey bird bobs more slowly. The -other adult, returning from an upstream forage, alights on the same -rock, occasioning a new outcry from the fledglings. Each in turn, the -parent birds fly up to feed their young, beating their wings to maintain -their position at the perchless nest. Not pausing to regard me further, -they split the stream between them again, one flying upstream and one -down, to continue the hunt. Blinking and shaking the collected mist from -its bill, the single young sentry renews its watch. - - - In Shallow Waters - -Life abounds in the shallow lakes and ponds. Calm, protected John's Lake -offers a fine example of how a complex aquatic plant-and-animal -community can exist in balance in a confined space. The water teems with -the microscopic algae, protozoans, and rotifers that sustain the barely -visible zooplankton. Dancing, flitting, hopping, and swaying through the -water, these zooplankton in turn support the larger plankton-eating -animals. - -Dragonflies and damselflies shoot past, crackling their wings, and perch -in the bog grass. Looking into the shallow water, you will see a wealth -of small animal life. A spotted frog swims into view, floating to the -surface beside a lily pad so that its eyes protrude above the water. - -The ribbonlike form of a leech swims across the bottom toward deeper -water. Looking closer, you see that the water swarms with bizarre -shapes--water boatmen propelling themselves with oarlike appendages, a -gliding mayfly nymph, then a predacious diving beetle surfacing, -grasping a bubble of air beneath its shiny brown wing plates and -disappearing downward again--the bubble's edge shining silver--into the -brown bottom debris. Suddenly a whirligig beetle sets the surface to -spinning, wrinkling the view below. - -Everywhere in the water there is animal life, forms that are attached, -free-swimming, crawling on the bottom, and clinging to or swimming on -the surface film. The gray, slimy encrustation on a sunken log looks -like a covering of lichen but is really a freshwater sponge, a colonial -animal that feeds by filtering minute plankton from the water. Another -attached creature is the barely visible hydra; this twig-shaped -predator, related to marine jellyfish, captures water fleas and other -small animals in its several poisonous tentacles. - -Water beetles, backswimmers, water boatmen, and many other creatures -move about more or less freely in the water, propelling themselves along -with jerky movements. Suspended between surface and bottom are the -zooplankton, the tiny water fleas, cyclops, daphnia, and others, which -feed by filtering minute algae. On the bottom and below live scavenging -worms. Water striders skate on the surface film. - -Along the shore, frogs, salamanders, garter snakes, and water shrews are -hunting. Dabbling and diving ducks patrol about, tipping or submerging -for the bottom plants. Moose tracks circle the muddy shore. Because it -produces vegetation abundantly, John's Lake sustains a great diversity -of animal life. - - - Beaver Ponds - -Fully 10 percent of all the present meadow area in the Rocky Mountains -is estimated to have been created by beaver, the only animal besides man -that engineers extensive changes in the environment to suit its own -needs. - -When beavers dam a stream, they set in motion another form of -succession. If the resulting backwater floods a forest area, the trees -are soon killed, creating a broad opening in the forest canopy. -Water-associated plants and shrubs quickly invade the pond and -shoreline, creating favorable habitat for waterfowl, moose, blackbirds, -amphibians, wading birds, warblers, marsh hawks, and a score of other -animals. - -After many years the water becomes shallow, filling in with silt and -plant debris. When the beavers abandon the site, the dam may rupture for -lack of maintenance and the pond will rapidly drain. Or it may continue -to hold, delaying for several more years its slow conversion to meadow. -Stimulated by the nutrient-rich mud, the water grasses, sedges, and -shrubs finally choke the water with their accumulating debris, -transforming the area into a bog. - -Gradually the ground firms as more humus is created and more silt is -trapped. The area becomes meadow, supporting grasses, sedges, and other -flowering plants. Trees begin to reinvade the drier ground, and -eventually the meadow reverts to forest. Centuries may be required to -see this cycle through, from forest to pond, to bog, to meadow, to -forest again. At each stage many of the animal inhabitants change: the -song of the western robin and the chatter of a red squirrel in the -original, pre-beaver forest give way to the croak of a heron; the heron -is replaced by the insect-and-berry-eating cedar waxwing; the waxwing is -followed by the tree-dwelling western robin and red squirrel. - - - Lakes Cold and Deep - -Seeming to skate on its own reflection, a spotted sandpiper comes in low -over the quiet water, wingtips almost touching the surface of the lake. -It alights at the shore and folds its wings. Amid the rounded rocks, -this plain but elegant little shorebird is all but swallowed up. -Teetering constantly on long legs, it sets off along the water's edge, -pecking here and there, coming closer and closer, never forgetting to -stop and curtsy, as if acknowledging, while hurrying offstage, the -applause of an audience. - -As it draws near, several water striders skate away from the shore. A -stonefly, scuttling between two rocks, is deftly speared. So large a -morsel makes the bird pause and rough its feathers, then scamper into -the water to take a drink. Teetering again, it passes in front of me and -continues down the shore, where I soon lose sight of it rounding a rocky -point. - -I am sitting at the foot of Lake McDonald, watching the darkness gather -over the valley, seeing the last light slide upward to the tips of the -distant mountains. As daylight dissolves, this long fleet of familiar -peaks seems almost to glide toward darkness, slow and silent as sailing -ships. - -The sheet of motionless water stretches many kilometers away between -tree-covered moraines. The water is deep and cold. No emergent plants -line the barren shore. It would seem that no life, except for the single -gull that rests on the water far away, exists in this nearly -thousand-meter-high lake. - - -[_] -Considering the great volume of Glacier's large, deep lakes, the life -they support is indeed meager. A large part of the reason lies with the -nature of their shores, where almost no plants grow. A combination of -factors prevents the development of a lush shoreline growth. - -Contoured like bathtubs, these steep-sided lakes exhibit narrow or -non-existent shoreline shallows, which are vital for the production of -rooted plants. Strong wave action and extensive seasonal fluctuations in -the level of these natural reservoirs prevent the development of -emergent water plants in locations where they might otherwise be -expected. - -Since sunlight cannot penetrate to the bottom of these deep lakes, they -are deprived of bottom-anchored plants in midlake as well. As a result, -herbivorous animal life must depend almost wholly on algal growth. Wave -action inhibits the spread of free-floating algae by washing much of it -onto the shore. Deep lakes are also low in available oxygen, preventing -the development of bottom decomposers, which would rapidly release -nutrients as they break down the accumulating debris washed into the -lake. Without a steady supply of nutrients, plant growth is retarded. - -Since the food chain depends upon green plants, the ability of a lake to -support higher animals such as fish depends upon its ability first to -produce adequate plant growth. The production of one kilo of trout -requires that a lake produce about 1,000 kilos of plants to support 100 -kilos of herbivorous invertebrates, which are eaten by 10 kilos of -carnivorous insects, on which the trout feed. - -Compared to smaller shallow lakes, which teem with visible life, cold, -deep, nutrient-poor lakes such as McDonald appear to be watery deserts. -Yet because of their great volume--Lake McDonald contains 5 or 6 cubic -kilometers of water--these large lakes do sustain significant numbers of -fish. Of the 22 kinds of fishes found within the park, most are -coldwater species. Trout, whitefish, grayling, suckers, minnows, and -carp fill the roles of herbivore, carnivore, and scavenger. Agile, -highly mobile, and acutely sensitive, fish represent the most successful -total adaptation to the aquatic environment. - -Through the stocking of nonnative species, including plantings in -formerly fish-free lakes, the natural aquatic communities of many of -Glacier's lakes and streams have been permanently modified. - -Aquatic food chains are not confined to the water. Ospreys, ducks, -mergansers, otter, mink, and many other semi-aquatic or terrestrial -birds and mammals utilize the plants and animals of the water. In fall, -a remarkable spectacle occurs along the outlet of Lake McDonald. -Attracted to the kokanee salmon concentrations, which run from Flathead -Lake to spawn and die in these clear, shallow waters, bald eagles -collect to exploit the vulnerable fish. In 1977, 444 eagles were counted -in one census. This food resource is also exploited by grizzlies, -coyotes, skunks, gulls, loons, and other animals. On occasion, even -white-tail deer have been observed swallowing salmon! - - [Illustration: Sunset] - - - - - Shooting Stars - - -This park is very special. The people who know it well feel proprietary -toward its mountains, scattered lakes, and glaciers. Perhaps it is the -arrangement of the land, an unsurpassed concentration of American -wilderness. Time and again I have thought, as I regarded some aspect of -this country, _yes, this is exactly right_--almost, it would seem, as if -some magic existed that could translate thought and emotion into rock -and bark. - -Glacier remains largely unexploited, bearing still the aspect of the -Earth the Indians knew for 500 generations--a land where it is yet -possible to feel a sense of discovery, sense that a single man matters. -On too many mountains, man has tarnished whatever he has touched; but -here the land has shed, as a fir sloughs snow, a long succession of -traders, trappers, explorers, hunters, surveyors, prospectors, loggers, -settlers, and tourists. - -You may walk the same trail a dozen times and not tire of the view. I -have given up wondering why. I know only that these are mountains a man -might grow old with, and that mountain-fever never diminishes but only -changes its look, as a forest does over many years. - -Repeatedly I have noticed that this park creates an instant bond between -strangers. A certain pause intrudes at the first mention of Glacier -National Park, and a look of distance comes, as Red Eagle becomes real -again, or the wind at Firebrand is remembered, or the flowers of -Fifty-Mountain converge once more upon the senses. - -Never are we quenched. If a goshawk rushes past, straining upward with -its squirming load of ground squirrel, forever afterward our blood -demands more. The sight of a wolverine running is not enough. Nor the -magnificent assemblage of bald eagles feasting on November salmon. More -days of this: mountain goats leaping impossible ledges, wave tracks from -a beaver reaching out on dawn water. There are messages here, loud as -kingfishers. The land has languages, stories to tell. - -But in wilderness there is no moral, save that it must continue. For all -our probings and plottings we discover no adequate interpretation of the -forces we find swirling about us. A larch you must touch to know; your -neck must feel the ache of too much looking up. Watch its treepoint -pirouette. Then, looking back at the world level, you will find that you -have lost all answers. We have learned the art of building bridges, -cataloging plants, predicting what a shrew might do. Of the essential -mystery, we know nothing. - -For nature assigns no "roles" to its creatures; there is no "reason" for -a forest fire, which burns mightily but with no intent. Life's only -"purpose" is the feeding of life, and the beauty we see therein is but -its lack of guarantee: for the chipmunk and the weasel, and the man who -measures his life to theirs, no assurance of long days and tempered -seasons, abundant seeds, ample meat. In wilderness there is mystery yet, -unsimplified, not reduced, resplendent and immense. - -Whatever the conclusion of this planet, however many the acts to follow -in this consuming drama--mountains coming up, mountains going down, -forests, lakes, and seas skimming past like wind-driven scud clouds -before a storm--at least in the scant shadow of this present age there -is an achievement of sorts. For now, with this creature man, such things -as mountains can be loved. And men have memories to fill. - -Tomorrow I will look for shooting stars--purple spring flowers that -point their fire down, always down toward the center of the Earth, as if -to give in their brief term beneath the sun a tribute to this most -excellent mystery. - -Today I can say nothing more, neck-sore now from looking at larchtops -swaying with the wind of this splendid morning. - - [Illustration: Shooting star.] - - [Illustration: Mountain goats.] - - - - - Appendix - - -Mammals of Glacier National Park - -Distribution information was obtained from _Meet the Mammals of -Waterton-Glacier International Peace Park_, by Robert C. Gildart (see -Reading List). Nomenclature follows, for the most part, _a Field Guide -to Mammals_, by William H. Burt and Richard P. Grossenheider. - - Key to symbols: - E--occurs east of Continental Divide (spruce-fir forest; aspen; - bunchgrass meadows) - W--occurs west of Continental Divide - (redcedar-hemlock-lodgepole-fir-larch forest; some meadows) - A--occurs in alpine areas (above upper edge of continuous forest) - R--rare in Glacier National Park - - Shrews - Masked shrew, _Sorex cinereus_ - E, W, coniferous forests, meadows, pond and stream edges - Vagrant shrew, _Sorex vagrans_ - E, W, A, moist forests and grasslands, marsh and stream edges - Northern water shrew, _Sorex palustris_ - E, W, stream edges - - Bats - Little brown myotis, _Myotis lucifugus_ - E, W, coniferous forests, often around buildings, caves; nocturnal - Long-eared myotis, _Myotis evotis_ - E, W, A, R, coniferous forests, meadows; nocturnal - Long-legged myotis, _Myotis volans_ - E, W, A, coniferous forests, meadows; nocturnal - Big brown bat, _Eptesicus fuscus_ - E, W, coniferous forests; often around buildings, caves; nocturnal - Silver-haired bat, _Lasionycteris noctivagans_ - E, W, coniferous forests; meadows; nocturnal - Hoary bat, _Lasiurus cinereus_ - E, W, coniferous forests; mostly nocturnal - - [Illustration: Cougar] - - Cats - Bobcat, _Lynx rufus_ - E, open forests, brushy areas - Lynx, _Lynx canadensis_ - E, W, coniferous forests - Cougar, _Felis concolor_ - E, W, coniferous forests - - Raccoon, bears - Raccoon, _Procyon lotor_ - E, W, R, open forests, stream bottoms - Black bear, _Ursus americanus_ - E, W, A, forests, slide areas, alpine meadows - Grizzly, _Ursus arctos_ - E, W, A, forests, slide areas, alpine meadows - - [Illustration: Coyote] - - Canines - Red Fox, _Vulpes vulpes_ - E, grasslands, open forest - Coyote, _Canis latrans_ - E, W, A, forests, grasslands - Gray wolf, _Canis lupus_ - E, W, R, coniferous forests - - [Illustration: Wolverine] - - [Illustration: Longtail weasel] - - Mustelids - Striped skunk, _Mephitis mephitis_ - E, W, open forests, grasslands - Badger, _Taxidea taxus_ - E, W, grasslands - River otter, _Lutra canadensis_ - E, W, R, rivers, lakes - Wolverine, _Gulo gulo_ - E, W, A, coniferous forests, alpine meadows - Least weasel, _Mustela rixosa_ - E, R, open forests, grasslands - Shorttail weasel, _Mustela erminea_ - E, W, A, coniferous forests, meadows - Longtail weasel, _Mustela frenata_ - E, W, A, open forests, meadows - Mink, _Mustela vison_ - E, W, creek and lake edges - Marten, _Martes americana_ - E, W, A, coniferous forests - Fisher, _Martes pennanti_ - E, W, R, coniferous forests - - Lagomorphs - Pika, _Ochotona princeps_ - E, W, A, rockslides - Snowshoe hare, _Lepus americanus_ - E, W, coniferous forests - Whitetail jackrabbit, _Lepus townsendii_ - E, W, R, grasslands - - Squirrels - Hoary marmot, _Marmota caligata_ - E, W, A, rocky areas, alpine meadows - Richardson ground squirrel, _Spermophilus richardsonii_ - E, R, grasslands - Columbian ground squirrel, _Citellus columbianus_ - E, W, A, open woodlands, grasslands, alpine meadows - Thirteen-lined ground squirrel, _Spermophilus tridecemlineatus_ - E, R, grasslands - Golden-mantled squirrel, _Spermophilus lateralis_ - E, W, A, high, open forests; rocky areas - Least chipmunk, _Eutamias minimus_ - E, W, A, high, open forests; brushy, rocky areas; alpine meadows - Yellow pine chipmunk, _Eutamias amoenus_ - E, W, open forests; brushy, rocky areas - Redtail chipmunk, _Eutamias ruficaudus_ - E, W, open forests; brushy, rocky areas - Red squirrel, _Tamiasciurus hudsonicus_ - E, W, coniferous forests - Northern flying squirrel, _Glaucomys sabrinus_ - E, W, coniferous forests; nocturnal - - Pocket gophers - Northern pocket gopher, _Thomomys talpoides_ - E, W, A, meadows - - [Illustration: Beaver] - - Beaver - Beaver, _Castor canadensis_ - E, W, streams, lakes - - Voles and kin - Deer mouse, _Peromyscus maniculatus_ - E, W, A, forests, grasslands, alpine meadows - Bushytail woodrat, _Neotoma cinerea_ - E, W, A, rocky areas, old buildings - Northern bog lemming, _Synaptomys borealis_ - W, R, coniferous forests - Mountain phenacomys, _Phenacomys intermedius_ - E, W, A, coniferous forests, alpine meadows - Boreal redback vole, _Clethrionomys gapperi_ - E, W, coniferous forests - Meadow vole, _Microtus pennsylvanicus_ - E, W, open forests, meadows; along streams; marshy areas - Longtail vole, _Microtus longicaudus_ - E, W, coniferous forests, grasslands - Water vole, _Arvicola richardsoni_ - E, W, A, high-elevation stream and lake edges - Muskrat, _Ondatra zibethica_ - W, streams, lakes, marshy areas - Western jumping mouse, _Zapus princeps_ - E, W, A, grasslands, alpine meadows - - Deer - Wapiti (American elk), _Cervus canadensis_ - E, W, A, open forests, meadows - Mule deer, _Odocoileus hemionus_ - E, W, A, open forests, meadows, often at high elevations - Whitetail deer, _Odocoileus virginianus_ - E, W, coniferous forests, meadows, creek and river bottoms - Moose, _Alces alces_ - E, W, coniferous forests, lakes, slow streams, marshy areas - - [Illustration: Mountain goat] - - Bovids - Mountain goat, _Oreamnos americanus_ - E, W, A, high peaks and meadows - Bighorn, _Ovis canadensis_ - E, A, open mountainous areas - - -Reptiles and Amphibians of Glacier National Park - -Note: This check list is based upon actual specimens in the Park and -other collections, according to Dr. Royal Brunson, Montana State -University. - - Reptiles - Great Basin Garter Snake, _Thamnophis elegans vagrans_ - A large garter snake of mountainous areas, usually with large spots. - - Great Plains Red-sided Garter Snake, _Thamnophis ordinoides - parietalis_ - Dorsal stripes varying from yellow to blue or black. Usually found - near water. - - Hypothetical List: - Rubber Boa, _Charina bottae utahensis_ - May occur in rock slides or, possibly, in forested areas, on either - side of the Divide. - - Gopher Snake, _Pituophis catenifer sayi_ - May occur along eastern boundary (Great Plains). - - Yellow-bellied Blue Racer, _Coluber constrictor mormon_ - May occur on eastern boundary of Park along border of Great Plains. - - Painted Turtle, _Chrysemys picta_ - May occur in ponds and sluggish waters from Upper Sonoran Zone to - Canadian Zone. - - Western Skink, _Eumeces skiltonianus_ - May occur in Transition Zone along western border of Park. - - [Illustration: Northern Alligator Lizard] - - Northern Alligator Lizard, _Gerrhonotus coeruleus principis_ - May occur in Transition Zone along western border of Park. - - Amphibians - Tiger Salamander, _Ambystoma tigrinum melanostrictum_ - Ground color either black or bluish-black, with large spots or - blotches of yellow. - - Long-toed Salamander, _Ambystoma macrodactylum_ - Ground color black or dark brown; wide band of yellow extends from - back of head to tip of tail. - - Northwestern Toad, _Bufo boreas boreas_ - Widely distributed over entire Park. (Also known as Columbian, - Northern, or Western Toad.) - - [Illustration: Western Spotted Frog] - - Western Spotted Frog, _Rana pretiosa pretiosa_ - Widely distributed over entire Park. (Also known as Western or Pacific - Frog.) - - Green Frog, _Rana clamitans_ - One specimen, from Bowman Lake. (Chicago Natural History Museum) - - Tailed Frog, _Ascaphus truei_ - Should be fairly common, although it is not often taken. - - Pacific Tree-toad, _Hyla regilla_ - Small size and disks on fingers and toes identify this species. Common - throughout Park. - - -Fishes of Glacier National Park - -Classification and common scientific names are from: "A List of Common -and Scientific Names of Fishes from the United States and Canada," -American Fisheries Society Publication No. 2, 1960. - - Key to symbols: - N Species native to at least one major drainage of the Park. - I Non-native species, having been introduced into Park waters by man. - S A species of sporting qualities and valued for recreational angling. - 1 Waterton Drainage - 2 Belly River Drainage - 3 Swiftcurrent Drainage - 4 St. Mary Drainage - 5 Two Medicine Drainage - 6 Middle Fork Flathead River Drainage (exclusive of McDonald Valley) - 7 McDonald Valley Drainage - 8 North Fork Flathead River Drainage - - [Illustration: Lake Trout] - - Family _Salmonidae_ (trouts, whitefishes, and grayling) - Lake Whitefish, _Coregonus clupeaformis_ (I) (1, 2, 3, 4, 7) - Pygmy Whitefish, _Prosopium coulteri_ (N) (7) - Mountain Whitefish, _Prosopium williamsoni_ (N) (S) (1, 2, 3, 4, 5, 6, - 7, 8) - Kokanee (Sockeye) Salmon, _Oncorhyncus nerka_ (I) (S) (3, 7, 8) - Cutthroat Trout, _Salmo clarki_ (N) (S) (1, 2, 3, 4, 5, 6, 7, 8) - Rainbow Trout, _Salmo gairdneri_ (I) (S) (1, 2, 3, 4, 5, 7) - Brook Trout, _Salvelinus fontinalis_ (I) (S) (1, 2, 3, 4, 5, 6, 7) - Dolly Varden, _Salvelinus malma_ (N) (S) (1, 2, 3, 4, 6, 7, 8) - Lake Trout, _Salvelinus namaycush_ (N) (S) (1, 2, 4, 5, 7, 8) - Arctic Grayling, _Thymallus arcticus_ (I) (S) (2, 8) - - Family _Esocidae_ (pikes) - Northern pike, _Esox lucius_ (N) (S) (1, 2, 3) - - [Illustration: Redside Shiner] - - Family _Cyprinidae_ (minnows and carps) - Longnose Dace, _Rhinichthys cataractae_ (N) (2, 3, 4, 5, 6, 7, 8) - Northern Pearl Dace, _Margariscus margarita_ (N) (3, 5) - Redside Shiner, _Richardsonius balteatus_ (N) (7, 8) - Streamline Chub, _Hybopsis dissimilis_ (N) (1, 3) - Northern Squawfish, _Ptychocheilus oregonensis_ (N) (7, 8) - - [Illustration: White Sucker] - - Family _Catostomidae_ (suckers) - White Sucker, _Catostomus commersoni_ (N) (1, 2, 3, 4, 5) - Largescale Sucker, _Catostomus macrocheilus_ (N) (6, 7, 8) - Longnose Sucker, _Catostomus catostomus_ (N) (1, 2, 3, 4, 5, 6, 7, 8) - - Family _Gadidaie_ (codfishes and hakes) - Burbot, _Lota lota_ (N) (S) (1, 4) - - Family _Cottidae_ (sculpins) - Mottled sculpin, _Cottus bairdi_ (N) (5, 6, 7, 8) - Spoonhead sculpin, _Cottus ricei_ (N) (1, 2, 3, 4) - - -Birds of Glacier National Park - - Key to symbols: - E--occurs on east side of the park (east of the Divide) - W--occurs on west side of the park (west of the Divide) - A--occurs in alpine areas - ab--abundant - c--common - u--uncommon - r--rare - i--introduced - a--accidental - - [Illustration: Common Loon] - - Loons - Common Loon E, W, ab - Arctic Loon? - Red-throated Loon? - - [Illustration: Western Grebe] - - Grebes - Red-necked Grebe E, W, c - Horned Grebe E, W, ab - Eared Grebe E, W, c - Western Grebe E, W, u - Pied-billed Grebe E, W, r - - Pelicans, Cormorants - White Pelican E, W, u - Double-crested Cormorant E, r - - [Illustration: Great Blue Heron] - - [Illustration: American Bittern] - - Herons, Bitterns - Great Blue Heron E, W, c - Black-crowned Night Heron a - American Bittern, W, r - - [Illustration: Mallard] - - [Illustration: Wood Duck] - - [Illustration: Ruddy Duck] - - Swan, Geese, Ducks - Whistling Swan E, W, ab - Trumpeter Swan E, W, r - Canada Goose E, W, c - Snow Goose E, W, c - Ross' Goose E, W, r - Mallard E, W, ab - Gadwall E, W, r - Pintail E, W, c - Green-winged Teal E, W, c - Blue-winged Teal E, W, u - Cinnamon Teal E, W, u - European Widgeon E, W, c - American Widgeon E, W, ab - Northern Shoveler E, W, c - Wood Duck E, W, r - Redhead E, W, c - Ring-necked Duck E, W, u - Canvasback E, W, u - Lesser Scaup E, W, c - Greater Scaup? - Common Goldeneye E, W, c - Barrow's Goldeneye E, W, ab - Bufflehead E, W, u - Harlequin Duck E, W, c - White-winged Scoter E, W, r - Ruddy Duck E, W, c - Hooded Merganser E, W, u - Common Merganser E, W, ab - Red-breasted Merganser, E, W, u - - [Illustration: Cooper's Hawk] - - [Illustration: Marsh Hawk] - - Vultures, Hawks, Eagles - Turkey Vulture E, W, r - Goshawk E, W, c - Sharp-shinned Hawk E, W, u - Cooper's Hawk E, W, u - Red-tailed Hawk E, W, c - Red-shouldered Hawk a - Swainson's Hawk E, W, c - Rough-legged Hawk E, W, r - Ferruginous Hawk E, W, u - Golden Eagle, E, W, A, c - Bald Eagle, E, W, ab - Marsh Hawk E, W, ab - Osprey E, W, ab - Prairie Falcon E, W, A, r - Peregrine Falcon E, W, r - American Kestrel E, W, c - - [Illustration: Sharp-tailed Grouse] - - Grouse, Ptarmigans - Blue Grouse, E, W, ab - Spruce Grouse E, W, ab - Ruffed Grouse E, W, ab - Sharp-tailed Grouse E, r - White-tailed Ptarmigan A, c - Willow Ptarmigan ? - Ring-necked Pheasant E, W, r, i - Gray Partridge E, W, r, i - - Cranes - Sandhill Crane E, r - - [Illustration: American Coot] - - Rails, Coots - Sora E, W, r - American Coot E, W, ab - - [Illustration: Greater Yellowlegs] - - Shorebirds - Killdeer E, W, c - Black-bellied Plover E, r - Common Snipe E, W, c - Long-billed Curlew E, r - Upland Sandpiper E, r - Spotted Sandpiper E, W, A, ab - Solitary Sandpiper E, r - Willet, E, r - Pectoral Sandpiper E, r - Baird's Sandpiper E, W, r - Lesser Yellowlegs, E, W r - Greater Yellowlegs E, W, r - American Avocet E, W, u - Northern Phalarope E, W, r - Wilson's Phalarope E, W, u - Black Turnstone ? - Long-billed Dowitcher E, W, r - - [Illustration: Herring Gull] - - Gulls, Terns - Herring Gull E, W, r - California Gull E, W, ab - Ring-billed Gull E, W, c - Franklin's Gull E, W, c - Bonaparte's Gull E, u - Forster's Tern E, W, u - Common Tern E, r - Caspian Tern a - Black Tern E, W, u - - [Illustration: Mourning Dove] - - Doves, Pigeons - Band-tailed Pigeon E, W, r - Mourning Dove E, W, c - Rock Dove E, W, r, i - - [Illustration: Great Horned Owl] - - Owls - Screech Owl E, W, r - Great Horned Owl E, W, ab - Snowy Owl E, W, u - Hawk Owl E, W, u - Pygmy Owl E, W, ab - Barred Owl E, W, c - Great Gray Owl E, W, u - Long-eared Owl E, W, r - Short-eared Owl, E, W, c - Boreal Owl E, W, r - Saw-whet Owl E, W, u - - [Illustration: Common Nighthawk] - - Nighthawks, Swifts - Common Nighthawk E, W, ab - Black Swift E, W, u - Vaux's Swift E, W, ab - White-throated Swift W, A, r - - Hummingbirds - Broad-tailed Hummingbird E, W, r - Rufous Hummingbird E, W, A, ab - Calliope Hummingbird E, W, A, ab - Black-chinned Hummingbird E, W, r - - [Illustration: Belted Kingfisher] - - Kingfishers - Belted Kingfisher E, W, ab - - Woodpeckers - Common Flicker E, W, ab - Pileated Woodpecker E, W, ab - Red-headed Woodpecker E, W, r - Lewis' Woodpecker E, W, c - Yellow-bellied Sapsucker E, W, ab - Williamson's Sapsucker E, W, u - Hairy Woodpecker E, W, ab - Downy Woodpecker E, W, ab - Black-backed Three-toed Woodpecker E, W, ab - Northern Three-toed Woodpecker E, W, ab - - [Illustration: Ash-throated Flycatcher] - - Flycatchers - Eastern Kingbird E, W, ab - Western Kingbird E, W, u - Ash-throated Flycatcher a - Say's Phoebe E, W, r - Willow Flycatcher E, W, c - Hammond's Flycatcher E, W, ab - Olive-sided Flycatcher E, W, ab - Western Flycatcher E, r - Western Wood Peewee E, W, c - - Larks - Horned Lark E, W, A, ab - - [Illustration: Barn Swallow] - - Swallows - Violet-green Swallow E, W, A, ab - Tree Swallow E, W, ab - Bank Swallow E, W, ab - Rough-winged Swallow E, W, u - Barn Swallow E, W, u - Cliff Swallow E, W, A, ab - - [Illustration: Common Crow] - - Jays, Magpies, Crows - Gray Jay E, W, ab - Blue Jay E, W, r - Steller's Jay E, W, ab - Black-billed Magpie E, W, ab - Common Raven E, W, A, ab - Common Crow E, W, ab - Clark's Nutcracker E, W, A, ab - - Chickadees - Black-capped Chickadee E, W, ab - Mountain Chickadee E, W, ab - Boreal Chickadee E, W, r - Chestnut-backed Chickadee E, W, u - - Nuthatches, Creepers - White-breasted Nuthatch E, W, u - Red-breasted Nuthatch E, W, ab - Brown Creeper E, W, ab - - [Illustration: Winter Wren] - - Dippers, Wrens - Dipper E, W, A, ab - House Wren E, W, u - Winter Wren E, W, ab - Long-billed Marsh Wren a - Rock Wren E, W, u - - Catbirds, Thrashers - Gray Catbird E, W, u - - [Illustration: Mountain Bluebird] - - Thrushes, Bluebirds, Solitaires - American Robin E, W, A, ab - Varied Thrush E, W, ab - Hermit Thrush E, W, ab - Swainson's Thrush E, W, ab - Veery E, W, c - Western Bluebird E, W, r - Mountain Bluebird E, W, A, ab - Townsend's Solitaire E, W, A, ab - - Kinglets - Golden-crowned Kinglet E, W, ab - Ruby-crowned Kinglet E, W, ab - - Pipits - Water Pipit E, W, A, ab - - [Illustration: Cedar Waxwing] - - Waxwings - Bohemian Waxwing E, W, ab - Cedar Waxwing E, W, ab - - Shrikes - Loggerhead Shrike E, W, r - Northern Shrike E, W, r - - [Illustration: Starling] - - Starlings - Starling E, W, c, i - - [Illustration: Red-eyed Vireo] - - Vireos - Solitary Vireo E, W, ab - Red-eyed Vireo E, W, ab - Warbling Vireo E, W, ab - - Warblers - Black and White Warbler W, r - Tennessee Warbler E, W, r - Orange-crowned Warbler E, W, r - Nashville Warbler E, W, r - Yellow Warbler E, W, ab - Yellow-rumped Warbler E, W, ab - Townsend's Warbler E, W, ab - Northern Waterthrush E, W, ab - MacGillivray's Warbler E, W, ab - Common Yellowthroat E, W, ab - Wilson's Warbler E, W, ab - American Redstart E, W, ab - Yellow-breasted Chat ? - - [Illustration: House Sparrow] - - Weaver Finches - House Sparrow E, W, r, i - - Blackbirds, Orioles - Bobolink E, r - Western Meadowlark E, W, u - Red-winged Blackbird E, W, ab - Northern Oriole E, W, r - Brewer's Blackbird E, W, u - Rusty Blackbird E, W, r - Yellow-headed Blackbird E, r - Common Grackle E, r - Brown-headed Cowbird E, W, c - - [Illustration: Evening Grosbeak] - - Tanagers, Grosbeaks - Western Tanager E, W, ab - Evening Grosbeak E, W, ab - Pine Grosbeak E, W, ab - Black-headed Grosbeak E, W, r - - [Illustration: American Goldfinch] - - Finches, Sparrows, Buntings - Lazuli Bunting E, W, c - Lark Bunting E, W, r - Snow Bunting E, W, c - Cassin's Finch E, W, A, ab - Gray-crowned Rosy Finch E, W, A, ab - American Goldfinch E, W, u - Common Redpoll E, W, c - Pine Siskin E, W, A, ab - Red Crossbill E, W, ab - White-winged Crossbill E, W, u - Rufous-sided Towhee E, W, u - Green-tailed Towhee E, W, r - Savannah Sparrow E, W, c - LeConte's Sparrow E, W, u - Vesper Sparrow E, W, ab - Tree Sparrow E, W, r - Chipping Sparrow E, W, A, ab - Brewer's Sparrow E, W, r - Harris' Sparrow E, W, r - White-crowned Sparrow E, W, A, ab - Fox Sparrow E, W, A, ab - Lincoln's Sparrow E, W, A, c - Song Sparrow E, W, ab - Dark-eyed Junco E, W, c - McCown's Longspur E, c - Lapland Longspur E, W, c - Chestnut-collared Longspur E, c - - - - - Suggested Reading - - -Alexander, Taylor R. and George S. Fichter, _Ecology_ (a Golden guide). - Western Publishing Co., Inc., Racine, Wis. 1973. - -Alt, David D. and Donald W. Hyndman, _Rocks, Ice and Water, the Geology - of Waterton-Glacier Park_. Mountain Press Publishing Co., - Missoula, Mont. 1973. - -Baker, William, et. al., _Wildlife of the Northern Rocky Mountains_. - Naturegraph Co., Healdsburg, Calif. 1961. - -Borland, Hal, _The History of Wildlife in America_. National Wildlife - Federation, Washington, D.C. 1975. - -Brooks, Maurice, _The Life of The Mountains_. McGraw-Hill, New York. - 1967. - -Costello, David F., _The Mountain World_. Thomas Y. Crowell Co., New - York. 1975. - -Craighead, John J., et. al., _A Field Guide to Rocky Mountain - Wildflowers_. Houghton Mifflin Co., Boston. 1963. - -Dobie, J. Frank, _The Voice of the Coyote_. Little, Brown and Co., - Boston. 1950. - -Farb, Peter, _Face of North America_. Harper and Row, New York. 1963. - -Gildart, Robert C., _Meet the Mammals of Waterton-Glacier_. Glacier - Natural History Association, Inc. Thomas Printing, Inc., - Kalispell, Mont. 1975. - -McCormick, Jack, _The Life of the Forest_. McGraw-Hill, New York. 1966. - -Milne, Lorus and Margery Milne, _The Balance of Nature_. Alfred A. - Knopf, Inc., New York. 1960. - -Nelson, Alan G., _Wildflowers of Glacier National Park_. Nelson, Great - Falls, Mont. 1970. - -Peattie, Donald Culross, _A Natural History of Western Trees_. Bonanza - Books, New York. 1953. - -Ruhle, George C., _Roads and Trails of Waterton-Glacier Parks_. John W. - Forney, Minneapolis, Minn. 1972. - -Shea, David S., _Animal Tracks of Glacier National Park_. Special - Bulletin No. 11, Glacier Natural History Association, Inc., West - Glacier, Mont., 1969. - -Storer, John H., _The Web of Life_. Devin-Adair Co., Old Greenwich, - Conn. 1953. - -Zwinger, Ann H. and Beatrice E. Willard, _Land Above the Trees_. Harper - and Row, New York. 1972. - - [Illustration: WATERTON LAKES NATIONAL PARK--GLACIER NATIONAL PARK] - - Using Metrics - - As we go to press with this book, the United States is in the early - stages of conversion to the metric system of measurement, and though - we urge you to think metric--for most of the world does--we provide - this table to help you understand the measurements given in the - book. - - To convert from to multiply by - - Millimeters Sixteenth-inches 0.6301 - Centimeters Inches 0.3937 - Meters Feet 3.2808 - Kilometers Miles 0.6214 - Hectares Acres 2.4711 - Hectares Square miles 0.00386 - Grams Troy Ounces 0.0322 - Kilograms Pounds 2.2046 - Degrees--Celsius Degrees--Fahrenheit 1.8, and add 32 - - [Illustration: Temperature Conversion Chart] - - [Illustration: Length Conversion Chart] - - Drawings from David S. Shea, _Animal Tracks of Glacier National - Park_ - - [Illustration: red fox, - hind foot, in mud - 53 mm.] - - [Illustration: mule deer, - adult buck, in snow - 72 mm.] - - [Illustration: badger, - left front foot, in mud - 43 mm.] - - [Illustration: coyote, - hind foot, in snow - 63 mm.] - - About the Author - - Greg Beaumont's interest in Glacier National Park dates from 1963, - when he was a summer employee at Lake McDonald Lodge. In 1966 he and - his wife were fire-control lookouts on Numa Ridge in the Bowman - Valley. Now a free-lance writer-photographer, he lives with his - family in Lincoln, Nebraska. - - National Park Service - U.S. Department of the Interior - - As the Nation's principal conservation agency, the Department of the - Interior has responsibility for most of our nationally owned public - lands and natural resources. This includes fostering the wisest use - of our land and water resources, protecting our fish and wildlife, - preserving the environmental and cultural values of our national - parks and historical places, and providing for the enjoyment of life - through outdoor recreation. The Department assesses our energy and - mineral resources and works to assure that their development is in - the best interests of all our people. The Department also has a - major responsibility for American Indian reservation communities and - for people who live in Island Territories under U.S. administration. - - - - - Transcriber's Notes - - ---Retained publication information from the printed edition: this eBook - is public-domain in the country of publication. - ---Corrected a few palpable typos. - ---Included a transcription of the text within some images. - ---In the text versions only, text in italics is delimited by - _underscores_. - - - - - - - -End of the Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -*** END OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - -***** This file should be named 55150-8.txt or 55150-8.zip ***** -This and all associated files of various formats will be found in: - http://www.gutenberg.org/5/5/1/5/55150/ - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - -Updated editions will replace the previous one--the old editions will -be renamed. - -Creating the works from print editions not protected by U.S. copyright -law means that no one owns a United States copyright in these works, -so the Foundation (and you!) can copy and distribute it in the United -States without permission and without paying copyright -royalties. 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} -span.pn { display:inline-block; width:4.7em; text-align:left; margin-left:0; text-indent:0; }</style> -</head> -<body> - - -<pre> - -The Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -This eBook is for the use of anyone anywhere in the United States and most -other parts of the world at no cost and with almost no restrictions -whatsoever. You may copy it, give it away or re-use it under the terms of -the Project Gutenberg License included with this eBook or online at -www.gutenberg.org. If you are not located in the United States, you'll have -to check the laws of the country where you are located before using this ebook. - -Title: Many-Storied Mountains - The Life of Glacier National Park - -Author: Greg Beaumont - -Release Date: July 19, 2017 [EBook #55150] - -Language: English - -Character set encoding: UTF-8 - -*** START OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - - - - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - - - - - - -</pre> - -<div id="cover" class="img"> -<img id="coverpage" src="images/cover.jpg" alt="Many-storied Mountains: The Life of Glacier National Park" width="600" height="647" /> -</div> -<div class="verse"> -<p class="t0">★GPO:1978-261-215/3</p> -<p class="t0">For sale by the</p> -<p class="t0">Superintendent of Documents,</p> -<p class="t0">U.S. Government Printing Office,</p> -<p class="t0">Washington, DC 20402.</p> -<p class="t0">Stock Number 024-005-00709-1.</p> -</div> -<div class="verse"> -<p class="t0">Library of Congress Cataloging In Publication Data</p> -</div> -<div class="verse"> -<p class="t0">Beaumont, Greg, 1943-</p> -<p class="t0">Many-storied mountains.</p> -</div> -<div class="verse"> -<p class="t0">(Natural history series)</p> -<p class="t0">1. Natural history—Montana—Glacier National Park.</p> -<p class="t0">2. Glacier National Park. I. Title. II. Series: Natural history series (Washington, D.C.)</p> -<p class="t0">OH105 M9B43 <span class="hst">500.9′786′52</span> <span class="hst">78-606071</span></p> -</div> -<div class="box"> -<h1>Many-storied Mountains -<br />The Life of Glacier National Park</h1> -<p class="center"><span class="smaller">Written and -<br />photographed by</span> -<br />Greg Beaumont</p> -<p class="center smaller">1978 -<br />Natural History Series -<br />Division of Publications -<br />National Park Service -<br />U.S. Department of the Interior</p> -</div> -<div class="pb" id="Page_i">i</div> -<div class="img" id="fig1"> -<img src="images/p001.jpg" alt="" width="1000" height="543" /> -<p class="pcap">The landform of Glacier National Park is a monument -to the power of moving ice. This view from Stoney -Indian Pass is startlingly different -from the scene of a million years ago, when the glaciers -of the Pleistocene were sculpturing the land. Only the -higher peaks would then have been visible above the -blanket of ice that flowed like a slow-moving river -down into the Mokowanis Valley and out into the -Great Plains beyond.</p> -</div> -<div class="pb" id="Page_iii">iii</div> -<h3>About This Book</h3> -<p>This natural history of the mountain -wilderness called Glacier National Park -is not a guidebook, but provides an overview -of the ecology of the region. At the -same time, it is a personal statement, -revealing one individual’s response to this -rugged, delicate land.</p> -<p>For their consistent cooperation and -helpfulness, I wish especially to thank -Chief Naturalist Ed Rothfuss and his -capable staff. Technical and field assistance -came from many; for special -thanks, I would like to single out Art -Sedlack, Francis Singer, Bert Gildart, -Walt Martin, Craig Kuchel, and Danny -On. The manuscript profited greatly from -the criticism of Douglas Chadwick, to -whom I am deeply grateful.</p> -<p><span class="lr">—G.B.</span></p> -<p class="tb">The National Park Service Division of -Publications gratefully acknowledges the -financial support given this book project -by the Glacier Natural History Association, -Inc., West Glacier, Mont.</p> -<div class="pb" id="Page_iv">iv</div> -<h2 class="center">Contents</h2> -<dl class="toc"> -<dt><a href="#c1"><b>Song of the High Peaks</b></a> <b>1</b></dt> -<dt><a href="#c2"><b>Cycles and Seasons</b></a> <b>5</b></dt> -<dd><a href="#c3">Bedrock: The First Story</a> <b>6</b></dd> -<dd><a href="#c4">The Rising of the Sun and the Running of the Deer: A Glacier Year</a> <b>39</b></dd> -<dt><a href="#c5"><b>Plant-and-Animal Communities</b></a> <b>43</b></dt> -<dd><a href="#c6">Over Going-to-the-Sun Road</a> <b>44</b></dd> -<dd><a href="#c7">Groves and Grasslands: The Prairie Sea</a> <b>46</b></dd> -<dd><a href="#c8">The Forest</a> <b>70</b></dd> -<dd><a href="#c9">Scrub Forest</a> <b>105</b></dd> -<dd><a href="#c10">Tundra</a> <b>109</b></dd> -<dd><a href="#c11">Water Communities</a> <b>114</b></dd> -<dt><a href="#c12"><b>Shooting Stars</b></a> <b>121</b></dt> -<dt><a href="#c13"><b>Appendix</b></a> <b>125</b></dt> -<dt class="jl"><b>Pictorial Features</b></dt> -<dd><a href="#f2fig1">The Mountains of Glacier</a> <b>10</b></dd> -<dd><a href="#f2fig2">The Forests of Glacier</a> <b>48</b></dd> -<dd><a href="#f2fig3">The Vital Predator</a> <b>78</b></dd> -<dd><a href="#f2fig4">Protective Coloration</a> <b>84</b></dd> -<dd><a href="#f2fig5"><i>Ursus arctos horribilus:</i> The Vulnerable King</a> <b>88</b></dd> -<dd><a href="#f2fig6">Bald Eagles and Kokanee Salmon: A Recent Gathering</a> <b>92</b></dd> -<dd><a href="#f2fig7">A Triumph of Many Colors</a> <b>96</b></dd> -<dd><a href="#f2fig8">Fire Succession: Key to Continuity</a> <b>100</b></dd> -</dl> -<p class="tb"><span class="small">Illustrations by Celia Strain/Morgan-Burchette Assoc.</span></p> -<div class="pb" id="Page_v">v</div> -<div class="img"> -<img src="images/p002.jpg" alt="Soaring eagle" width="700" height="770" /> -</div> -<div class="pb" id="Page_1">1</div> -<h2 id="c1"><span class="small">Song of the High Peaks</span></h2> -<div class="pb" id="Page_2">2</div> -<p>April again and the wind turns on the Great -Plains. Wedges of geese, high and determined, -began this storm of spring, their -voices sharp as the morning frost. Sicklebills -cry to claim the land, sandhill cranes wheel -and talk overhead, and everywhere the killdeer -shout. Pasqueflowers push the bleak -soil aside, beginning the westward rush that -I must join, seeking again the sight of -mountains.</p> -<p>In Glacier National Park the land is -folded up. On the east, Chief Mountain, Curly -Bear, and Rising Wolf break the prairie’s -hold. When the early French fur trappers -saw these peaks glistening in the distance -with summer-long snows and perpetual ice, -they named this region “the land of shining -mountains.” But for all the ice and snow -that reflect the summer sun, the park’s present -glaciers are but snowflakes compared to -the mighty rivers of ice that carved this -land. Glaciation, the magnificent sculptor, -left its bold signature everywhere, and this -park honors with its name the force that -shaped it.</p> -<p>But the essential excitement of this land -is more than cliff face, spire, and sudden -storm. It comes to you when you realize -that here is an aggregation of dramatically -differing life zones, where a day’s walk can -easily take you from prairie and forest to -treelimit and tundra; where a dense forest -of redcedar and hemlock, similar to the rain -forests of the Pacific coast, exists a score of -kilometers from the great prairie sea.</p> -<p>Or it comes when you discover that -these mountains—young and sharp with -shadows, snow-jeweled and newly gowned -with forests—are chiseled from the oldest -unaltered sedimentary rocks on earth.</p> -<p>I come from the prairie and love its -broad strokes; I’ve learned to hear the singing -in the grass and to see those long, slow -seasons soar the level horizons like gliding -hawks. But here I learned to match my days -against a wild earth, and in me grew the -mysterious need to know a mountain from -its every side. Mountains that wear the dawn -like yellow hats, repeated in the named and -nameless lakes. Mountains that stretch the -storms between them and balance rainbows -ridge to ridge.</p> -<p>I must see again the secret forest places, -where the paleflowered wood-nymphs hover -like a breath, and know once more the endless -meadows painted camas blue.</p> -<p>I need the perfect freedom of this land, -to be able to say, <i>today I will climb Siyeh</i>: -to stand, for a time, on the rugged shoulders -of this upright earth.</p> -<div class="pb" id="Page_3">3</div> -<div class="img" id="fig2"> -<img src="images/p003.jpg" alt="" width="681" height="700" /> -<p class="pcap">The sharp spire of little Matterhorn and the broad face -of Mt. Edwards loom above Going-to-the-Sun Road in -the upper McDonald Valley. During warm days in spring -the valleys of the park resound with the thunder of -avalanches.</p> -</div> -<div class="pb" id="Page_4">4</div> -<div class="img"> -<img src="images/p004.jpg" alt="Twilight view." width="700" height="772" /> -</div> -<div class="pb" id="Page_5">5</div> -<h2 id="c2"><span class="small">Cycles and Seasons</span></h2> -<div class="pb" id="Page_6">6</div> -<h3 id="c3">Bedrock: The First Story</h3> -<p>On the trail that connects the Logan Pass -visitor center to Hidden Lake overlook -there is a shallow pond. Near Hidden Pass, -it collects its meltwater from the Continental -Divide and sends it down the shallow gorge -that drains the Hanging Gardens; as a -waterfall it plunges into the upper St. Mary -Valley where it becomes Reynolds Creek; -joined by other tributaries, it continues its -long journey to Hudson Bay.</p> -<p>The surface of this pond is seldom still, -for the wind treats it like a sea. Because the -water is shallow, the wave action wrinkles -the bottom mud into ripple patterns, mimicking -the churning waves.</p> -<p>I like to come here early in the morning. -Sometimes, arriving before the wind awakes, -I catch reflections of the surrounding mountains. -Beyond the low bench of Logan Pass -the Garden Wall begins, running northward -with the Divide. In the eastern valley the -pitched peak of Going-to-the-Sun hunkers in -the morning light like a tensed warrior. To -the south, the incisor Bearhat, beautiful -cloud cutter of Hidden Lake Valley, juts -above the nearby saddle of the pass. But -over this place, standing as fresh monuments -to an age of ice, tower the cliffs of Clements -and the pyramid Reynolds.</p> -<p>I am sitting on a wedge of red rock. -Its surface exhibits a wrinkled pattern identical -to the ripples in the soft mud of the -shallow pond. The distance is not great; -with a stick I could reach out and touch the -mud. Yet this represents a gulf no bird can -fly, for between the ripples of this rock and -the ripples of this mud lie billions of vanished -mornings, a constellation of years.</p> -<p>These red, green, tan, white, black and -purple bands of rock that layer Glacier’s -mountains comprise the oldest unaltered -sedimentary rocks on Earth. They were laid -down in Precambrian time, more than a -billion years ago, when life was just beginning, -as the deposits of an inland sea.</p> -<p>For millions of years, sand, mud and -carbonates washed into the ancient sea, -compressing the lower layers into mudstones -and limestones, building up a sediment -thickness that may have been as much as -10,000 meters (<i>see</i> metric conversion table -on <a href="#Page_136">page 136</a>).</p> -<p>When we look at the sharp contours of -Glacier’s mountains, we see the evidence of -uplift, overthrust and glaciation. But on the -geologic clock these are recent events, a -mere eyeblink of time ago. For the vast -majority of years, the rocks lay undisturbed -and level beneath the sea and land.</p> -<p>To understand better the tremendous -time scale these rocks represent, we need a -way to visualize the vast collection of years. -If we were to make a movie of these geologic -events, we would first need to determine -how many years each minute should -represent. Since the Pleistocene lasted about -3,000,000 years (its four ice ages sculpting -the present muscle of this land), let us make -<span class="pb" id="Page_7">7</span> -each minute portray a million years. To -chronicle these rocks we will then need a -film 60 hours long!</p> -<p>Not until the fifty-seventh hour of our -film will the Mesozoic lowlands begin to -bulge with the coming Rocky Mountain -chain. During the long preceding hours we -would have seen little else but sea—withdrawing, -advancing, deep and shallow; yellow, -green, and brown with great colonies -of algae. Unseen below the water, lava has -spilled out occasionally on the sea bottom; -once, it intruded between the rock layers -below, forming the conspicuous, 60-meter-thick -band of black diorite that we see today -on many mountain faces in Glacier.</p> -<p>During this time of initial uplift an -amazing process is going on deep underground. -A major fault has developed, -fracturing the buckled layers of rock. A -vast mountain plate begins to slide eastward, -over-riding and submerging the rock layers -to the east and opening the wide trench -that is today the North Fork Valley. Known -as the Lewis Overthrust, this gigantic earth-force -has created an unusual situation: ancient -rock strata lying atop recent rock -strata.</p> -<p>Now less than 3 minutes of film remain. -The arrival of the ice is imminent. We look -at the landscape of featureless mountains and -wonder at the dramatic difference that this -last 3 million years will make. We do not -see the familiar forests and lakes, the -savage peaks, and the broad, deep valleys -of this present land. These mountains are -gentle, arid, and shallow-valleyed. The -vague outlines are there; we recognize the -general alignments of the drainage systems, -the bloated domes from which sharp peaks -will be cut. The mountains are connected -to one another by blunt ridges and smooth -saddles, and the shadows they cast are dull, -dunelike.</p> -<p>Suddenly the ice is there, filling the -landscape, with only the mountaintops protruding. -Four times in these last 3 minutes -of film the ice sheets advance and retreat, -each time leaving an altered landscape. -Strange lakes and forests fill the gaps between -the glacial invasions. Then we -see the mountains we now know come into -being rapidly, as if the land were being -hacked into shape by giant cleavers.</p> -<p>After this flicker of Pleistocene time, -the film ends, the forests return, and familiar -lakes shine beneath the sun again—these -lakes and forests we had thought to -be timeless.</p> -<p class="tb">■<br />Up springs the morning wind from Hidden -Valley, making the nearby alpine fir branches -whiz with its passing and shattering the perfect -reflection of Bearhat Peak on the pond. -From where I sit, it is a short distance to -Hidden Pass; so I leave the pond and walk -to the overlook to see again the fine basin -quarried by an ancient glacier.</p> -<p>Hidden Lake, deep, far below, so blue, -<span class="pb" id="Page_8">8</span> -fits into its cliffed, crooked valley like a -polished boomerang. Closely ringed by -ridge and peak—distant Sperry Glacier and -pointed Gunsight peering up from the -southern jumble, and broad Bearhat impossibly -close—this lovely lake is almost lost -amid such sharp proclamations of rock. Its -outlet gorge gives a narrow view across the -angled, hidden valleys of Avalanche and -McDonald, past the pyramid of Stanton, to -the low, faraway undulations of the Whitefish -Range.</p> -<p>Glaciation is a cruel master of mountains, -biting deeply into their bulk and leaving -sheer, spectacular contours when the -glaciers disappear. The landforms here attest -to their power, everywhere exhibiting -the effects of glaciation.</p> -<p>In eating back the mountain headwall, -alpine glaciers formed rounded depressions, -called cirques. Unlike the narrow -clefts left by running water, these broad, -deep basins look as though they were made -by ice-cream scoops gouging into the rock. -Hidden, Ptarmigan, Iceberg, and Avalanche -Lakes sit in well-developed cirque basins, -and many mountains are dimpled by the -beginnings of other cirques—the conspicuous -amphitheater on the south shoulder of -Heaven’s Peak, for example.</p> -<p>Occupying all major drainage systems, -glaciers modified the contour of the valleys, -changing them from their narrow, stream-cut -V-shapes into broad U-shapes. Into -these wide main valleys, waterfalls plunge -from higher, smaller valleys. Like rivers, -flowing glaciers have tributaries. Lacking -the ice mass and cutting power of the main -glaciers, these tributary ice fingers could not -bite as deeply into the bedrock. When the -ice melted, hanging valleys were left -stranded high above the main valley floor. -Hidden Lake sits in one of these hanging -valleys, and from it Hidden Creek plunges -750 meters into Avalanche Basin toward -McDonald Creek.</p> -<p>On my many previous visits to this pass -I have been too busy enjoying the wildflowers, -the weather, or the scenery to realize -what an open textbook of glaciation is -everywhere displayed.</p> -<p>I stand here on a small saddle of a pass. -Wherever glaciers met, passes, or cols, -were created. A high, notched pass like this -one (or Swiftcurrent or Gunsight) reveals -recent connections. Broad, lower passes, -such as Logan, resulted where the ice early -overran the mountain ridge and had a -chance to work longer.</p> -<p>Where two glaciers worked on opposing -sides of a ridge and failed to meet, they -formed an arête—a thin, steep-walled remnant -resembling a saw blade. Another ice -age would probably consume the park’s -many thin arêtes, such as the Garden Wall -and Ptarmigan Wall; but it would also -create new ones from existing ridges.</p> -<p>Further testimony to the sculpting -power of ice is presented by Mt. Reynolds, -looming to the east. The most dramatic -<span class="pb" id="Page_9">9</span> -feature of a glaciated landscape is the -pyramid-shaped mountain called a horn—and -Reynolds is a perfect example. Horns -were formed when three or more glaciers -cloaked the mountain, excavating its sides -toward its core and gradually transforming -its original domed shape into a sheer-sided -peak. Glacier has many remarkable horns, -from the sleek spire of St. Nicholas in the -south to exquisite Kinnerly in the northern -Kintla valley.</p> -<p>Sperry Glacier stares back at me from -the flank of Gunsight. Glaciers found in -the park today are not remnants of the -last ice phase, which ended here about -8,000 years ago, but are newly formed, -having come into existence some 4,000 -years ago. They reflect a cooling trend in -the present climate.</p> -<p>Shrinking steadily from their period of -greatest extent in the middle of the last -century, these modern glaciers finally stabilized -in the late 1940s and since then have -shown only a slight increase in area.</p> -<p>Movement distinguishes glaciers from -icefields, and the movement of ice is a force -on as well as a feature of a landscape. A -glacier excavates by abrading and plucking -at the rock. Alternately melting and freezing, -ice at the headwalls plucks out blocks of -rock. Ultimately the rocks are deposited -along the sides or at the feet of the glacier -as moraine debris. But as they move in the -grip of the ice, they constantly abrade the -rock surfaces they encounter. Polished rock -beds of past glaciers show striations—grooves -gouged by rock fragments imbedded -in the moving ice.</p> -<p>Flow rate of a glacier depends upon -the thickness of the ice and the degree of -slope. Under tremendous pressure, ice becomes -plastic, like thick taffy. Unlike kilometer-thick -continental glaciers, which may -move a hundred meters a day, small alpine -glaciers seldom progress more than two or -three centimeters per day.</p> -<p>Although a glacier moves, it gets nowhere -if in a state of equilibrium—when -annual melting equals annual accumulation. -Snow mass gained at the sun-shielded headwall -is usually lost as melt at the exposed -snout. Glaciers such as Sexton or Weasel -Collar, whose snouts perch on cliff edges, -also lose mass by calving. Thunder you hear -on a late-summer day near such a glacier -may actually be the sound of ice pushed off -from the lip of a cliff.</p> -<p>Walking back to the visitor center, I -suddenly stop where the trail skirts the steep -moraine of Mt. Clements. From the opposite -side of the moraine five mountain goats have -appeared. Spotting me on the trail below, -they also halt. But before I can get to my -camera they are off in a stiff-legged gallop, -running in single file along the crest of the -moraine to the distant safety of the mountain -face.</p> -<p>Moraines are ridges of rock debris piled -up along the edges and terminuses of glaciers. -Like a bracelet lying against the wall -of this mountain, the circle of steeply piled -debris marks the extent of a small, recently -vanished glacier. Ghost of the power that -once resided here, a stagnant icefield lies -beneath the confining walls of the moraine. -The recent accumulation of these rock fragments -is a mighty accomplishment, attesting -to the force of moving ice.</p> -<p><span class="lr"><i><span class="small">continued on <a href="#Page_38">p. 38</a></span></i></span></p> -<div class="pb" id="Page_10">10</div> -<div class="img" id="fig3"> -<img src="images/p005.jpg" alt="" width="1000" height="606" /> -<p class="pcap"><b id="f2fig1">The Mountains of Glacier</b></p> -<p class="pcapc">Lying astride the Continental Divide in the -Northern Rockies, Glacier is above all -else a mountain park. The special beauty -of its lakes, streams, and forests derives -from the microclimates and varied -topography and soil produced by -mountain-building and mountain-eroding -forces.</p> -</div> -<div class="pb" id="Page_12">12</div> -<div class="img" id="fig4"> -<img src="images/p006.jpg" alt="" width="1000" height="618" /> -<p class="pcap"><b>Overthrust Mountains</b></p> -<p class="pcapc"><b>1</b> A hypothetical block of the Earth’s -crust in the region of Glacier National -Park as it existed more than 60 million -years ago. The two layers shown actually -represent many strata of sedimentary -rocks.</p> -<p class="pcapc"><b>2</b> Lateral pressure begins to force the -rock layers to buckle.</p> -<p class="pcapc"><b>3</b> A large fold has been created, forcing -the rock strata to double over and -overturning some layers. A break, or -<i>fault</i>, is forming at the plane of greatest -stress.</p> -<p class="pcapc"><b>4</b> The break has been completed and the -strata west of the fault have slid eastward, -up and over the rocks east of the fault.</p> -<p class="pcapc"><b>5</b> The Glacier landscape today. Throughout -the millions of years during which the -folding, faulting, and overthrusting have -been taking place, the process of erosion -has continued; a thousand meters of -stratified rocks have been worn away, so -that only a remnant of the overthrust -layers can be seen today. Because -Glacier’s eastern slope represents the -eroded face of the overthrust block, the -mountain range rises precipitously from -the prairie, with no foothills breaking the -abrupt transition from open prairie to -mountain valley.</p> -</div> -<div class="pb" id="Page_13">13</div> -<div class="img" id="fig5"> -<img src="images/p006a.jpg" alt="" width="600" height="339" /> -<p class="pcap">The peaks in this photograph (a view to the northwest -from Marias Pass) are remnants of the overthrust block, -which moved eastward. The dividing line between -the light-colored rocks and the gray talus slopes -beneath them is the Lewis Overthrust Fault.</p> -</div> -<div class="pb" id="Page_14">14</div> -<div class="img" id="fig6"> -<img src="images/p007.jpg" alt="" width="1000" height="492" /> -<p class="pcap"><b>Glaciation</b></p> -<p class="pcapc"><b>1</b> This is how the landscape in this region -might have appeared before the onset of -the Pleistocene, millions of years ago. -Note the stream-eroded, V-shaped -valleys. The climate at that time was dry.</p> -<p class="pcapc"><b>2</b> Glaciers began to form high on the -peaks, crept downward, and joined to -form larger glaciers.</p> -<p class="pcapc"><b>3</b> After many centuries of glaciation, -tributary glaciers have cut back into the -peaks, forming basins called <i>cirques</i>. -Thick glaciers, moving rapidly and -carrying rock fragments, have abraded -the main valleys’ floors and sides, -widening and deepening the valleys into -characteristic U-shapes.</p> -</div> -<dl class="undent pcap"><dt>V-shaped Valley</dt> -<dt>Tributary Glacier</dt> -<dt>Unglaciated Peak</dt> -<dt>Headwall</dt> -<dt>Meltwater Stream</dt> -<dt>Nose of Glacier</dt> -<dt>Crevasse</dt></dl> -<div class="pb" id="Page_16">16</div> -<div class="img" id="fig7"> -<img src="images/p008.jpg" alt="" width="1000" height="337" /> -<p class="pcap"><b>4</b> In the present landscape, free of all but -remnant glaciers, small lakes called -<i>tarns</i> occupy many of the cirque basins; -and waterfalls plunge into the main -valleys from higher, shallower, tributary -valleys, called <i>hanging valleys</i>. <i>Alluvial -cones</i>—recent accumulations of rock -debris—have begun to build along the -valley walls. In the main valley, a <i>moraine</i> -(a deposit of rock materials left by the -retreating glacier) has formed a dam that -holds back a large lake.</p> -<p class="pcapc">During all this time, all parts of the terrain -not buried under ice and snow have been -weathered and eroded by nonglacial -forces. Thus the contours of the jagged -peaks and sheer cliffs have been -softened.</p> -</div> -<dl class="undent pcap"><dt>Unglaciated V-shaped Valley</dt> -<dt>U-shaped Valley</dt> -<dt>Hanging Valley</dt> -<dt>Cirque</dt> -<dt>Tarn</dt> -<dt>Alluvial Cone</dt> -<dt>Moraine</dt> -<dt>Morainal Lake</dt></dl> -<div class="pb" id="Page_17">17</div> -<div class="img" id="fig8"> -<img src="images/p008a.jpg" alt="" width="600" height="332" /> -<p class="pcap">Glacial landforms can be identified in this view of the -Mokowanis Valley.</p> -</div> -<div class="pb" id="Page_18">18</div> -<div class="img" id="fig9"> -<img src="images/p009.jpg" alt="" width="1000" height="456" /> -<p class="pcap"><b>A Divided Climate</b></p> -<p class="pcapc">Because of an eastward flow of cool, -moist Pacific air masses, the climate of -northwestern Montana, including the -western portion of Glacier National Park, -differs from that of other portions of -Montana. As a result of increased precipitation, -Glacier’s western valleys support -a rich flora, more typical of the Pacific -Northwest.</p> -<p class="pcapc"><b>West</b></p> -<p class="pcapc">Moist Pacific air</p> -<p class="pcapc">As the moisture-laden Pacific winds are pushed up the -windward slopes of Glacier’s mountains, the air cools -and water vapor condenses, forming fog or clouds. -Rain or snow begins to fall as the air continues to rise -and cool. By the time the air mass reaches the crest and -flows down the leeward slopes, most of the moisture -has been lost.</p> -<p class="pcapc">Western slopes average about 70 cm. of precipitation at -elevations between 900 and 1,100 m. Upper elevations -average 200 to 250 cm., mostly in the form of snow; and -300 to 500 cm. is common.</p> -<p class="pcapc"><b>East</b></p> -<p class="pcapc">Dry chinook winds</p> -<p class="pcapc">Eastern slopes, under the influence of Continental air -masses, receive less annual precipitation. West Glacier’s -annual average is 66.5 cm. Babb, a small town east of the -park, averages 49.3 cm. Frequent high winds east of the -Divide further reduce moisture through evaporation.</p> -<p class="pcapc">Exposed to Arctic air masses flowing down from Canada, -locations east of the Divide also suffer more severe -winter conditions than do protected western valleys. -Average January temperature is -5°C at West Glacier, --8° at Babb.</p> -<p class="pcapc">Moreover, 80 percent of the winter days in the western -portion of the park are overcast, a condition almost -identical to that of Seattle, Wash. This serves to moderate -winter temperatures and to minimize evaporation.</p> -</div> -<div class="pb" id="Page_20">20</div> -<div class="img" id="fig10"> -<img src="images/p010.jpg" alt="" width="800" height="532" /> -<p class="pcap">Moss campion and mountain forget-me-not colonize a -fellfield. Fellfields are rocky alpine sites that are -slightly less than 50% bare rock, interspersed with -such plant pioneers as cushion plants, mosses, and -lichens.</p> -</div> -<div class="pb" id="Page_21">21</div> -<div class="img" id="fig11"> -<img src="images/p010a.jpg" alt="" width="700" height="721" /> -<p class="pcap">High lakes generally occupy cirque basins. These -depressions in the valley bedrock, quarried by glaciers, -are deepest near the headwall where ice thickness was -greatest. Cold and deep, and ice-free only weeks each -year, tarns cannot support vascular plants or vertebrates. -Iceberg Lake, shut off from the sun most of the -year by the encompassing 1,000-meter walls of Mt. -Wilbur and the Ptarmigan Wall, is never completely -free of ice.</p> -</div> -<div class="pb" id="Page_22">22</div> -<div class="img" id="fig12"> -<img src="images/p011.jpg" alt="" width="800" height="522" /> -<p class="pcap">Lake McDonald, 16 kilometers long, 2 kilometers wide, -and 134 meters deep, is the largest lake in the park. -Its basin is the classic U-shaped glacial valley. -Forested lateral moraines on either shore gently rise -600 meters above lake level. Going-to-the-Sun Road -snakes along the eastern shore, and Logan Pass lies -near the center of the photograph, behind the peaks -of the Lewis Range.</p> -</div> -<div class="pb" id="Page_23">23</div> -<div class="img" id="fig13"> -<img src="images/p011a.jpg" alt="" width="700" height="716" /> -<p class="pcap">Subjected to the drying and shaping effects of wind -both winter and summer, this Douglas-fir, growing in -the prairie community near St. Mary, will attain neither -the symmetrical shape nor the great size of the -Douglas-firs growing in moister, more sheltered sites -on the western slopes of the Continental Divide.</p> -</div> -<div class="pb" id="Page_24">24</div> -<div class="img" id="fig14"> -<img src="images/p012.jpg" alt="" width="800" height="512" /> -<p class="pcap">Freeze-and-thaw cycles continually fracture and loosen -rocks along joints, making them subject to removal by -the actions of water, gravity, and avalanche. The resulting -fans of rock debris (talus cones) indicate the -extent of erosion since the withdrawal of the -Pleistocene glaciers.</p> -</div> -<div class="pb" id="Page_25">25</div> -<div class="img" id="fig15"> -<img src="images/p012a.jpg" alt="" width="800" height="509" /> -<p class="pcap">Although moving water is an agent of erosion—the -primary destructive force of mountain masses—it also -permits life. Even small watercourses, such as this -freshet, abound with plant and invertebrate life.</p> -</div> -<div class="pb" id="Page_26">26</div> -<div class="img" id="fig16"> -<img src="images/p013.jpg" alt="" width="457" height="495" /> -<p class="pcap">Going-to-the-Sun Mountain, towering above the St. -Mary Valley, from the trail to Siyeh Pass. The coniferous -forest at its base and the alpine tundra plants at -its summit are closely juxtaposed in space; but if these -two communities grew at the same elevation they would -be separated by thousands of kilometers. Hiking from St. -Mary Lake up to Siyeh Pass is going, in effect, from -Montana to the Arctic Circle; but here the life zones -are compressed and sharply divided rather than -extended and overlapping.</p> -</div> -<div class="img" id="fig17"> -<img src="images/p013a.jpg" alt="" width="460" height="500" /> -<p class="pcap">Setting moon and snow shelf near the summit of -Heavens Peak. Note stratification of Precambrian -sediments.</p> -</div> -<div class="pb" id="Page_27">27</div> -<div class="img" id="fig18"> -<img src="images/p013b.jpg" alt="" width="700" height="720" /> -<p class="pcap">Western redcedars line the shores of Lake McDonald. -Because of prevailing air currents from the Pacific -coast, winters in the protected western valleys are -moist and comparatively mild, and this deep body of -water freezes over an average of only one winter in -four.</p> -</div> -<div class="pb" id="Page_28">28</div> -<div class="img" id="fig19"> -<img src="images/p014.jpg" alt="" width="453" height="800" /> -<p class="pcap">Moose often follow the spring snowmelt upwards to the -headwaters of drainages. This bull will remain at -Thunderbird Pond, at the base of Brown Pass, until -autumn, when it will return to its Waterton Valley -wintering ground.</p> -</div> -<div class="pb" id="Page_29">29</div> -<div class="img" id="fig20"> -<img src="images/p014a.jpg" alt="" width="800" height="529" /> -<p class="pcap">Because of the high reproductive capacity of insects -and small mammals, if all their offspring survived the -earth’s plant life would be consumed within one year. -This is prevented by natural controls such as predation -and parasitism. The American kestrel (“sparrow hawk”) -feeds primarily on large insects and on small rodents -such as the meadow vole here.</p> -</div> -<div class="pb" id="Page_30">30</div> -<div class="img" id="fig21"> -<img src="images/p015.jpg" alt="" width="461" height="801" /> -<p class="pcap">Gray jays are found in the deep coniferous forests of -the park. In some parks gray jays, or “camp robbers,” -loiter about campgrounds and picnic areas begging or -stealing food. In Glacier, however, they are seldom -noticed as they search out seeds, berries, and insects.</p> -</div> -<div class="pb" id="Page_31">31</div> -<div class="img" id="fig22"> -<img src="images/p015b.jpg" alt="" width="684" height="700" /> -<p class="pcap">A generalized predator, the coyote will eat almost anything, -from berries to carrion. When man eliminated -most of the coyote’s enemies and competitors, including -the wolf, grizzly, and cougar, it enlarged its range -to fill the void. Intelligent and social, the coyote thrives -despite man’s persecution. Although most numerous -in the prairie community, it ranges up to timberline.</p> -</div> -<div class="img" id="fig23"> -<img src="images/p015c.jpg" alt="" width="500" height="510" /> -<p class="pcap">The spruce grouse is a year-round resident of the -spruce/fir and lodgepole communities. It forages on the -ground for seeds and insects, in winter turning to -needles. Several other species of grouse occupy -different habitats in Glacier.</p> -</div> -<div class="img" id="fig24"> -<img src="images/p015d.jpg" alt="" width="500" height="520" /> -<p class="pcap">Chipmunks are found in every community, from prairie -to tundra, in Glacier. Each of the park’s three very -similar species has its preferred habitat. The diurnal -counterpart to nocturnally active mice, which have -the same diet of seeds, berries and occasional insects, -chipmunks adapt easily to the presence of people and -become nuisances if encouraged by handouts. Feeding -rodents is dangerous and is harmful to them. By altering -their diets and blunting their cautious instincts, -daily exposure to “free lunches” makes the animals -less fit to face the harsh realities of their natural -environment.</p> -</div> -<div class="pb" id="Page_32">32</div> -<div class="img" id="fig25"> -<img src="images/p016.jpg" alt="" width="449" height="801" /> -<p class="pcap">Unlike whitetail deer, which remain in lowland areas -all year, mule deer range upward into high meadows -during the summer. The bucks, especially, are wanderers -and travel together. Velvet antlers, worn during -the time of summer sociability, presage the autumn -contests to come.</p> -</div> -<div class="pb" id="Page_33">33</div> -<div class="img" id="fig26"> -<img src="images/p016a.jpg" alt="" width="483" height="500" /> -<p class="pcap">The checkerspot butterfly belongs to the most diverse -group of animals on the planet—the insects, whose -importance can hardly be overestimated. They not only -help recycle nutrients in the living community and -provide an abundant food base for other lifeforms, but -are instrumental in pollinating most of the earth’s -terrestrial plants.</p> -</div> -<div class="img" id="fig27"> -<img src="images/p016b.jpg" alt="" width="486" height="496" /> -<p class="pcap">Alpine vegetation must be able to survive freezing -temperature during the growing season, since winter -conditions are possible even in summer. Early bloomers, -such as the glacier lily, endure repeated snowfalls -during the unstable weather conditions of June.</p> -</div> -<div class="pb" id="Page_34">34</div> -<div class="img" id="fig28"> -<img src="images/p017.jpg" alt="" width="456" height="800" /> -<p class="pcap">Unlike mountain goats, these bighorn rams will desert -the alpine zone at the approach of winter; they will -join other bighorns congregating in the lower valleys.</p> -</div> -<div class="pb" id="Page_35">35</div> -<div class="img" id="fig29"> -<img src="images/p017a.jpg" alt="" width="800" height="539" /> -<p class="pcap">In November bighorn sheep rams end their summer-long -isolation from the ewes, move down from -the higher slopes, and begin a bloodless but taxing -ritual of strength and endurance to determine the -harem master. The sharp reports of clashing horns -may carry for kilometers, and the contests continue for -weeks until the dominant ram emerges. (Note the Many -Glacier hotel complex in the valley below.)</p> -</div> -<div class="pb" id="Page_36">36</div> -<div class="img" id="fig30"> -<img src="images/p018.jpg" alt="" width="500" height="507" /> -<p class="pcap">Hummingbirds, like shrews and other small-bodied, -warm-blooded animals, exist at the theoretical thresh-hold -of life. Because of their small size, body volume -is not large enough in relation to surface area to -prevent a rapid loss of body heat. To compensate for -this, metabolic rates must be high; food is rapidly -processed and used up. Thus, since fat reserves are -not practical on such small animals, they must eat at -frequent intervals.</p> -<p class="pcapc">Two species of hummingbirds—the rufous and the -calliope—are found in Glacier. Pictured is a female -rufous (which weighs about the same as a dime) -landing on its lichen decorated nest to feed its two -young on a protein-rich mixture of nectar and small -insects.</p> -</div> -<div class="img" id="fig31"> -<img src="images/p018a.jpg" alt="" width="497" height="524" /> -<p class="pcap">The insect-eating yellowthroat prefers moist habitats. -Unlike many of its treetop-dwelling relatives, this tiny -(10-11 cm.) warbler is usually seen near or on the -ground.</p> -</div> -<div class="pb" id="Page_37">37</div> -<div class="img" id="fig32"> -<img src="images/p018b.jpg" alt="" width="700" height="720" /> -<p class="pcap">Bands of bighorn ewes and lambs do not summer as -high as the rams and are often encountered in the -scrub-forest zone. Note the gnarled limber pine in the -foreground of this photograph taken on the south face -of Altyn Peak.</p> -</div> -<div class="pb" id="Page_38">38</div> -<p>Reaching the mountain wall, the goats -scramble upward to a ledge, sending scree -streams pouring from several clefts. Encountering -a narrow, steep snowbank, they -do not hesitate but continue across the -slope. Above the rock fingers of this peak -the gathering clouds grow black. A sudden -crack of thunder hurries me down the trail.</p> -<p>Although geologically young, the Rocky -Mountains in Glacier are composed of soft -sedimentary rocks that are easily assailed by -the many agents of weathering and erosion. -If not rejuvenated by continual uplift, these -magnificent peaks will glimmer but briefly -in the long memory of the planet.</p> -<p>Already the sharp countenance of this -land is being softened by the ongoing forces -of erosion. Chief among these is water, -which attacks the mountains everywhere. -In addition, frost action continually exploits -rock fractures, breaking down blocks of rock -into talus and scree. Avalanche and rockfall -sweep down the slopes. Layers of softer rock -erode quickly, undercutting more resistant -rock and creating overhangs which gravity, -in time, will collapse.</p> -<p>The lashing rain catches me on this -sun-and-storm-contested pass. Ice, gravity, -wind, and especially water—all attack a land -that dares the clouds.</p> -<div class="pb" id="Page_39">39</div> -<h3 id="c4">The Rising of the Sun and the Running of the Deer: A Glacier Year</h3> -<p>As if to make up for the days-long darkness -of this last blizzard, the peaks today wear -snow plumes—long, graceful trails of white, -curving up into an ice-blue sky. Yesterday -the snow-mad wind raced through the forest. -Today the motionless trees are cloaked in -heavy, glistening robes, the leafless aspen -and young larch bent down.</p> -<p>Moderate snowfall helps many plants -and animals survive the winter. For ground -dwellers it provides insulation from the -wildly fluctuating winter temperatures encountered -east of the Divide, protecting the -hibernators and providing cover for the -many small mammals that remain active -during the winter. Wind-swept ground -freezes deep; but under a mantle of snow -life-sustaining heat is trapped, permitting -many animals to survive and allowing the -work of decomposers to continue.</p> -<p>But this has been a winter of too much -snow and too many temperature extremes. -The heavy snowpack has forced the sharp-hoofed -deer to yard up in great numbers; -unable to range freely in deep snow, they -are forced into smaller and smaller confines -where their numbers allow them to break -and maintain trails. But in time they exhaust -the food supply. Younger deer, unable -to reach the increasingly higher browse line, -starve first. Then the does, heavy with unborn -fawns, grow weak and fall to predators. -So the imprisoned herds dwindle quickly -this year, sometimes less than a kilometer -from plentiful browse.</p> -<p>Deep snow is also death for many seed-eating -birds. As they are unable to scratch -for food, their body furnaces quickly fail, -and during a night of cold wind their fluffed -corpses drop into the snow.</p> -<p>Exposed to the noon sun, the snow surface -thaws; when refrozen, it is restructured -to crystalline ice. If snow repeatedly thaws -and freezes, an ice barrier is formed, shutting -off vital air exchange. Plants are then -subject to rot, and micro-animal life is -smothered. Travel beneath the snow is made -more difficult for mice and shrews and they -are deprived of food and cover. Under such -conditions their numbers rapidly decline.</p> -<p>But while many starve in a winter of -deep snow, others benefit. The exposed -traffic of small mammals is to the owl’s -advantage. Foxes and coyotes more easily -run down rabbits and hares on crusted snow. -Deer and, to a lesser extent, wapiti and -moose—their hoofs punching through the -snowpack—swiftly tire in deep snow and -become helpless before cougar or wolf, -whose lighter weight is supported by the -crust.</p> -<p>Grim as this winter’s toll becomes, -enough will survive to begin the process of -renewal in spring. Last winter, a season of -light snow, was a time of hardship for predators. -The deer remained strong, the wapiti -remote on high, windswept ridges, and the -<span class="pb" id="Page_40">40</span> -small mammals hidden.</p> -<p>Only the water ouzel, winter after winter, -seems not to notice the hardships of the -season. Lord of his small world of open -water, he sings in February, wading and -swimming his diminished stream to find a -never-failing supply of water insects and -small fish. It is a voice of spring—glad, wild, -continual as the moving water—an incongruous -song in this winter-shrouded land.</p> -<p>But with the growing stature of the -sun, the grip of winter softens. The firs and -spruce send their loads of snow sliding to -the ground. Streams begin to sing again and -soon the lakes increase, the booming of -splitting ice breaking the silence of the valleys. -Avalanches thunder down the steeper -slopes, carrying trees to the swollen streams. -Rivers hiss and rage, speeding the debris -along. A spring that comes too suddenly will -bring flood to lower elevations.</p> -<p>Snow geese thread through the valleys, -and ground squirrels tunnel up through snow -to find invasions of birds returning from the -south. Soon the three-petaled wakerobins -appear, chasing the snowline up the ridges. -Glacier lilies and Calypso orchids are next, -and with the shooting stars spring arrives.</p> -<p>The melting snow releases a new group -of animals to populate the winter-thinned -land. Up come chipmunks. Bears reappear. -Young red squirrels, helpless and blind, -squirm in their nest holes. Hidden dens -rustle with pups and kits. Soon warm days -will bring them out and the business of -learning to cope with their world will begin.</p> -<p>All life responds irresistibly to the -growing strength of the Sun. Cottonwood, -willow, and maple come into flower and -unfold new leaves; green needle clusters -spot the limbs of larches that in winter -had seemed lifeless snags among the other -conifers. Beneath the soil of prairie, -meadow, and forest, in the mud of lakes and -ponds, other life stirs; armies of insects, -spiders, crustaceans, amphibians, and fish -will strive to complete their life cycles -against the formidable odds of a predatory -world.</p> -<p>Spring reaches higher up the mountains, -the lowlands passing into summer. Wapiti -and mountain sheep follow the rising tide -of succulent browse up to the high meadows. -In forest, grove, and meadow and along the -stream new fledglings appear—thrush, vireo, -hummingbird, waxwing, harlequin duck, -bluebird, osprey, and flicker—as holes, nests, -and cavities brim with begging mouths.</p> -<p>In the alpine meadows, where snow -overlaps the spring and winter follows hard -behind the summer, the growing season is -short and the climate unstable. Sensing the -stronger light, flowers push up impatiently -through the snow and hasten into bloom. -Pikas and marmots scurry and sunbathe -among the rocks of scree slopes.</p> -<p>Summer matures in ripening huckleberries, -and the bears that grazed the spring -grasses now gorge themselves fat. Dry days -of August bring probing lightning, threatening -<span class="pb" id="Page_41">41</span> -the forests with fire.</p> -<p>Sweeps of beargrass reach their climax -now in the highest meadows. In dizzy succession -wildflowers set seed. Fat and sluggish, -marmots and ground squirrels disappear beneath -the rocks. The golden eagle must -search longer each day to find prey within -its vast domain.</p> -<p>Autumn lingers in the valleys and on -the flanks of low ridges. The morning sun -glints on hoarfrost, firing the yellow leaves -of larch, aspen, birch, maple, and cottonwood, -and shines on the blood-red berries -of mountain-ash. Soon a night of killing -frost will bring down the corpses of insects -and spiders by the millions. The reptiles and -amphibians, being cold-blooded animals, -seem out of place in this long-wintered land. -Unable to maintain body temperatures appreciably -above their surroundings, they are -the first to seek the protection of hibernation, -collecting in dens or burying themselves -beneath the ooze of pond bottoms.</p> -<p>Songbirds gather and leave the valleys. -The harsh cries of jays sound ominous now -in the forest. Only the chickadees seem to -ignore the long tree shadows; their ceaseless -conversations carry through the leafless -underbrush as they busily search for seed.</p> -<p>Velvet has gone to bone, and in these -final noon-warm days the rut runs through -the land. It begins in the valleys in September -with the joustings of deer and moose -and the buglings of bull wapiti puncturing -the forest silence. By November the higher -meadows ring with the collisions of bighorn -rams who compete for ewes by smashing -together their massive, curled horns. On -high slopes mountain goat billies posture and -swagger; head to tail, they circle, threatening -each other with dagger-like horns.</p> -<p>From Flathead Lake, 100 stream kilometers -to the south, kokanee salmon return to -spawn in the clear, cold shallows of McDonald -Creek. Gathering bald eagles surround -the stream, again and again lifting -vulnerable fish from pool and riffle. Perched -by the hundreds along the stream course, -their white heads and tails glistening against -the dark trees, they stand out like lanterns -strung for a banquet.</p> -<p>Now the stinging wind comes down -from the peaks and shuts the lakes. Life -slows or sleeps. Ptarmigan, snowshoe hare, -and longtail weasel, all wearing winter white, -seek shelter and food in a silent land where -spring and yellow lilies seem forever lost.</p> -<p class="tb">■<br />All life faces one ultimate challenge: to survive -or not, to reproduce or fail, to bring -one’s kind to tomorrow’s sun or vanish forever. -This land is harsh. To survive in nature -demands skill in the individual, excellence -in the species, and a chance from the -environment.</p> -<div class="pb" id="Page_42">42</div> -<div class="img" id="fig33"> -<img src="images/p019.jpg" alt="" width="700" height="752" /> -<p class="pcap">The mink, a solitary predator associated with low-elevation -watercourses, preys on anything it can catch -and subdue.</p> -</div> -<div class="pb" id="Page_43">43</div> -<h2 id="c5"><span class="small">Plant-and-Animal Communities</span></h2> -<div class="pb" id="Page_44">44</div> -<h3 id="c6">Over Going-to-the-Sun Road</h3> -<p>I like to begin with St. Mary, a lake the -whitecaps love to run. From the far passes -the several winds gather and collect, arranging -long lines of white waves for the race -downlake. Past the purple scree of Mahtotopa -and Little Chief they go, white as the -headdress of Going-to-the-Sun Mountain, -colliding, collapsing along the promontory -snares about the Narrows. Onward they -press, spreading out and setting sail for the -straight rush to the final shore where a line -of cottonwoods sings with a sound like -applause.</p> -<p>Across the lake the timbered ridge -starkly contrasts the finger of prairie that -claims the north shore. This is a flower-glad -place, a meeting-ground for mountain and -prairie plants. Along the road the grassland -holds the conifers back, allowing only -scattered clumps of aspens.</p> -<p>Finally, at Rising Sun, beneath the -shadow of Goat Mountain, the prairie ends -and wind-seasoned Douglas-firs announce -the coming forest.</p> -<p>There’s excitement now, with the prairie -heat gone, the wind scent raw with fir and -high meadows, honed by waterfall and tall, -dank rock. Our mountain thirst is never -extinguished, and a road that tightens down -to cliff face and sudden turn brings back -to our blood the ancient need to go to the -highest place.</p> -<p>There is sword-edged Citadel, and the -snow-flanked spike of Fusillade holding -court like a queen in this valley of peaks; -then the dome of Jackson and the Gunsight -notch. Our eyes are kept high, transfixed at -last by looming Heavy Runner and the distant -promise of Reynolds.</p> -<p>Looking for mountain goats, we scan -the walls around the sweep of Siyeh Bend, -catching a glimpse of the trail that crosses -the scree to hidden Piegan Pass.</p> -<p>Beargrass heads lean out above the road -like old men conferring on the view. The -purple trumpets of penstemon crowd the -rocks, and spots of Indian paintbrush lead -like a blood-trail to the higher slopes.</p> -<p>Intoxicated now, feeling the fresh full -force of the wind from Logan Pass, we race -on. We hardly notice the struggle of the -forest in Reynolds Creek far below, how it -thins and loses strength in its own hard -climb. We sweep past it on the broad magnificence -of this pass.</p> -<p>Level but a moment, the road dips to a -shelf on the headwall above Logan Creek -and swings over the great sculptured cliff of -the Garden Wall. For several kilometers this -masterpiece of a road glides down a constant -grade, squeezed between rock face -and space, twisting into tight drainages—a -road for storm lovers, wet with spray and -snow-seep, its quick turns concealing sudden -winds.</p> -<p>Mighty, snow-robed Heaven’s Peak appears, -taking our attention from the Pass-group -mountains and the hanging valley -<span class="pb" id="Page_45">45</span> -that spills Birdwoman Falls. Northward is -the great array of peaks encircling distant -Flattop, jumbles of mountains and glaciers. -How are we to notice the forest far below?</p> -<p>Not until we have passed the Loop and -are moving past the blackened snags of a recent -burn do we realize the stature of this -forest. The long road down will take us -into a valley much deeper than any on the -eastern side. Near Avalanche Creek are -trees we have seen nowhere else in the -park—giant western redcedars, western -hemlocks with their nodding tops, monstrous -black cottonwoods with bark so -deeply furrowed that it looks hewn by -hatchet.</p> -<p>We take a long ride down the valley, -past the low pyramid of Mt. Stanton, final -peak in the Livingston Range. Near the outlet -end of Lake McDonald, birch and aspen -again appear in numbers, and the road -enters a crowded stand of lodgepole pine.</p> -<p>Our memories cluttered with mountains, -waterfalls, and snowfields, we do not -quite realize the significance of this 80-kilometer -journey. We have crossed the boundaries -of several different plant-and-animal -communities, spanning a range of climate -that would be encountered on a 5,000-kilometer -north-south journey at sea level.</p> -<p>At first glance the various trees, wildflowers, -and animals seem randomly distributed, -scattered about like the distant -mountains. But mountainous terrain represents -an organized high-rise approach to -life. From the lowest, most protected valley -to the highest wind-and-ice-cut summit, the -life-forms align themselves, each according -to its own climatic tolerance.</p> -<p>Here too can be seen the great cycles -of nature: fire and regrowth, the building of -soil and its erosion, the incessant duel of the -eaters and the eaten.</p> -<p>In the following sections we will spend -some time in these various communities, -from prairie to tundra.</p> -<div class="pb" id="Page_46">46</div> -<h3 id="c7">Groves and Grasslands: The Prairie Sea</h3> -<p>There is something about spring on the -prairie that gets me up before dawn. I like -to watch the seasons change their guard -over the landscape, from the wintry cold of -pre-dawn dark to the spring-scented morning -air to the hot summer-foretaste of the -noon May sun.</p> -<p>Hoarfrost surrounds these patches of -pasqueflowers, blue goblets on downy -stems. On this windless night, frost has -formed everywhere, reclaiming for a time -its vast winter range, sparkling over the -green handiworks of spring.</p> -<p>But the god of the growing grasslands -is the sun, and it now proclaims itself, -stretching out to make the mountains shine. -With its assault the frost collapses, becoming -bright beads on grass tip and leaf joint -by which a beetle might refresh itself.</p> -<p>Spring is best perceived ant-level, at its -ground beginnings, where the bright yellow-green -tips of new grass shoots reclaim the -winter-blighted land. I look closely at a drag -line of spider silk; a necklace of dewdrops -slides down, collects to a moment’s greatness, -in which I briefly see a curved horizon, -the morning sunburst, and myself, before it -falls away.</p> -<p>Getting up from my prone position, my -belly damp from the prairie earth, I startle -a whitetail jackrabbit; bounding high, it zigzags -off. The commotion disturbs a distant -badger, which faces about from its diggings -to confront danger in whatever form it might -take. It swings its snout to scent the air. -Somewhat uncertainly, it returns to the business -of hunting, then hesitates, swings about -once more and waits, myopic, patient.</p> -<p>Satisfied at last, the spurt of the now -distant rabbit lost in its brain, the creature -snorts a defiance at the mystery and resumes -its morning gopher hunt.</p> -<p>Overhead a marsh hawk skims past, its -flight erratic as a butterfly’s. Far away a -magpie rattles at the passing hawk and -takes flight, briefly flashing black and white.</p> -<p class="tb">■<br />It is easy to see only pieces in the natural -puzzle—a badger throwing dirt, horned -larks dipping into wind, black ants dragging -the rosette of a dead spider—and be satisfied -with the scattered scenes. But at last, to -make it meaningful, we must complete the -picture. There is that special joy in discovering -larger schemes: green plants utilizing -sunlight; a rabbit building its days at the -plants’ expense; the falcon tearing the rabbit -meat for its young; magpies picking at -the fallen falcon; and then, in the end, all -returning to the earth.</p> -<p>Here on the prairie, as in every plant-and-animal -association, the ancient drama -repeats itself over and over; the distant tundra -is a drastically different stage with different -actors, but the cycle is the same. Life -depends upon the interaction of all its -<span class="pb" id="Page_47">47</span> -many forms. Unseen bacteria are as necessary -to the land as green grass; the meadow -vole and the coyote are as much a part of -the prairie as the grasses.</p> -<p>The secret of life rests in the wonder of -photosynthesis. Only green plants can manufacture -food from the earth’s raw minerals. -This is the vital first step upon which the -great pyramid of animal and plant life is -built. Using energy from the sun, green -plants combine water and carbon dioxide to -synthesize sugar, and give off oxygen as a -by-product. The caterpillar takes its energy -from the plant tissue, converting to protein -the sugar and minerals in its body. The -caterpillar is then food for a spider or other -predator. A yellow warbler may take the -spider and in turn be ambushed by the -prairie falcon. Thus the energy produced by -the plant travels through the food chain. -When the prairie falcon dies, scavengers—including -insects and other invertebrates, -birds, and mammals—redistribute its wealth -among themselves; the rest is decomposed -by bacteria. Thus, eventually, the nutrients -on which the plants depend return to the soil.</p> -<p>When we look at any living organism, -whether it is plant, herbivore, carnivore, -parasite, scavenger, or decomposer, we are -soon made aware of its associations with -other living things, each puzzle piece leading -us to another and another. We begin to see -a picture whole—the fox, meadow mouse, -grasshopper, bunchgrass, and sparrow hawk—all -interlocked.</p> -<p>Geologically speaking, grasslands are a -recent development. As the Rocky Mountains -were being uplifted, the prevailing -warm, moist climate began to change. The -rising mountain mass intercepted moisture-laden -winds that blew in from the Pacific, -creating a rain shadow that lengthened eastward -as the mountains rose higher. A continental -climate, characterized by severe -winters and dry, wildfire summers gradually -took shape, extinguishing the great forests -that had grown across the continent’s interior. -Herbaceous plants, which had been evolving -amid the forests, inherited the land.</p> -<p>Unlike trees, grasses die back to the -ground each winter, hoarding their life-germ -beneath the protecting soil. Growing -not from the tip but from the joints, grasses -regenerate quickly after fire or grazing. -Suspension of the normal metabolic processes -enable the grasses to go dormant and thus -survive periods of severe heat and drought.</p> -<p>Although the great prairie sea washes up -against Glacier’s eastern boundary, with -estuaries probing into the mountain valleys -on the drier, south-facing slopes, the grassland -community comprises less than 5 percent of -the land area of Glacier National Park. -This includes the puddles of prairie west of -the Divide that interrupt the dense coniferous -forests along the North Fork of the -Flathead River.</p> -<p>From the pasqueflowers that bloom in -early May to the asters and goldenrod of -September, these summer-long gardens of -grasses and flowers lean with the wind. Here -are timothy, oatgrass and the bunchgrasses—rough -fescue, bluebunch fescue, and bluebunch -wheatgrass. Among the grasses bloom -bitterroot, blue camas, lupine, gaillardia, -balsamroot, cinquefoil, sticky geranium, and -wild rose.</p> -<p><span class="lr"><i><span class="small">continued on <a href="#Page_68">p. 68</a></span></i></span></p> -<div class="pb" id="Page_48">48</div> -<div class="img" id="fig34"> -<img src="images/p020.jpg" alt="" width="1000" height="617" /> -<p class="pcap"><b id="f2fig2">The Forests of Glacier</b></p> -<p class="pcapc">From the lush redcedar-hemlock forest in -the McDonald Valley to the subalpine fir, -whitebark pine, and Engelmann spruce -struggling for existence near treeline, the -forests of Glacier reflect the conditions -of temperature, exposure, soil, and -drainage prevailing; and each forest has -its characteristic association of understory -trees and shrubs, herbaceous -ground cover, and vertebrate and -invertebrate animal life.</p> -</div> -<div class="pb" id="Page_50">50</div> -<div class="img" id="fig35"> -<img src="images/p021.jpg" alt="" width="1000" height="443" /> -<p class="pcap"><b>Life Zones</b></p> -<p class="pcapc">Many physical and climatic factors -determine the range of Glacier’s plant-and-animal -communities. Boundaries -between communities are seldom sharply -defined, but rather merge together in -broad zones of transition.</p> -<p class="pcapc">With elevation gain, average daily temperature drops -at the rate of 5° per 900 meters. Precipitation, wind -velocity, and evaporation loss increase. Soil thins. -These factors, along with others such as fire frequency, -north or south exposure, and availability of moisture, -combine to determine the range of each community.</p> -<p class="pcapc">In the forest community below 1,800 meters, Douglas-fir, -lodgepole pine, and western larch predominate. In the -valleys, Engelmann spruce and subalpine fir are found. -The somewhat lower and much better watered western -valleys of the park support western redcedar and -western hemlock.</p> -<p class="pcapc">Treeline is the upper limit to which the tolerances of -trees to environmental conditions permit them to grow. -Because there are so many controlling factors (wind, -temperature, exposure to sunlight, snow cover, etc.) -treeline in the diagram is only approximate. In Glacier -it averages 2,000 meters. Avalanche chutes or sheer -cliff walls may suppress it to below 1,500 meters; on -protected slopes it may be as high as 2,150 meters.</p> -<p class="pcapc">At the eastern edge of the park below 1,200 meters, the -forest gives way to the prairie community, composed -mostly of soft-stemmed plants adapted to the conditions -of low precipitation that prevail here in the rainshadow -of the mountain range. Clumps of aspen, found in the -prairie in sheltered spots, occur here in the transition -zone between prairie and forest.</p> -</div> -<div class="pb" id="Page_52">52</div> -<div class="img" id="fig36"> -<img src="images/p022.jpg" alt="" width="1000" height="650" /> -<p class="pcap"><b>A Mountain Profile</b></p> -<p class="pcapc">This diagram represents the eastward-facing -slope of a hypothetical mountain -near the eastern boundary of Glacier -National Park. Its life communities are -somewhat different from those of -mountain slopes at the western edge, -chiefly because of the differential in -annual precipitation.</p> -<p class="pcapc">Illustration: Here, above approximately 2,750 meters, in a realm of -ice, snow, and barren rock, there is little life.</p> -<p class="pcapc"><span class="large"><b>Alpine tundra</b></span></p> -<p class="pcapc">Below 2,750 meters and above 2,000 meters, depending -on other factors such as exposure to sun and wind and -steepness of terrain, exists the alpine tundra community, -with vegetation similar to that of the vast, -essentially level, treeless zones of the Arctic.</p> -<p class="pcapc"><span class="large"><b>Scrub-forest</b></span></p> -<p class="pcapc">Roughly between 1,800 and 2,000 meters, the dominant -vegetation is scrub-forest. Trees here are stunted; -except in sheltered spots they are more or less prone -rather than upright. Net growth is slow, not only because -of the short growing season but also because -of the pruning effect of icy mountain winds. Very -few tree species can survive in this harsh habitat.</p> -<p class="pcapc"><span class="large"><b>Coniferous forest</b></span></p> -<p class="pcapc">In the forest community below 1,800 meters, Douglas -fir, lodgepole pine, and western larch predominate. In -the valleys, Engelmann spruce and subalpine fir are -found. The somewhat lower and much better watered -western valleys of the park support western redcedar -and western hemlock. See <a href="#Page_54">page 54</a></p> -<p class="pcapc"><span class="large"><b>Prairie</b></span></p> -<p class="pcapc">At the eastern edge of the park below 1,200 meters, -the forest gives way to the prairie community, composed -mostly of soft-stemmed plants adapted to the -conditions of low precipitation that prevail here in the -rainshadow of the mountain range. Clumps of aspen, -found in the prairie in sheltered spots, occur here -in the transition zone between prairie and forest.</p> -</div> -<div class="pb" id="Page_54">54</div> -<div class="img" id="fig37"> -<img src="images/p023.jpg" alt="" width="1000" height="711" /> -<p class="pcap"><b>The Forest Community</b></p> -<p class="pcapc">A forest is organized vertically like an -apartment house or office building, with -layers corresponding to stories. The -<i>canopy</i> is the branches and foliage of -tall trees that form a roof over the -community. Below the canopy are the -<i>understory</i> trees: young individuals of -the canopy species; and small, shade-tolerant -trees that will never become part -of the canopy. Beneath the understory -branches is the <i>shrub layer</i>, occupied by -knee-high-to-man-high woody plants; -beneath that is the <i>herb layer</i>, where most -of the ferns, wildflowers, grasses, and -smaller woody plants grow. The <i>forest -floor</i> is the zone of mosses, mushrooms, -creeping plants, and forest litter (leaves, -twigs, needles, feathers, bits of bark, -animal droppings, etc.). The forest has a -“basement,” too, interlaced by plant -roots, mycelia of fungi, and tunnels of -myriad animals.</p> -<p class="pcapc">Each layer of the forest has its characteristic -animal species, but most forage -over more than one level. Some nest in -one story and feed in another. The red -squirrel races back and forth from the -forest floor to the highest branches.</p> -<p class="pcapc">The forest community also has a socio-economic -organization. Every animal (and -plant) takes up space and consumes -a portion of the available nutrients. -Each has a place in the community -food chain—as, for example, <i>herbivore</i>, -<i>carnivore</i>, or <i>scavenger</i>. Each directly or -indirectly affects all the other organisms.</p> -<p class="pcapc"><b>The Forest Community</b></p> -<p class="pcapc">The role of a species in the community, like the job and social -function of a person, is its <i>niche</i>. Similar species of animals have different niches, -thus lessening competition for food and living space. Thrushes hunt close to the -ground; vireos and kinglets hunt among the branches; flycatchers snap up -airborne insects. The flicker feeds upon insects, excavates nesting holes that are -later occupied by other species such as squirrels and owls, and is preyed upon -by the great horned owl; its niche is <i>insect exterminator / food for carnivores / homebuilder</i>. -The great horned owl, hunting mammals, birds, and reptiles by night, -preys on species different from those hunted by the goshawk, and thus -occupies a parallel niche. When it dies, its remains, like those of other animals, -are decomposed and return to the soil.</p> -</div> -<dl class="undent pcap"><dt>Canopy</dt> -<dd>Great Horned Owl</dd> -<dd>Yellow-bellied Sapsucker</dd> -<dt>Understory</dt> -<dd>Flying Squirrel</dd> -<dt>Shrub Layer</dt> -<dd>Ruffed Grouse</dd> -<dt>Herb Layer</dt> -<dd>Red Squirrel</dd> -<dd>Western Toad</dd> -<dt>Forest Floor</dt> -<dd>Shorttail Weasel</dd> -<dd>Scavenging Insects</dd> -<dd>Deer Mouse</dd> -<dd>Garter Snake</dd> -<dt>Soil Layer</dt> -<dd>Ground Squirrel</dd> -<dd>Earthworm</dd> -<dd>Masked Shrew</dd></dl> -<div class="pb" id="Page_56">56</div> -<div class="img" id="fig38"> -<img src="images/p024.jpg" alt="" width="1000" height="673" /> -<p class="pcap"><b>Sun, Green Plants, and Animals</b></p> -<p class="pcapc">The sun is the source of energy for any -plant-and-animal community. Green -plants draw nitrogen and minerals from -the soil, and in a process called photosynthesis -use sunlight to convert raw -materials (carbon dioxide and water) into -carbohydrates (sugar, starch, cellulose), -giving off oxygen as a by-product. -Besides burning oxygen, animals depend -on plants for food.</p> -<p class="pcapc"><b>Green Plants</b>, trees and shrubs, grasses -and sedges, wildflowers, ferns, mosses, -algae and lichens—are fed upon by -animals, which are unable to manufacture -their own food.</p> -<p class="pcapc"><b>The Redback Vole</b>, like other rodents, -pikas and hares, seed-eating birds, -grazing and browsing hoofed animals, -and herbivorous insects, derives its -energy from the seeds and other parts -of green plants that it eats.</p> -<p class="pcapc"><b>The Garter Snake</b>, feeding upon the vole, -is dependent upon plants even though it -does not eat them.</p> -<p class="pcapc"><b>The Great Horned Owl</b>, preying upon the -garter snake, is one more step removed -from the green plants—but still -dependent on them.</p> -<p class="pcapc"><b>Scavengers</b> such as carrion beetles feed -upon the carcass of the owl; the remains -are then attacked by <b>Decomposers</b>, -primarily bacteria, that break down the -animal tissues into basic organic -compounds.</p> -<p class="pcapc"><b>The Soil</b>, enriched by the minerals and -carbon and nitrogen compounds added to -it by the decomposers (and by other -processes such as fire) supports new -green plant growth.</p> -<p class="pcapc">Thus energy derived from the sun flows -through the ecosystem in a food chain. -A plant-and-animal community is a -complex, interlocking web of such food -chains.</p> -</div> -<dl class="undent pcap"><dt>Sun</dt> -<dd>Green Plants</dd> -<dd>Redback Vole</dd> -<dd>Garter Snake</dd> -<dd>Great Horned Owl</dd> -<dd>Scavengers, Decomposers</dd> -<dd>Soil</dd></dl> -<div class="pb" id="Page_58">58</div> -<div class="img" id="fig39"> -<img src="images/p025.jpg" alt="" width="1000" height="655" /> -<p class="pcap"><b>A Pyramid of Numbers</b></p> -<p class="pcapc">Necessarily, the number of plants in an -ecosystem far exceeds the number of -plant eaters, and the number of prey -species must exceed the number of predators. -During its lifetime, a golden eagle -will consume a vast number of lesser -animals. The combined mass of prey -animals necessary to sustain an eagle -greatly outweighs the eagle itself. Ecologists -refer to this proportional relationship -of mass between each link in the -food chain as the <i>pyramid of numbers</i>.</p> -<p class="pcapc">The diagram represents a numbers -pyramid for the alpine zone. Because of -its limiting environment, the alpine zone -supports a lesser plant mass than the -forest zone. As a result, the carrying -capacity of the alpine is less than that -of the forest.</p> -<p class="pcapc"><span class="large"><b>1 Kilo</b></span></p> -<p class="pcapc"><i>Tertiary</i> (third-order) <i>consumers</i> are the predators -(Golden Eagle, Swainson’s Hawk, etc.) that feed upon -other predators. Because of the 90% loss of energy at -each level of the food chain, there will be very few -hawks and eagles in comparison to the numbers of -marmots.</p> -<p class="pcapc"><span class="large"><b>10 Kilos</b></span></p> -<p class="pcapc"><i>Secondary consumers</i> are the predators (weasels, -shrews, carnivorous insects and birds, etc.) that eat -herbivores. The animals at this level of the pyramid are -often—though not always—larger than the animals they -feed upon. But they are much less numerous, because -it takes many prey animals to sustain one predator.</p> -<p class="pcapc"><span class="large"><b>100 Kilos</b></span></p> -<p class="pcapc"><i>Primary consumers</i> (plant eaters, or herbivores) convert -plant tissue into animal flesh. In the process about -90% of the energy stored as plant food is lost, mostly -as heat energy. In the alpine community the herbivores -include pikas, marmots, ground squirrels, and ptarmigan, -as well as herbivorous insects.</p> -<p class="pcapc"><span class="large"><b>1,000 Kilos</b></span></p> -<p class="pcapc"><i>Producers</i> are the green plants at the base of the food -pyramid, manufacturing food for the animals of the -alpine community. The <i>biomass</i> (total weight) of each -level of the food chain is ten times (more or less) the -weight of the stage above it: 1,000 kilos of green plants -will produce only 100 kilos of primary consumers.</p> -</div> -<div class="pb" id="Page_60">60</div> -<div class="img" id="fig40"> -<img src="images/p026.jpg" alt="" width="800" height="578" /> -<p class="pcap">Great horned owls are the nocturnal equivalent of -Cooper’s hawks and goshawks in the low-elevation -forests of the park. Large and powerful, they are -capable of taking prey as big as skunks. This young -bird, disturbed on its day roost, clacked its bill and -fluffed its feathers in a menacing manner.</p> -</div> -<div class="pb" id="Page_61">61</div> -<div class="img" id="fig41"> -<img src="images/p026a.jpg" alt="" width="700" height="720" /> -<p class="pcap">The only sizable mature stand of ponderosa pine found -within the park is along the North Fork truck trail. -A scattering of old ponderosas growing at the lower -end of Lake McDonald suggests that at one time -ponderosa forests were more extensive in this region -than at present.</p> -</div> -<div class="pb" id="Page_62">62</div> -<div class="img" id="fig42"> -<img src="images/p027.jpg" alt="" width="800" height="688" /> -<p class="pcap">A black bear near treelimit. Bears will eat almost anything, -from ants to carrion, grass to garbage. Color -phases include brown and blonde bears. Unlike the -larger, more aggressive grizzly, which ranges out onto -the plains, black bears are strictly forest creatures.</p> -</div> -<div class="pb" id="Page_63">63</div> -<div class="img" id="fig43"> -<img src="images/p027a.jpg" alt="" width="487" height="500" /> -<p class="pcap">The water ouzel, or dipper, a creature of fast mountain -water, is admirably outfitted to cope with its -demanding environment. Stubby wings, chunky body, -short tail, and oily plumage allow it to walk under -water, where it scavenges for aquatic insect larvae and -small fish. In flying up- and down-stream, ouzels never -shortcut but follow the winding streamcourse.</p> -<p class="pcapc">As long as there is open water, the dipper suffers no -hardship from the mountain winter. Then, when the land -is shut down and lakes are frozen over, this little bird -carries on in its mountain-stream habitat, plunging into -the cold water to find food, and pausing occasionally to -sing.</p> -</div> -<div class="img" id="fig44"> -<img src="images/p027b.jpg" alt="" width="488" height="500" /> -<p class="pcap">Ouzels construct their nests of living moss on cliff -faces or ledges where constant spray keeps the moss -moist. At fledging, the four young of this nest in -Avalanche Gorge tumbled one by one into the torrent -below, to be collected by the adults in quieter water -downstream. Within a day they appeared to have -mastered the underwater gymnastics and were feeding -on their own.</p> -</div> -<div class="pb" id="Page_64">64</div> -<div class="img" id="fig45"> -<img src="images/p028.jpg" alt="" width="800" height="389" /> -<p class="pcap">From their lowland wintering grounds, wapiti move up -to higher elevations in spring. Summer range in the -park is abundant, but winter range is limited; as a -result, wapiti have a tendency to increase their populations -beyond the carrying capacity of available winter -range. In a severe winter many starve. But in a -balanced ecosystem such loss is not waste, for the -carrion helps sustain scavengers; it is an important -initial food source for bears emerging from hibernation.</p> -</div> -<div class="pb" id="Page_65">65</div> -<div class="img" id="fig46"> -<img src="images/p028a.jpg" alt="" width="500" height="518" /> -<p class="pcap">Cedar waxwings nest in moist areas of low valleys -where fruits and berries are abundant. Although they -also subsist on insects (which they can capture on -the wing), their weakness for fruit is so pronounced -that the birds will sometimes gorge themselves until -rendered incapable of flight.</p> -</div> -<div class="img" id="fig47"> -<img src="images/p028b.jpg" alt="" width="376" height="801" /> -<p class="pcap">The Columbian ground squirrel is found at all park -elevations, from prairie to alpine meadow. Hibernation -occupies almost three-quarters of its five-year lifespan. -Unlike other park ground squirrels, it lives in colonies. -Although not as tightly structured as a prairie dog -town, the association is beneficial to all members in -that danger is readily detected.</p> -</div> -<div class="pb" id="Page_66">66</div> -<div class="img" id="fig48"> -<img src="images/p029.jpg" alt="" width="700" height="705" /> -<p class="pcap">The tundra community is encountered above Preston -Park on the Siyeh Pass trail. Mt. Reynolds, a -classic example of a horn, dominates the distant -Logan Pass area.</p> -</div> -<div class="pb" id="Page_67">67</div> -<div class="img" id="fig49"> -<img src="images/p029a.jpg" alt="" width="800" height="508" /> -<p class="pcap">Camas blooms in the prairie community along the Red -Eagle road. An important staple, camas bulbs were -gathered as food by Indians.</p> -</div> -<div class="pb" id="Page_68">68</div> -<p>Conspicuous also are many insects—including -grasshoppers; flies; ants, wasps and -bees; butterflies and moths; bugs; and beetles—which -fulfill important roles as herbivores, -carnivores, and scavengers while also acting -as pollinators for flowering plants and providing -an abundant food source for other -animals.</p> -<p>Below the ground are the tunnels. Burrowing -is an important means of survival on -the open prairie, and life underground is -extensive. Some of the animals are rarely -seen—the northern pocket gopher, for example, -with a diet of underground insects, -grubs, worms, and roots, spends most of its -life tunneling just below the surface. Others, -like the badger, leave their burrows during -the day to dig for rodents. Most conspicuous -of the burrowing animals in the park’s -grasslands is the Columbian ground squirrel. -Its alert upright stance has earned it the -nickname “picket pin.” When danger approaches -from the air or on land, its shrill -alarm whistle passes the warning to others -of its kind.</p> -<p>Where prairie and forest meet, a never-ending -struggle for dominion is waged. The -isolated patches of prairie that dot the -North Fork Valley near Polebridge hold the -great forest of the park’s northwest region -at bay.</p> -<p>This broad valley, floored with coarse -glacial outwash and terraced downward to -the deep channel of the North Fork River, -presents a graphic battleground between -grass and tree. Lining the upper terraces, -from which they glower down on the dry, -well drained grass flats like a line of warriors, -are the Douglas-fir, western larch, and -ponderosa pine. Seedling trees continually -invade the prairie. But most perish early, -their shallow roots no match for the extensive -root systems of the fast-growing, moisture-greedy -grasses. If encouraged by a -series of wet summers, however, the young -lodgepoles quickly gain stature. They had -made significant inroads at Big Prairie when -the disastrously dry summer of 1967 killed -most of these 15-year-old pioneer trees.</p> -<p>These North Fork grasslands and the -immediately surrounding lodgepole pine forests -are an important spring range. Deer, -wapiti, and grizzly—and, in the wetter -areas, moose—graze or browse here. And -here, low on the western slopes of the -Livingston Range, are the park’s only stands -of ponderosa pine, a tree that prefers warm, -dry habitats. As a result, at low elevations it -often merges with the prairie community.</p> -<p>Groves of aspen colonize the eastern -prairies in areas where there is sufficient -water and protection from wind. These aspen -parklands are important havens for -<span class="pb" id="Page_69">69</span> -animals. Wherever two differing communities -interact, a phenomenon known as -“edge effect” occurs. Here wildlife exists -in abundance; the animals that favor forest -cover mingle freely with those that prefer -open areas. Aspen groves—supporting -grasses, herbs, and shrubs beneath their thin -canopies—are favored haunts for grouse, -varying hare, deer, and wapiti, all of which -find among the trees abundant food, shelter -and concealment. Populations of insects, -small mammals, and birds, which are high -for the same reasons, attract a wide range of -predators.</p> -<p>Isolated aspen groves are characteristically -dome-shaped. Because aspens are -capable of reproducing themselves vegetatively, -the grove slowly expands outward -from the parent tree. As a result, most of -these groves are either exclusively male or -exclusively female.</p> -<p>Since quick-growing aspens provide a -bountiful food source for beaver, streams -near these trees are often dammed by the -rodents flooding lowlands and creating additional -habitat in the form of willow flats. -Another “edge effect” is established, attracting -animals found near water. Waterfowl, -marsh birds, moose, mink, muskrat, skunks, -amphibians, and many others find such areas -to their liking.</p> -<p class="tb">■<br />Before the appearance of the white man, -these eastern prairies were a paradise for -animals. Once, on the summit of Rising -Wolf, light-headed from the climb and the -view of endless prairie, I fancied that I saw -that vast, undisturbed animal panorama -spread before me.</p> -<p>Principally there were the bison, darkening -the uneven land. Pronghorn bands -flashed white on ridgetops, and moose -moved through the long fingers of willow -that extended eastward with the rivers. -Caribou and wolves inhabited the shadows. -Among vast cities of prairie dogs, swift fox -and grizzly roamed. There were the clamorings -of sandhill crane, and white clouds of -trumpeter swans.</p> -<p>This land, endowed with a wealth of -wild grass, wore its wilderness well.</p> -<div class="pb" id="Page_70">70</div> -<h3 id="c8">The Forest</h3> -<p>On Gunsight Pass, the rain lancing down, I -found a sharpedged rock that split the -continent in two. On both sides the rain -rivulets ran down, a fraction of an inch -determining the stream’s destination: Pacific -or Atlantic.</p> -<p>The Continental Divide is a mighty -barrier, a line of consequence that does -more than determine watersheds. Its effect -in Glacier is dramatic, as a look at the -forests will reveal.</p> -<p>Obstructing the eastward flow of the -moisture-laden Pacific winds, the Divide -extracts a heavy annual tribute of precipitation -from the air mass, forcing it to rise -up the mountain chain, where it cools and -condenses. Chief benefactors are the low -western valleys, which respond with a lush -growth of Pacific coastal-type forests.</p> -<p>The eastern valleys, however, deprived -of abundant annual moisture and exposed to -the wind and temperature ravages of the -prairie’s continental climate, support a -dramatically different kind of forest. Here -Engelmann spruce and subalpine fir are the -climax trees, contrasted with such trees as -the western redcedar and western hemlock -of the mild and moist McDonald valley.</p> -<p>Elevation exerts an additional restriction -on the distribution of tree species. -Since climatic conditions vary with change -in elevation—lower temperatures resulting in -shorter growing seasons, and increased wind -exposure resulting in greater loss of moisture -through evaporation—we would expect -to find the forest composition change as -we ascend a mountain slope. In Glacier, -eastern valleys average 240 meters higher -than western, and thus even if they had -more moisture they would not sustain the -redcedars and hemlocks. All plants have -range limits, some narrow, some broad; and -they excel where their particular set of -preferences as to moisture, soil, sunlight, -and wind exposure are best met. On sites -that do not meet their optimum requirements, -they face being crowded out by -species better adapted to the prevailing -conditions.</p> -<p>Physical features of the land determine -vegetation also. Certain trees prefer the -moist areas along a streambed—the great -black cottonwoods, for example. And on -steep hillsides, avalanches prevent the -growth of climax trees, permitting instead -only shrubby, pliant growth—mountain-ash, -mountain maple, alder, menziesia.</p> -<p>Forest communities are named for -their dominant tree species. Thus, an area -in which Douglas-fir dominates is called a -“Douglas-fir forest.” Glacier does have -forests in which Douglas-fir is the climax -species; these are chiefly dry areas, below -1,800 meters, with south and west exposures. -But we usually associate the park with its -Engelmann spruce-subalpine fir forests, -found extensively between 1,200 and 2,100 -meters, and with the western redcedar-western -<span class="pb" id="Page_71">71</span> -hemlock forests in the McDonald -valley.</p> -<p>Because forests mature slowly and -change is usually imperceptible, we are -tempted to think of them as static and eternal. -But since a forest is a community of -living things, it responds to changes in the -environment. Subtle physical or climatic -changes, such as a rising or falling water -table or a slight increase or decrease in -annual precipitation, will favor some species -of trees and hinder others, eventually altering -the composition of the forest.</p> -<p>Other changes are more dramatic. Most -notable of these is fire.</p> -<h4>From Fire to Forest</h4> -<p>Heat lightning, glimmering soundless behind -the western peaks. Then the first low rumble. -At first the flashing had been from -cloud to cloud, but now, as the storm -nears, the first ground-spears appear, -lighting up the night. Here is a big storm, -many-celled, engulfing more and more territory -beneath its angry bulk. Lightning -dances into the dry August forest. In their -towers the lookouts stay awake.</p> -<p>Close strike and a flare-up! The ridge -snag burns like a Roman candle, sending -bright embers down. Valley, ridge, and peak -blink on and off with blue light as the -storm roars like night-firing artillery.</p> -<p>Passing overhead, the low cloud belly -brings a sudden lash of rain. But it is not -enough: tomorrow will mean long hours -of fire watch.</p> -<p>The next day dawns clear, a morning -of heavy dew. The ridge strikes did not -ignite the forest. Inspecting the storm path, -aircraft and lookouts find no evidence of -fire.</p> -<p>But two days later, in a morning of -high wind, thin smoke plumes rise upward. -Smoldering in the thick duff of the forest -floor, a lingering hot spot explodes with -the fanning wind. It quickly spreads from -a hectare to ten while the quadrants are -called in and the hot-shot crews dispatched; -then to a hundred, bringing in the smoke -jumpers and mobilizing the vast fire-control -network. A thousand hectares, perhaps ten -thousand might burn this week of big fires.</p> -<p>In the resulting skeleton forest, the -scene of devastation is almost overpowering: -life seems forevermore excluded from -this blackened ruin. But fire is nothing new -to forest communities. We may think fire -demonic because it takes from our life span -this block of mature forest, a sight we will -never again see in this place. But nature -does not operate in terms of human time -scales. This forest is simply pushed back -closer to its starting point, to begin again -its long progression toward a climax vegetation -cover.</p> -<h4>Forest Succession</h4> -<p>Through a series of complex vegetation -stages, each characterized by different herbs, -trees, and shrubs, the forest slowly returns -<span class="pb" id="Page_72">72</span> -to the type of vegetation best suited to the -physical and climatic conditions of the site; -this is called a climax community. The fact -that most of Glacier’s forests are in some -stage of recovery from fire accounts in part -for the mosaic of forest cover found here.</p> -<p>The forest of Huckleberry Mountain -on the Camas Creek road was consumed in -the 1967 fire. By 1969, among the charred, -lifeless trunks of the former forest, lush -grass and sunloving fireweed, thistle, and -paintbrush were growing. And by 1974 lodgepole -pine seedlings along the road were a -meter or two high. Lodgepole is a fast-growing -tree that requires full sun to germinate. -Forest fire is necessary for the regeneration -of these trees: the intense heat causes the -tightly closed cones to open, releasing -the seeds that will establish the forest. So -young pines developed among fireweed, -spiraea, willow, and mountain maple shrubs.</p> -<p>The lodgepole forest near the western -entrance to the park has been developing -since 1929, when fire destroyed the redcedar-hemlock -forest in the area between Apgar -and West Glacier. Beneath the scattered -spires of old larch that survived the burn, -the lodgepoles have now grown up, forming -a canopy that shades the forest floor. Because -lodgepole live only about 80 years -and will not germinate in shade, this forest -will not exist long. Shade-tolerant Douglas-fir, -white pine, Engelmann spruce and -western redcedar seedlings are now taking -hold. But the physical characteristics of -this area—the climate, terrain, and soil—are -ultimately most favorable for western redcedar -and hemlock; and unless other disruptions -intervene, this area will eventually -again become a dense redcedar-hemlock -forest.</p> -<p>But this will not happen quickly. The -soil after hundreds of years of collecting debris -will again become rich and moist. Young -hemlocks will germinate on and near -decaying logs. When old larches, firs, -and pines fall, the slow-growing redcedars -and hemlocks will take their places in the -canopy.</p> -<p>Forest succession is a more complicated -story than this; it is a fascinating study involving -herbs, shrubs, small and large -trees, and animal populations. From location -to location it will vary; only in its broad -outlines is it predictable. It is based on the -observation that, given time, a forest—or -any other plant community—will progress -until it reaches climax—that is, the stage -that will perpetuate itself.</p> -<p class="tb">■<br />How then are we to think about fire? Increasingly, -experts are concerned not so -much with fire suppression as with fire -management. For suppression has at least -three disadvantages: it allows the accumulation -of unburned fuels that can result in -“fire storms” when they are finally ignited; -an undiversified climax forest is more vulnerable -to disease than is a mixed forest; -<span class="pb" id="Page_73">73</span> -and a dense forest canopy discourages shrub -growth, an important food source for deer, -wapiti, moose, and smaller animals.</p> -<p>As the well-being of the deer herd depends -on the predators that thin its numbers, -so the long-term well-being of the forest -depends on fire to rejuvenate it periodically. -We must realize that wilderness is identified -with fire, landslide, avalanche, windfall, and -flood. Nature not only has learned to cope -with these agents of change—she depends -upon them for maintaining the delicate -balances between landscape and life. There -is in the business of nature, after all, more -than the pleasing of man’s eye.</p> -<h4>Spruce Morning</h4> -<p>Of all times to get a rock in my boot! I had -just started out, the morning was still cool -in this eastern valley, and the heavy pack -was not yet biting into my shoulders. Sitting -down beside the trail, I leaned the pack -against the base of an old spruce and began -unlacing.</p> -<p>I could hear the scratching of the red -squirrel descending to investigate, but I -didn’t look up until it let go with long indignant -chatter at finding its territory invaded. -I plunked out the pebble and began relacing -my boot. Cautiously the squirrel came down, -pausing frequently to scold, its lower jaw -quivering with rage and exposing yellow -rodent teeth. Neighboring squirrels joined -in and soon the trees danced with flicking -tails.</p> -<p>Down the squirrel came, almost to the -ground, then raced back up the tree, stopping -at each lateral branch to deliver a -vocal broadside. Finding no danger to themselves, -the other squirrels soon quit the -uproar and went about their morning business. -I was beginning to suspect that I was -committing some graver offense than the -mere exercise of squatters’ rights—perhaps I -threatened its cache of fir cones. Then into -the corner of my vision shot another form, -streaking soundless as a shadow; the squirrel -also saw it—but too late. With a thin -terrified squeak, the rodent started to go -higher; but the pine marten was above it. -The squirrel quickly reversed itself, sending -bits of bark showering down.</p> -<p>As the squirrel leaped from the tree in -desperation, the marten overtook it in mid-air; -they came down together. Clamping the -limp creature firmly in its jaws, the marten -strode up the incline of a fallen spruce. -Before it hopped off onto a shelf of higher -ground to disappear, it looked briefly back -at me. I fancied I could read, fixed in its -eyes, a certain recognition of my having -distracted its prey.</p> -<p>A breeze made me shiver, snapping me -back from that swift vision of luxuriant fur, -that blinding grace which flashed its orange -throat-patch through the trees, and I realized -I was sweating. For a moment I had been -that squirrel, eyes wide with terror, seeing -fate bear down, and powerless before the -natural order of things.</p> -<div class="pb" id="Page_74">74</div> -<p>The incident got the other squirrels -singing again; but the confidence was gone, -and soon it was quiet. What dreams do -squirrels dream, I wondered, looking -around. I saw that place more clearly then, -having been caught between a marten and -its prey. I saw each spruce: its age, its condition, -the onslaughts it had borne; the -beargrass coming up in an opening; and -down the trail a meadow that was yellow, -white, and red with sulphur plant, mariposa, -and Indian paintbrush. Bees, flies, spiders, -and butterflies worked that little garden -tucked among the crowding trees. Countless -forms of life beneath the soil and bark, in -tunnel, crevice, hole, and pocket, working -unseen to sustain their lives, and somehow, -when all were added up, maintaining the -forest as well.</p> -<p>A flicker called, its loud <i>Klee-yer</i> breaking -the forest hush. Birds, mammals, plants, -insects—all hide together here, their lives -so skillfully embroidered that no loose -thread exists that my mind might grasp -to unravel and understand the work.</p> -<p>The forest had once been a place that -obstructed my view, a great blank to stride -through, a few hours of necessary blur -before the high lake or pass was reached. -Now I was quite content to remain awhile -beneath these great-boled trees.</p> -<p class="tb">■<br />A forest, like the mountains themselves, -supports various levels of life. The floor and -substratum are a great processing plant where -bacteria, fungi, and insects work, decomposing -the plant and animal litter, recycling -dead and discarded tissue back to simpler -organic compounds, gases, and minerals, -thereby providing sustenance for growing -plants. As spiders, shrews, wrens, and -thrushes seem to know, there is good hunting -on the forest floor.</p> -<p>Just above the forest floor is the herb -layer, a seasonal layer of growth including -flowers, mushrooms, grasses, and other -small plants.</p> -<p>Above that grows the shrub layer, then -the understory of young trees awaiting their -chance to take a place in the forest’s canopy -high above. From the swaying canopy, exposed -to the full force of sun and wind, to -the dim, moist floor, the forest provides a -wide range of habitat.</p> -<p>Relatively few animals live in the treetops. -The almost incessant motion makes -nesting too hazardous for birds. Red squirrels -venture up to cut cones in the canopy, -but store their booty and make their nests -farther down.</p> -<p>In the mid-range between canopy and -understory, goshawks and Cooper’s hawks -nest. Woodpeckers, nuthatches, and sapsuckers -forage on the tree trunks and nest -in cavities they excavate or appropriate. Red -squirrels and the nocturnal flying squirrels -create a major traffic here, along with the -martens and owls that hunt them.</p> -<p>The understory and shrub layers house -<span class="pb" id="Page_75">75</span> -the greatest numbers of nesting birds. Here -the effects of storm and rain are minimized -and protective cover is greatest. Vireos, -thrushes, warblers, hummingbirds, bluebirds, -flycatchers, and others can be found among -the tangle of this sometimes impenetrable -layer.</p> -<p>The most populated area, the forest -floor, supports an astonishing abundance of -organisms. Below the busy traffic of mice, -shrews, and larger animals is a bewildering -array of insects and other invertebrates. The -attrition rate in the litter of the forest floor—a -continual battleground difficult to comprehend—is -enormous. The smaller the organism, -the greater its numbers are likely -to be. This humus-rich, moist soil teems -with bacteria, and a handful will contain -surprising numbers of small spiders, pseudo-scorpions -and almost microscopic mites.</p> -<p>Each year some two to three thousand -kilograms, dry weight, of falling material -litter an average hectare of forest. All this -plant and animal waste—twigs, leaves, -limbs, fallen trees, feathers, hair, feces, and -carcasses—is processed by the armies of -decomposers that thrive on the forest floor. -With the aid of larger creatures that break -up the plant and animal tissue, most microscopic -bacteria are able to decompose from -a hundred to a thousand times their own -weight every day.</p> -<p>Few trees die of old age in the forest. -The seedling mortality rate is necessarily -high, since far greater numbers of seeds -germinate each year than can reach maturity. -Of those that do, many fall victim to -the ever-present dangers of disease, insect -infestation, windfall, stream erosion, and -fire. Insects alone present a formidable -threat to trees, for they have evolved every -means of attack—chewing and mining -leaves, boring into twigs, eating cambium -and heartwood, sucking sap, triggering galls. -If the insect world did not police itself, -aided by spiders, insectivorous birds and -other animals, forests and other plantlife -would quickly fade before the chewing, boring, -sucking horde.</p> -<p class="tb">■<br />Through the trees the light on Citadel shows -the morning slipping by. As I start to get -up I see a garter snake sliding out into -the dusty trail, seeking the sun-warmed -earth. Moving slowly, alert for danger, it -probes the air frequently with its sensitive -tongue. But against the lightcolored duff -its dark shape offers a fine target, begging -attack. A chipmunk, watching from a nearby -lookout stump, twitches its tail nervously -over its back, curious—perhaps suspicious—at -the sight of a snake. Very slightly the -snake’s head goes up, its tongue flickering. -For a few seconds reptile and rodent regard -each other. Then the chipmunk drops back -soundlessly into its hollow stump, and the -snake lowers its head onto warm ground.</p> -<p>Some day soon, a sparrowhawk or weasel -will interrupt the snake’s morning sun-bath. -<span class="pb" id="Page_76">76</span> -The snake will fuel bird or mammal -for a time, as mice, fledgling birds, and -insects now sustain the snake. The chipmunk -too, rummaging nearby, lives in -shadows of talon and tooth.</p> -<p>Until that time of sharp encounter, -each has its own niche, a way of life, a shaft -of sun, and food enough.</p> -<h4>A Walk in the Redcedar Forest</h4> -<p>Climax! The word takes on a true significance -here, among these broad-based trees. -When you enter this forest the road noise -does not follow far—as, when you walk into -a cave and turn a corner, sound and light -are left behind. There is a surprising spaciousness, -a feeling of openness in a mature -western redcedar forest. With scant understory -and the canopy so far above and -everywhere complete, it seems like some -vast, high-ceilinged catacomb, pillared by -the huge, shaggy-barked cedars and the -deeply scored trunks of the black cottonwoods. -The floor is strewn with fallen giants -in magnificent disarray, uplifted roots still -grasping fractured rock.</p> -<p>A rainy day is a good time to walk a -cedar trail, when the dull light seems to -shine from the wet moss, making the underleaves -of devil’s-club and Rocky Mountain -maple glow. Wind and rain, like light, -penetrate with difficulty the latticework of -this canopy; thin lines of fog develop over -the bogs. The air is fresh with growing -plants, snow-cold still when the first spring -flowers appear.</p> -<p>Fiddleheads of unfolding lady ferns line -the trail in May, pushing up from the hub -of last year’s leveled, lifeless fronds. Beds -of trillium shine their white, three-pointed -flowers like flashlights in the dark recesses. -Unlike the small, hidden calypso orchid, -which bears its purple spikes and yellow -throat low above the moss, the trilliums -make no secret of spring growth. They are -bold, handsome plants, broad-leaved and -tall, with waxy white petals that tinge to purple -in their month-long bloom.</p> -<p>Moss covers everything. Boulders are -green and weightless-looking, resilient and -topped with miniature forests of cedar -seedlings. Ancient fallen trees are disguised -with blankets of moss, sprouting -hemlock here and there. The rich greens -that characterize Glacier’s summers seem -to begin here amid the moisture-glossed -leaves of twinflower, bunchberry and bead-lily.</p> -<p>Later, the spiders will spin thousands of -kilometers of gossamer filament among the -trees. The orb-weavers will hang their webs -high and low, suspended in every opening. -Walking through the forest then, you will see -shafts of sunlight whirling in the higher -webs until they seem like tops set spinning -among the treetrunks.</p> -<p>Indianpipes, the “ghost flowers” that -need no light to grow, will break through -the forest soil. Like mushrooms, with fruiting -bodies that are nourished by underground -<span class="pb" id="Page_77">77</span> -mycelia, these saprophytes absorb -their nutrients from a fungus that covers -their roots.</p> -<p>Receiving an average of about 18 centimeters -more annual precipitation than -forests east of the Divide, Glacier’s redcedar-hemlock -community hoards its moisture. -Its dense growth and the surrounding -mountain walls inhibit the circulation of -drying winds. Mosses and ferns transpire -their moisture, which you can feel; place -your hand close, and you will sense a coolness -like the air exuding from an ice cave. -Draped from the tree limbs are long filaments -of squawhair and goatsbeard, black -and grey lichen strands that flourish in the -damp air.</p> -<p>Except for the black bear, few large -animals inhabit the deep forest. Grizzlies -find better forage in meadows or along the -forest edge. Since shade discourages shrubby -undergrowth, deer and wapiti will search -elsewhere for browse. In summer, wapiti, -grizzlies, and mule deer bucks tend to -wander up into high meadows.</p> -<p>Contrasted to the noisy, conspicuous -birds of the prairie—meadowlarks and bobolinks—birds -of the forest seem elusive -and secretive. Although numerous, the -varied thrushes, Townsend’s solitaires, and -Swainson’s thrushes are seldom seen; but -when approached, they fly silently off and are -swallowed by the forest shadow.</p> -<p>There seems to be serenity in a mature -forest, as though the struggle for life is -somehow suspended, the needs of the animals -here less urgent, muffled. The towering -redcedar forest seems to be no battlefield -at all, but rather a monument to what -Earth can do.</p> -<h4>The Perpendicular Night</h4> -<p>Behind Avalanche campground a trail leads -back toward Lake McDonald Lodge. I decided -to follow it one June evening, to experience -the sensation of the deep forest -changing into night. With the nearby mountain -wall intercepting the sun, dusk comes -early to this valley. On the prairie, night -passes across the landscape in an even line, -forthright as a waxing tide; you can almost -feel the globe in its turning from the sun. -There is reassurance in the night’s coming, -its steady purple doming over the sky.</p> -<p>But here darkness seems to sprout from -the earth. It collects beneath the hemlock -clumps, bridges the creekbottoms. It seems -to flit from place to place. You look about, -uneasy, trying to catch it here or there, but -always miss its infiltrations. It captures the -narrow clearings when you look away; -pockets of tree-darkness join together, -forcing the light upward until the tree-tops -seem impossibly bright and distant.</p> -<p>Through the trees I could see a dozen -fires dance in the growing shadow, wood-smoke -and camp sounds filling the air. -Turning uptrail, I felt a reluctance to leave -the presence of those fires—a senseless feeling, -but strong. A growing forest-dread impelled -me almost physically backward to -those circles of firelight. I felt the need to -be near a fire, to be reassured by heat and -light. Fire was our greatest friend, our -greatest weapon. With it we beat the long -ages of ice and held the forest gloom -away. There was no harm here, only silence; -yet the longer I walked, with beard-moss -hanging down like daggers all around, -the more I craved the comradeship of fire.</p> -<p><span class="lr"><span class="small"><i>Continued on <a href="#Page_104">p. 104</a></i></span></span></p> -<div class="pb" id="Page_78">78</div> -<p class="pcap"><b id="f2fig3">The Vital Predator</b></p> -<p class="pcapc">The merciless law of predation might at -first thought seem cruel; but the predator -plays a vital part in maintaining the -balance of the biotic community. Without -the controlling factor of predation, prey -species quickly enlarge their populations. -If plant eaters are not checked, the resulting -excess population exceeds the -carrying capacity of the range. Food -supply rapidly diminishes. In a damaged -range, competition and stress result, -usually culminating in a massive die-off -through starvation and disease.</p> -<p class="pcapc">Ironically, predators thus provide a service -to their prey. First to fall to the predator -are the old, the diseased, the unwary, and -the young. By removing many young and -old deer from a typical herd, cougars -lessen competition among the deer for -choice range, thus tending to keep herbivore -numbers at parity with the land’s -carrying capacity. Only the strongest and -wariest deer survive, ensuring that the -fittest will continue the species. When -man upsets this delicate balance—destroying -predators in the hope of increasing -numbers of game animals—the -result is ecological disaster. In the 1930s, -in a misguided attempt to “preserve” the -whitetail deer herds of the park’s North -Fork area, many coyotes and cougars -were exterminated. In 1935 alone, 50 -cougars were killed. Relieved of the pressure -of predation, the deer flourished. In a -few years, however, the normally adequate -range was severely overbrowsed. Suffering -also from this imbalance were wapiti -(“elk”) and moose, ungulates that share -the winter range with deer.</p> -<p class="pcapc">Some predators are more specialized -than others. The Canada lynx, for -example, has oversize feet, an adaptation -that helps it move across deep snow -without breaking the surface. As a result, -it is an efficient predator of the snowshoe -hare, another large-footed animal. Relying -on this adaptation, the lynx feeds almost -exclusively on snowshoe hares. Consequently, -its numbers inevitably fluctuate -with the 10-year “boom and bust” cycle of -the snowshoe.</p> -<p class="pcapc">The coyote, on the other hand, is a -generalized predator, exploiting whatever -prey is currently abundant. Should mice -or ground squirrels be in short supply, it -will subsist on anything from grasshoppers -to berries until favored prey again becomes -available. (Animals that normally -eat both plant and animal food are -referred to as omnivores.) Generalized -predators are thus better equipped to -survive temporary ecological imbalances, -maintaining their numbers at relatively -consistent levels from year to year.</p> -<p class="pcapc">Carnivores all, the animals on these pages -illustrate various adaptations for -capturing prey.</p> -<div class="pb" id="Page_79">79</div> -<div class="img" id="fig50"> -<img src="images/p030.jpg" alt="" width="800" height="580" /> -<p class="pcap">The population of the Canada lynx, which is widely distributed -in Glacier’s coniferous forests, fluctuates in -cycles. The lynx is abundant or scarce depending on -the population condition of its chief prey, the -equally cyclic snowshoe hare.</p> -</div> -<div class="pb" id="Page_80">80</div> -<div class="img" id="fig51"> -<img src="images/p031.jpg" alt="" width="700" height="817" /> -<p class="pcap">The cougar, which feeds primarily on deer, requires -a large territory. Because of its strength, stealth, and -speed, American folklore has given this wary cat a -false reputation as a man-stalker.</p> -</div> -<div class="pb" id="Page_81">81</div> -<div class="img" id="fig52"> -<img src="images/p031a.jpg" alt="" width="800" height="597" /> -<p class="pcap">The red fox depends largely on a well-developed -sense of smell to locate its prey; it also relies on -its keen eyesight, speed, and agility to capture mice, -hares, birds, and whatever else it can run down or -surprise.</p> -</div> -<div class="pb" id="Page_82">82</div> -<div class="img" id="fig53"> -<img src="images/p032.jpg" alt="" width="700" height="725" /> -<p class="pcap">To feed its demanding young, the Swainson’s thrush -hunts for insects along the forest floor and in the -dense underbrush. This thrush relies on its secretive -behavior to protect its nest near the ground from -detection by other predators.</p> -</div> -<div class="pb" id="Page_83">83</div> -<div class="img" id="fig54"> -<img src="images/p032a.jpg" alt="" width="500" height="514" /> -<p class="pcap">Armed with enlarged forelegs, the crab spider waits on -or near flowers to ambush visiting bees, flies, or -other insects. Its venom produces a quick kill, allowing -it to attack insects many times its own size.</p> -</div> -<div class="img" id="fig55"> -<img src="images/p032b.jpg" alt="" width="463" height="800" /> -<p class="pcap">The spotted frog is a large-mouthed predator that not -only eats water striders and other insects but also -gulps down smaller frogs and small fish.</p> -</div> -<div class="pb" id="Page_84">84</div> -<p class="pcap"><b id="f2fig4">Protective Coloration</b></p> -<p class="pcapc">To escape extermination, each species -must in some manner foil its enemies. -Protective coloration is one of the more -common adaptations helping to do this. -Most animals resemble their environment -to some extent. The conspicuous -markings of some, like the bitter-tasting -monarch butterfly or the striped skunk, -seem to function as a warning to -prospective predators that it is in their -best interest to look elsewhere for a meal.</p> -<p class="pcapc">Some animals, such as the white-tailed -ptarmigan and the snowshoe hare, have -seasonal changes in plumage or pelage, -wearing white in winter and brown in -summer. Even predators, such as -longtail and shorttail weasels, benefit -from seasonal camouflage. Protective -coloration makes them less noticeable -to prey species and to larger predators.</p> -<p class="pcapc">Many insects, too, change coloration with -the season. Bright green grasshoppers of -early summer become more brown with -each molt, matching the changes in the -surrounding vegetation.</p> -<p class="pcapc"><i>Obliterative shading</i> is especially important -to animals that frequent more than -one habitat. Seen from above, turtles -match their dark background; from below, -because of their lighter underbody -shading they blend into the bright -skylight.</p> -<p class="pcapc"><i>Disruptive coloration</i> aids in breaking up -an animal’s outline. Butterflies and moths -commonly have disruptive wing markings. -The distinctive shapes of eyes can be -concealed. Eye coloration may mimic -body color—as in the green katydid—or -the eye may continue disruptive body -markings.</p> -<p class="pcapc">Ground-nesting birds are especially vulnerable -to attack. Their eggs tend to be -heavily blotched with earthy colors, -making them less conspicuous. Chicks -also carry these disruptive colorations on -natal down.</p> -<p class="pcapc">Most mammals, with coats of brown or -gray, are inconspicuous when motionless. -Deer fawns are endowed with speckled -coats, mimicking the sun-flecked forest -floor; this disruptive coloration, coupled -with absence of scent and their -instinctive “freezing” behavior, makes it -difficult for predators to detect them.</p> -<p class="pcapc">The whitetail deer not only uses its white -“flag” to warn others in the herd of -danger; it also allows a pursuing predator -to use it as a target. When the tail is -suddenly dropped—abruptly obliterating -the bright white patch—the deer seems to -disappear into its dim surroundings.</p> -<p class="pcapc">Since overly conspicuous animals are -prone to predation, natural selection favors -development of appropriate camouflage.</p> -<div class="pb" id="Page_85">85</div> -<div class="img" id="fig56"> -<img src="images/p033.jpg" alt="" width="687" height="700" /> -<p class="pcap">For such ground-dwelling birds as the white-tailed -ptarmigan, camouflage is an important survival adaptation. -The ptarmigan changes its plumage to match its -surroundings: it is white in winter, speckled in summer. -Moving slowly and refraining from flight, it is less -likely than more-active birds to be detected by sharp-eyed, -motion-conscious predators.</p> -</div> -<div class="pb" id="Page_86">86</div> -<div class="img" id="fig57"> -<img src="images/p034.jpg" alt="" width="800" height="618" /> -<p class="pcap">Birds that when hatched are covered with down and -are able to move about freely are called <i>precocial</i>. -They are less dependent upon their parents than are -<i>altricial</i> young, which are naked and helpless when -they hatch; but they must rely heavily on a resemblance -to their surroundings for survival during their -first flightless weeks. This spruce grouse chick, which -blends into its sunflecked forest-floor habitat, is an -example of a precocial bird.</p> -</div> -<div class="pb" id="Page_87">87</div> -<div class="img" id="fig58"> -<img src="images/p034a.jpg" alt="" width="800" height="518" /> -<p class="pcap">The bold disruptive pattern of the killdeer chick’s -plumage helps this precocial bird avoid detection in -its open-prairie environment. This adaptation, coupled -with the chick’s instinct to freeze at the approach of -danger, ensures that enough young will survive to -perpetuate the species.</p> -</div> -<div class="pb" id="Page_88">88</div> -<p class="pcap"><b><i id="f2fig5">Ursus arctos horribilus</i>: The Vulnerable King</b></p> -<p class="pcapc">At the apex of the food pyramid, this great -beast is unquestionably the king of -Glacier’s biotic community. Yet the long-range -future of the grizzly bear is uncertain. -With the grizzly exterminated from -most of its former range—which once -extended into the midcontinent and south -into Mexico—its numbers have dwindled -in proportion to its diminished range. -Present concentrations in the contiguous -United States remain in and around -Yellowstone and Glacier National Parks. -Probably fewer than 200 of these magnificent -creatures live in Glacier National -Park.</p> -<p class="pcapc">Grizzlies are easily distinguished from -the more common black bear. In -addition to larger size and heavier build, -grizzlies have a characteristic shoulder -hump; long, conspicuous claws; and a -broad, concave face that gives them -a “dished-in” appearance. Fur is usually -brown; like the fur of the black bear, -however, color may range from black -to yellowish. Light tipped hairs make the -fur appear frosted, giving rise to the -nickname, “silvertip.”</p> -<p class="pcapc">Grizzlies, popularly considered arch -predators, are more accurately described -as omnivores. Carrion, grasses, cow -parsnip, and several species of berries, -bulbs, and tubers make up a grizzly’s diet, -along with insects, small mammals, and -an occasional ungulate that it can catch. -As a result, grizzlies play several roles in -the biotic community, functioning as -herbivore, scavenger, and predator.</p> -<p class="pcapc">Ranging widely in all life zones, grizzlies -follow the spring snowmelt up to the -alpine meadows, returning to lower elevations -to hibernate from November until -April. One to three cubs are born in -midwinter during hibernation. Since the -maternal bond lasts two years, a sow will -accept a mate only every other year. -Mortality of subadults is high, resulting -principally from competition among the -bears themselves. As with most animals, -range—habitat—appears to be the -limiting factor of grizzly populations.</p> -<p class="pcapc">The grizzly is normally shy and fearful -of man—but highly unpredictable. -Wounded or sick bears, sows defending -cubs, young adults, and bears that -have become conditioned to human -scent are the most dangerous. As -humans continue to encroach on grizzly -territory, odds of confrontation also -increase. Recent fatalities and personal -injuries inflicted by grizzlies pose a -vexing problem to the National Park -Service, which is charged with visitor -safety on the one hand and protection -of the park’s remaining grizzly -population on the other. Continuing -study of grizzly ecology and increasingly -enlightened bear management programs -will, it is hoped, allow man and bear -to co-exist in a wilderness both require.</p> -<div class="pb" id="Page_89">89</div> -<div class="img" id="fig59"> -<img src="images/p035.jpg" alt="" width="690" height="700" /> -<p class="pcap">Grizzlies are fond of succulent spring grasses.</p> -</div> -<div class="pb" id="Page_90">90</div> -<div class="img" id="fig60"> -<img src="images/p036.jpg" alt="" width="446" height="801" /> -<p class="pcap">Traversing all life zones in the park, the grizzly is a -true opportunist, eating anything from ants and -berries to wapiti.</p> -</div> -<div class="pb" id="Page_91">91</div> -<div class="img" id="fig61"> -<img src="images/p036a.jpg" alt="" width="688" height="700" /> -<p class="pcap">Seldom will a grizzly exceed 225 kilograms in Glacier. -This is a young adult.</p> -</div> -<div class="pb" id="Page_92">92</div> -<p class="pcap"><b><a id="f2fig6">Bald Eagles and Kokanee Salmon: A Recent Gathering</a></b></p> -<p class="pcapc">In 1916 the kokanee salmon, a small, -land-locked form of the Pacific coast -species, was planted in the Flathead -drainage. With the first planting augmented -by additional stockings, the fish -thrived in cold, deep Flathead Lake, and, -to a lesser extent, in Lake McDonald. -The salmon fed almost exclusively on -zooplankton.</p> -<p class="pcapc">By the mid-1930s, salmon runs were -becoming established. The outlet of Lake -McDonald provides an ideal spawning site -for the salmon. The fast-flowing water is -clear, cold, and shallow, and the creek -bed is gravelly.</p> -<p class="pcapc">Averaging 0.3 meters in length and weighing -less than a half-kilo, the 4-year-old -adult salmon cease feeding and begin to -migrate. Many thousands swim the 100 -kilometers from Flathead Lake to -McDonald Creek. Males appear in the -creek first, arriving in late September, and -are soon followed by the females.</p> -<p class="pcapc">Using her tail to dig a redd (a shallow -nest depression), the female deposits -about 650 eggs. After fertilization by the -male, the eggs are covered over. The -adults die within three weeks after spawning, -their bodies exhausted from the -rigorous migration journey and the weeks-long -lack of sustenance.</p> -<p class="pcapc">Egg fatalities are high, due to stream -erosion and disturbance by other spawning -salmon. Hatching in late March, the -fry work their way out of the gravel and -migrate downstream.</p> -<p class="pcapc">Attracted to the 75,000-150,000 salmon -concentrated in a 3-kilometer stretch of -shallow water, bald eagles begin gathering -at McDonald Creek in October. It is not -known where the eagles come from or -where they go after the spawning run. -Glacier has fewer than 20 summer-resident -bald eagles, and these are distributed -among the remote lakes of the North -Fork area.</p> -<p class="pcapc">In 1939, 37 bald eagles were counted -along the creek. By 1969, 373 were reported, -representing approximately 10 -percent of that year’s estimated winter -population for the contiguous United -States. Since 1960, the count has averaged -240 birds. (In 1977 there were 444.)</p> -<p class="pcapc">Eagles feed by swooping down to pluck -salmon from the water or by wading out -to grab a fish stranded on a shallow -riffle. An eagle may consume as many as -six fish a day. Immature birds are not as -adept at catching fish and may harry -adults or other immatures into releasing -their catch.</p> -<div class="pb" id="Page_93">93</div> -<div class="img" id="fig62"> -<img src="images/p037.jpg" alt="" width="684" height="700" /> -<p class="pcap">From its vantage point, this mature bald eagle -examines the waters of McDonald Creek. Average -weight is 5.7 kilograms; average wingspan is 2.2 -meters. Females are slightly larger than males.</p> -</div> -<div class="pb" id="Page_94">94</div> -<div class="img" id="fig63"> -<img src="images/p038.jpg" alt="" width="800" height="483" /> -<p class="pcap">This immature bald eagle lacks the familiar white head -and tail of the adult birds. It will not acquire those -markings until it is several years old.</p> -</div> -<div class="img" id="fig64"> -<img src="images/p038a.jpg" alt="" width="800" height="541" /> -<p class="pcap">Breeding male and female kokanee salmon are easily -distinguishable; as spawning time approaches, they -change appearance. The dark gray backs turn red; -heads become green, and the males develop humped -backs and hooked jaws.</p> -</div> -<div class="pb" id="Page_95">95</div> -<div class="img" id="fig65"> -<img src="images/p038b.jpg" alt="" width="800" height="481" /> -<p class="pcap">Swooping upward with a fish, a mature eagle heads -for a convenient perch to consume its catch. A -strategically located tree may contain 30 birds.</p> -</div> -<div class="pb" id="Page_96">96</div> -<p class="pcap"><b><a id="f2fig7">A Triumph of Many Colors</a></b></p> -<p class="pcapc">Grassland, meadow, tundra, or any other -area in Glacier suitable for plant growth -and supplied with abundant sunlight -produces an extravagance of wildflowers. -This display of various shapes and colors -is neither an accident nor a mere decoration -of nature. Nor would Earth’s -recent explosion of mammal and bird -species have been possible without the -evolution of flowering plants.</p> -<p class="pcapc">Two hundred million years ago, early -in the Age of Reptiles, angiosperms -(flowering plants) had not yet evolved. -Plant reproduction still relied on spores -and cones. Then, during the Cretaceous -Period, the last sediments were being laid -down in the inland sea that covered most -of Montana. (It was these sediments that -the ancient Precambrian rocks of Glacier’s -mountains later overrode, forming the -Lewis Overthrust.) During this period -the evolutionary miracle occurred: -flowering plants—grasses, vines, shrubs, -broadleaf trees, wildflowers—inherited -the Earth.</p> -<p class="pcapc">The timing was important. As Earth’s -tropical climate gradually changed to -temperate extremes during this period, -the domination of cold-blooded dinosaurs -ended and the moisture-demanding -coniferous forests that had covered the -earth in green monotony began to shrink. -Angiosperms provided a solution to the -ecological void: grasses and forbs grew -where trees no longer could. Most important, -relationships evolved between this -new class of plants and the relatively -few species of insects then existing.</p> -<p class="pcapc">Insects began to use the pollen of flowering -plants; the angiosperms, in turn, -evolved bright petals and nectar that -exploited visiting insects for the plants’ -own reproductive purposes. This partnership -allowed insects to diversify rapidly, -evolving new, specialized forms such as -bees, moths, and butterflies. As a result, -predatory forms of insects and arachnids -also rapidly diversified.</p> -<p class="pcapc">The most dramatic change, however, -involved warm-blooded birds and -mammals, whose high rates of metabolism -required high-energy fuels. Unlike -gymnosperm seeds, which contain no -protective covering, angiosperm seeds are -surrounded by a fruit. The development -of these highly nutritious seeds, and -the attendant explosion of insect -species, ensured survival of the newly -evolved birds.</p> -<p class="pcapc">As birds diversified into seed-eaters, -insectivores, and carnivores, mammals, -then uncertain little ratlike creatures -darting among the feet of dinosaurs, -began a rapid rise to dominance; -grasslands promoted an explosion of -herbivorous and carnivorous species.</p> -<p class="pcapc">The evolution of angiosperms, and the -animal revolution it made possible, came -with amazing speed. Most significant, it -was a vital first step upon which the -meteoric rise of man depended.</p> -<div class="pb" id="Page_97">97</div> -<div class="img" id="fig66"> -<img src="images/p039.jpg" alt="" width="700" height="715" /> -<p class="pcap">Indian paintbrush is common at all elevations -below tundra. It may be white, yellow, orange, -pink or red. The actual flowers, inconspicuous and -green, are surrounded by brilliantly colored bracts. -Semi-parasitic on other plants, paintbrush is normally -found growing in conjunction with other wildflowers; -its roots steal sustenance from neighboring plants.</p> -</div> -<div class="pb" id="Page_98">98</div> -<div class="img" id="fig67"> -<img src="images/p040.jpg" alt="" width="500" height="509" /> -<p class="pcap">Yellow stonecrop, widely distributed in forest and -scrub-forest zones, is one of the park’s few plants -having succulent leaves, an adaptation that helps it -survive in such situations as dry, rocky outcrops.</p> -</div> -<div class="img" id="fig68"> -<img src="images/p040a.jpg" alt="" width="500" height="520" /> -<p class="pcap">The Calypso orchid grows in the cool, shadowed -forest where light is dim. It lives in partnership with -certain fungi that exist about the orchid’s roots and -seem to help nourish it.</p> -</div> -<div class="pb" id="Page_99">99</div> -<div class="img" id="fig69"> -<img src="images/p040b.jpg" alt="" width="700" height="721" /> -<p class="pcap">Silky lupine, a legume, has nitrogen-fixing nodules on -its roots, thus allowing it to grow in nitrogen-poor -soil. It is widely distributed in grassland and forest -communities.</p> -</div> -<div class="pb" id="Page_100">100</div> -<p class="pcap"><b><a id="f2fig8">Fire Succession: Key to Continuity</a></b></p> -<p class="pcapc">Most of Glacier’s fires are lightning-caused. -Strikes may flare up immediately; -or fires may smolder in the forest duff -for days until fanned into flame by wind. -<i>Ground fires</i> may race through the forest -understory, causing minor damage; or -they may bridge the understory and reach -the canopy, thus becoming rapidly spreading -<i>crown fires</i>. Under certain conditions, -uncontrollable infernos may develop, -generating terrific winds and heat. These -rare conflagrations are called <i>fire storms</i>.</p> -<p class="pcapc">Every type of forest habitat has <i>climax -vegetation</i>—trees and shrubs that are best -suited to the site and thus maintain -themselves indefinitely if not disrupted.</p> -<p class="pcapc">After a major fire, habitat conditions are -usually so altered that the site must pass -through several <i>seral stages</i> before conditions -are such that climax vegetation can -return. A <i>sere</i> is a series of plant communities -that follow one another in orderly -fashion until climax conditions are again -reached.</p> -<div class="img" id="fig70"> -<img src="images/p041.jpg" alt="" width="800" height="490" /> -<p class="pcap">Lightning fires occur most often during the hot, dry -weeks of late summer.</p> -</div> -<div class="pb" id="Page_101">101</div> -<div class="img" id="fig71"> -<img src="images/p041a.jpg" alt="" width="800" height="486" /> -<p class="pcap">When the forest is dry, lightning often causes quick -flare-ups.</p> -</div> -<div class="img" id="fig72"> -<img src="images/p041b.jpg" alt="" width="800" height="546" /> -<p class="pcap">The forest may continue to burn for days after the -main conflagration has passed.</p> -</div> -<div class="pb" id="Page_102">102</div> -<div class="img" id="fig73"> -<img src="images/p042.jpg" alt="" width="700" height="717" /> -<p class="pcap">After a major fire, sun-loving grasses, shrubs, and -wildflowers quickly invade the former forest. Deer -and wapiti benefit from these new food sources.</p> -</div> -<div class="pb" id="Page_103">103</div> -<div class="img" id="fig74"> -<img src="images/p042a.jpg" alt="" width="500" height="512" /> -<p class="pcap">Lodgepole pine, a pioneer species quick to take over -burned areas at lower elevations, grows rapidly. These -trees are five years old.</p> -</div> -<div class="img" id="fig75"> -<img src="images/p042b.jpg" alt="" width="465" height="800" /> -<p class="pcap">This is a Glacier National Park forest 80 years after -a major fire.</p> -</div> -<div class="pb" id="Page_104">104</div> -<p>Sudden hammering made me jump. -Above the forest darkness, a pileated woodpecker -leaned out from a high larch snag, -braced against the trunk by its specialized, -stiff tail feathers. This was the first time I -had seen this big white-and-black bird, the -“cock-of-the-woods.” There was ample evidence -of his work: the deep, oblong excavations -in the trunk and the pile of large wood -chips at its base, both characteristic of this -species. Again he hammered, and I could -see the chips falling. After a little edge-work -around the hole, he extracted a grub -and flew off, yammering against the advancing -dark.</p> -<p>Near a stream I stopped to sit down, -to listen to the water and maybe catch sight -of some small animal. Across the narrow -defile, from a slope dense with young hemlock, -came the buzzing note of a varied -thrush. Several notes followed, all on a -different pitch, all drawn out, level and -clear; the quality was pure but songless, disjointed, -deliberate, like someone testing the -reed of a strange woodwind. There seemed -no gladness in the heart of this thrush. The -song was dark, haunting, lonely.</p> -<p>On the trail ahead I could make out a -bird hopping rapidly along. After passing -the spot I could hear its song. There -couldn’t be a hundred meters between -us, yet it seemed to be coming from a -great distance. I listened for as long as it -would sing. I tried to hear it for what it was, -a male Swainson’s thrush proclaiming its -territory. But the ethereal, flute-like phrases -seemed an evensong made not for man’s -ears but only for the forest itself.</p> -<p>I hurried on after the bird had ceased. -It was getting dark beneath the trees, but I -was beginning to be aware of creatures -underfoot, the mad dartings of shrew and -vole, more imagined than seen. When a deer -mouse jumped away I got out my flashlight. -Soon the beam caught a woodrat sitting atop -a fallen log. The light didn’t bother him -in the least; as I approached, he picked up -his bushy tail in his forepaws. Whiskers -twitching, he looked more caricature than -real. Then he bounded off the log with -graceful, arching hops, and disappeared into -the night.</p> -<p>Against a patch of sky that appeared in -a clearing, I could make out bats, circling -and dipping like swallows. Locating a -hovering moth, I kept the light beam on it -until it vanished into a furry streak of -silence. It was time to head back.</p> -<p>By now it had become utterly dark -within the trees, a moonless, sightless, alien -<span class="pb" id="Page_105">105</span> -world, given over to the marble-black eyes -of the small night mammals and the creatures -that hunt them. I thought of the -strange, unseen societies of the flying -squirrels, the nocturnal counterparts of red -squirrels; of the great-horned owls, inspecting -the same ground the goshawks scanned -during the day. Perhaps a foraging red fox -moved through the darkness nearby, or a -coyote on night patrol.</p> -<p>The flashlight beam probed ahead along -the trail. The exposed roots were given unnatural -shading and they seemed to thicken -and squirm as I approached. On either side -the tree trunks appeared to step backward -from the dim glow of the light. I felt lost -in this night, thinking of the great darkness -in all the timbered ridges that ran westward -from the Divide. In this vast cathedral -of crowded tree and peak, night was stood on -end, the stars shrunken to a circle overhead, -as if seen from the bottom of a well. -Mouselike, shivering, insignificant in this -wilderness, I scurried back to find a fire -and fill my empty senses with its heat and -snap and light, holding off the fright of -night and thinking of tomorrow’s sun.</p> -<h3 id="c9">Scrub-Forest</h3> -<p>The crowning beauty of Glacier—the high, -cirqueheld meadows that scent the wind with -wildflower and waterfall—belongs to the -zone of scrub-forest.</p> -<p>At Logan Pass you are introduced to -the highlands. Here an exquisite upland -basin holds the Hanging Gardens, a wildflower-clothed -gradient laced with stair-step -bogs and lines of wind-bent subalpine fir. In -the dawn sun, before the first engine noise, it -shines unbroken, dewbright and sagging like -a spider web secured to the circle of surrounding -peaks.</p> -<p>This is the region the hiker remembers -best. The tall mountains wear this zone close -to the cliffs, and the trails encounter it -near the passes or follow it for long, level -stretches, as along the Garden Wall. I -remember Preston Park and Fifty Mountain, -the fire-touched bench of Granite -Park and the first sight of Sperry chalet, -built on a brow of rock at the upper reach -of trees. But most of all I remember the -terrible waterfall that becomes Bowman -Creek, the plunge of nearly a kilometer -that drains the magnificent upland bench -called Hole-in-the-Wall.</p> -<h4>Hole-in-the-Wall</h4> -<p>September. The season is growing late, the -meadow-rue dying and the leaves of the -wild strawberry failing at last. Everywhere -the red contagion of autumn surrounds the -<span class="pb" id="Page_106">106</span> -vital green. The lower valleys have lost the -whistle of ground squirrels. They sun themselves -no longer these late, mild days. Ripe, -sluggish, and hawk-vulnerable, they sensed -the need of hibernation.</p> -<p>It has been eight years since I last -visited Hole-in-the-Wall, but I retain its -dimensions and hear its dozen waterfalls -at will. Once you have seen this basin you -have a measure by which to judge the high -country and a thirst for the meadows at -tree-line.</p> -<p>In Glacier, treelimit ranges between -1,850 and 2,300 meters, depending on local -conditions. The upper limit of tree growth—rarely -an even, horizontal line—is generally -an indistinct band running erratically across -a mountain’s face: a tension zone reflecting -variations in wind and sun exposure, degree -of slope, snowpack accumulations, and the -presence of adequate soil and water.</p> -<p>Subalpine fir, whitebark pine, and Engelmann -spruce do not relinquish easily their -upward climb; where conditions become -severe, their growth is retarded and their -stature dwarfed. Deformed and pruned by -wind, their leaders winter-killed when they -outreach the protection of the winter snowpack, -trees become shrubs, forced to hug -the ground. Size belies age in these elfin -forests, or krummholz, where the growing -season is painfully brief and progress is -always uncertain. A twisted, gnarled little -bush, more snag than live branch, bearing -a single cone or two, may be senior by a -century to the giants of its race in the valley -below, which yearly shower the ground -with an abundant crop of cones.</p> -<p>This time I will come from Goathaunt, -passing Lakes Janet and Francis, reaching -Brown Pass from the east, and camp in -the spectacular garden between Brown and -Boulder Passes.</p> -<p>Meadows and rock slides break the -forest as the trail gains elevation and distance -through the valley. The spruce and fir thin -out rapidly at the valley head, the trail -climbing the grassy slope to low, broad -Brown Pass. Below the pass is Thunderbird -Pond, which receives the meltwater from -a glacier high on a shelf of Thunderbird -Mountain and is bordered by a low jungle -of willow. In the water stands a bull moose, -its heavy, fully formed antlers ready for the -season’s impending business.</p> -<p>I was hoping again to see Cassin’s -finches and Audubon’s warblers on the pass; -but the fir grove is quiet. Sitting down to -rest and listen, I become aware of a strange -silence. No birds sing or flit among the -trees, no alarms pass back and forth among -alert ground squirrels. There is no wind—an -odd condition for the Continental Divide. -This place seems to be holding its breath. -High overhead, a veil of cirrus cloud arranges -long spears across the sky.</p> -<p>Moving off the pass, along the dome of -Mt. Chapman, I experience anew the old excitement -of this high country. Abruptly the -gorge of Bowman valley opens up, revealing -<span class="pb" id="Page_107">107</span> -the twisting blue snake of Bowman Lake -far down the narrow, cliff-imprisoned valley. -Here again are the northern titans—Numa, -Peabody, Boulder, Thunderbird, and Rainbow; -and Carter, with its high glacier -baring blue ice teeth to the sun.</p> -<p>It is not the climb that makes your -heart pound now; the trail is suddenly narrow -and cliff-defiant, cut by the plunging -waters of snowbanks far above. These are -splendid peaks, unmatched in a land of -muscled, brutal earth. Even the air seems -to retain the scent of glacier work.</p> -<p>At last the view of Hole-in-the-Wall, a -staircase cirque excavated between the gigantic -spread ribs of Mt. Custer. The slopes -of beargrass are seed-spotted and gaunt -now, the white fullness gone. Western pasqueflowers -have accomplished their magic -transformation; known in this season as old -man’s beard, they nod their tufts of grizzled -seedhead silk in the wind. Red and yellow -monkeyflowers bloom yet, crowding along -the many stream courses, and waterloving -sedges and mosses surround pools of collected -water on the broad horseshoe tiers.</p> -<p>A spur trail drops down into the campground -on the last ledge. Through a cleft in -its lip plummets the gathered water of the -basin. From the valley below, the waterfall -appears to be springing from a hole in the -headwall, giving this basin its name. Down, -down, down, roars the water where once a -mighty glacier ground its teeth.</p> -<p>I leave until later the making of camp; -by now the sharp shadows of Boulder -Peak stab the valley forest and are beginning -the upward assault of Thunderbird.</p> -<p>Around the basin headwalls, last winter’s -snowbanks remain formidable. Snow -caves send out meltwater torrents. Glacier -lilies and patches of spring beauty line their -fringes. Pasqueflowers bloom in pockets. -Here, among the asters of August, bloom -also the first flowers of spring, shooting up -as the snowbanks shrink, making these spots -of snow-free ground a patchwork of May -and July, August and June. The shrubs that -line the furious water are willows, still bud-swollen -this tenth day of September. The -coming days will bring a sharp surprise.</p> -<p>Winter will soon stop the melting of this -snow. Could it be that I am seeing the first -year of a reawakening ice age? If so, each -year the snowfields would grow thicker and -broader, connecting the shelves into one ice -mass again, lilies and willows entombed, the -summer heat failing to rescue them, until the -ice at last began to slide, stripping the soil -and once more plucking at living rock.</p> -<p>Then these dwarfed fir, which cling -precariously to the cliffs and hide behind the -backs of boulders, would be in more danger -than they were from their recent antagonists. -Engulfed by ice, they would know the shearing -wind no more. Their skeletons would -rain down into the valley below, signalling -another long forest retreat. But they have -waited out the mountain ice before and -would send their seeds again to this valley, -<span class="pb" id="Page_108">108</span> -changed however it might be, as they have -always done.</p> -<p>Evening brings out two sleek mule deer -does. As they graze, their large ears stand -erect, sorting out the lesser sounds from -the ceaseless roar of water. Both raise -their heads and point their ears, statue -straight, at the scuttle of a porcupine. A -noise among the rocks draws a backward -glance and focus of those ears. I would -like the sensitivity of such fine equipment, to -hear what deer have always heard.</p> -<p>Setting about the business of camp, I -wonder about those animals that watched -me for a while, then moved off, having -seen a tent go up before. With the appearance -of the moon the wind increases and -they test the air more often now. Do they -have visions of cougar or grizzly with every -snap the wind delivers?</p> -<p>In summer these high meadows see a -surprising variety of animal life. Briefly -out of hibernation are marmots and the -handsome golden-mantled ground squirrels. -Mice, voles, shrews, and woodrats run -among the shadows, feeding on the season’s -feast of seeds and insects. A nightmare -for these are the fierce little weasels that -haunt the rocks.</p> -<p>Tracks of cougar and wolverine are -sometimes seen, often teasingly fresh; to -glimpse either of these elusive predators is -to taste the finest wine of wilderness.</p> -<p>Before the berry season, grizzlies grub -the meadows for the tasty bulbs of glacier -lilies and the tubers of spring beauty; often -distracted by the scent of a ground squirrel -in its burrow, they sometimes make a huge -excavation for a small reward.</p> -<p>White-crowned sparrows sing in July -from the low tops of the battered trees, -though their nests are on the ground below. -Grey-crowned rosy finches patrol the drier -ground for seeds while water pipits hunt -insects in the wet areas. High above, a -golden eagle scans the basin again, circling -slowly before following a ridge south to -sight another likely slope in its 10,000-hectare -territory.</p> -<p>The moon shines through the tent top. -The wind, blowing more violently now, -shivers the nylon and interrupts the voice of -the waterfall. I have followed the pasqueflower -run from the April prairies here to -its highest bloom near treeline. I think about -the triangular seed pods of the glacier lilies, -colonies of steep-throated blue gentians, and -the season’s last glory of goldenrod. Indian -paintbrush, from white to fire red, blazes the -slopes that light the fringes of sleep.</p> -<p>I awake to a determined rain, the moon -gone and the tent shuddering with wind-blast. -I try not to think of the steel-cold air, -and slip into a fitful sleep that seems an -endless treadmill of rocky trail.</p> -<p>Stiff and unrefreshed, I look out into -the dawnless morning. The tip of Thunderbird -is detached from its base by grey clouds -swirling at its throat. A wave of sleet slants -down, dancing on the rocks, chanting triumph -<span class="pb" id="Page_109">109</span> -over the buried, bent, and broken -flowers of yesterday.</p> -<p>So I must make my escape, short of -Boulder Pass. Unattainable now, invisible -above the cirque, that high pass grows in -my memory. This testament to what a -glacier can do, to the struggle of trees and -the life-pioneers that invade such harsh -places, is at my feet but shrouded with -snow. My hands grow stiff and numb in the -blunt work of packing up.</p> -<p>I had wished to see Kinnerly Peak again, -rising from the western Kintla valley, -and walk along black ledges of the lava that -floors the pass. Beyond it grows a grove of -subalpine larch, stately, seldom encountered, -the least common tree species in Glacier. -Confined to this narrow zone between forest -and alpine, it reaches up tall and proud, -impervious to the gruelling climate that -makes cowering shrubs of other trees.</p> -<p>But all must wait another year, for this -season comes down hard. And the will of -winter is to erase whatever summer had -devised.</p> -<h3 id="c10">Tundra</h3> -<p>Porcelain-cold, the November sun dawns -in the southeast sky. The ledges, ice-encrusted, -layered with sleet from a recent -squall, whistle the cold morning wind aside. -Rattling down, a slide of rock plunges off the -final ledge, seconds passing before the hollow -sounds of impact clatter back. Like an -apparition of winter itself, white beard bent -sideways by the wind, a mountain goat -steps to the precipice edge. Looking out -across the vast white void, its long belly -hair and pantaloons streaming with the -ceaseless wind, this strange animal, product -of some unfathomable ingenuity, hesitates -but a moment; dropping down from step to -invisible step along the sheer rock face, -fracturing the ice glaze as it goes, it turns a -wall and disappears. A nimble, eight-months-old -kid follows.</p> -<p>Blinking and twisting in the dull light, -the shower of shattered ice clinks softly -downward against rock, fading away like -the short summers of this place.</p> -<p>But while the wind chants winter, -life has made a passage here, and also -waits, hidden in seed and root and den.</p> -<p class="tb">■<br />The nanny and her kid have bedded down -now, looking across the deep, snowy basin -below. Their ledge shines with the first spear -of sunlight.</p> -<p>Far below the pass that connects Mount -<span class="pb" id="Page_110">110</span> -Siyeh to the snow-giants Matahpi and Going-to-the-sun, -three male white-tailed ptarmigan -emerge from their night’s huddle -within a snowbank and step out to peck at -an exposed mat of willow. Ptarmigan, the -only birds on the winter tundra, wear white -plumage in this season, helping to camouflage -them in the snow, just as their mottled -brown summer plumage makes them difficult -to detect among bare rocks. There are -few predators here to hunt them now, but -they move with habitual slowness; quick -movement can be fatal when summer brings -numerous eyes to scan the slopes. With legs -and feet heavily feathered and sharp claws -to scratch for food beneath the snow, the -ptarmigan live at truce with winter. When -blizzards rage between the peaks, they nestle -together in snow dens, beyond the reach of -the winds. Ptarmigan hens winter lower in -taller willow thickets, but the males prefer -to take their winter as high as possible.</p> -<p>Now they crouch behind the wind-deflecting -rocks, dozing in the meager warmth -of the morning sun.</p> -<p>Near the snowless summit crags, a flash -of brown fur zigzags among the rocks. That -would be a pika. Only for a moment does -it show itself, so quickly does it move.</p> -<p>Also called the rock rabbit, the diminutive -pika belongs to the order of hares and -rabbits. Resembling a small guinea pig, this -sturdy creature spurns hibernation as a way -to beat the challenge of winter. Instead, it -spends the summer laying in a store of hay -for the lean season, spreading cut grass to -cure upon the rocks and tending its “haystacks,” -on which its survival hangs.</p> -<p>Winter is a great peril to small mammals. -Their small bodies, because of a large -surface area in relation to volume, retain -heat poorly, and their high metabolic fires -consume calories quickly. Great amounts of -energy are required to sustain an active -animal in rough terrain, placing further -demands on the animal’s capacity to survive -the cold. The pika may need to stack -as much as 25 kilos of hay; to keep its -furnace burning during winter it will have -to fuel its stomach almost hourly.</p> -<p>Small animals of cold climates often -show distinctive body adaptations. On the -pika the small, rounded ears lie flat along -the head, the tail is inconspicuous, the legs -are short; heat loss from exposed surfaces -is thus reduced. Fur insulates the soles of -the pika’s feet while at the same time providing -good traction on steep rock faces.</p> -<p>Hidden below these rocks are the hibernating -marmots and the sleeping ground -squirrels. Beneath the snow the mice, -shrews, and pocket gophers struggle on with -their lives. But above ground, directly confronting -this arctic climate, are the pika, -the ptarmigan, and the mountain goat.</p> -<p>A triumph of adaptation, the mountain -goat faces the winter day without benefit of -either the pika’s den or the ptarmigan’s snow -roost.</p> -<p>The nanny and kid descend from their -<span class="pb" id="Page_111">111</span> -ledge to search out browse at treeline with -other members of a loose band—yearlings, -young males, other nannies with kids. At -the fringes of the band a solitary adult billy -only grudgingly associates with other members -of his kind; for this is the season of rut.</p> -<p>Not really goats at all, these relatives of -the European mountaineering chamois are -insulated from the wind by coats of long, -hollow-haired fur overlying woolly underfur. -They are stocky, stiff-legged, and deliberate, -able to negotiate the walls and pinnacles -with their superbly adapted hoofs. The -unique design of these hoofs gives the animal -great traction and stability on precarious -crags. Opening towards the front, the -cleft between the two hoofs spreads each -outward as the animal descends a slope, -helping to grip the rocky surface. In addition, -the large, rough, and pliant sole of -each foot conforms to the bare rock, increasing -traction.</p> -<p>There is little need for the goat to leave -its steep sanctuaries; it can subsist on -lichens and mosses if browse is not available. -It depends on the inaccessibility of the -cliffs for its security. Accidents, avalanches, -and rockfall are greater enemies than predators. -Golden eagles sometimes attempt to -knock newborn kids from ledges and a -young goat quickly retreats under its nanny -when an eagle soars by. With the protection -of sharp spike horns and a terrifying terrain, -adult goats seldom fall victim to cougar -or grizzly.</p> -<p>It will be a long time before the snow -releases this land and wapiti, bighorn, -grizzly, and cougar wander back into these -high basins. In this winter minimum of life, -the spring songs of rosy finches, water pipits -and white-crowned sparrows seem an impossible -extravagance.</p> -<p class="tb">■<br />I am drawn to the spring tundra—to the -vigor and tenacity of its sparse life—where -survival itself seems ceremony enough. But -it is a strange world, where a man is out of -perspective. Here the plant cover is carpet-high, -and distance, for the lack of trees, -tricks the eye. Here the wind, snow, and sun -quickly burn skin, and the intense light, -reflected from snowbanks, stabs at the eyes. -Almost instantly, a sandwich is sucked dry -of its moisture. The desiccating wind probes -the ears until it seems at last to pierce your -brain. Except for fearful mountain walls the -only shadow is your own. Animals seem -somehow remote and unknowable, as if seen -through glass. A day on the tundra and you -feel the want of a company of trees.</p> -<p>Yet once exposed, you acquire a craving -for the look of tundra. Nowhere else is -there such an impatience for spring—the -flowers rush into bloom; the male water -pipit soars, its skylark song crystal sharp in -the thin air. The nesting birds are restless, -for sun-days and warm days are few, precious, -and quickly spent. Insects and spiders -abound—flying about the peaks or crawling -<span class="pb" id="Page_112">112</span> -among the rocks.</p> -<p>Summer brings bands of bighorn rams -up from the valley to explore the highest -meadows. Though not so sure-footed as the -goats, they too have hoofs adapted to climbing -steep faces, and they walk the slopes -not far below the goats.</p> -<p>Marmots, which whistle sharply when -threatened, spend their days sunbathing and -grazing; they must fill out their now loose-hanging -fur coats with life-sustaining fat for -the coming winter.</p> -<p>Alpine animals are blessed with mobility -and can choose their weathers, retreating -to burrow, den, or rock-harbor to escape the -worst fury of storms. But what about the -plants, rooted forever in one spot, assaulted -by an untempered sun and a drying wind, -and facing the almost daily threat of freeze -and storm?</p> -<p>Alpine plants, through their design and -growing habits, have adapted themselves to -the rigorous demands of this climate in -many ways. Most plants are perennial: there -just aren’t enough days or nutrients available -for the growing of entire plants each year -from seed. And they have the ability to -grow and carry on photosynthesis at temperatures -just above freezing, thus extending -their season. In this zone, temperatures are -rarely above 15° C; the mean summer temperature -is about 10° C. But a flower such -as the alpine buttercup, which is found at -treeline or above, can grow through several -centimeters of snow; heat given off during -the plant’s respiration will create an opening -through which it can emerge.</p> -<p>Plants have various adaptations to meet -the demands of the alpine environment. -Yellow stonecrop, not restricted to this zone, -is nevertheless able to survive here because -of its fleshy succulence and a waxy covering -that prevents water loss. On some plants, -protective hairs covering leaves and stems -help retard the burning effects of wind and -sun. Often this pubescent foliage looks more -grey than green, for the soft hairs mute the -color.</p> -<p>Cushion growth is another alpine adaptation. -The moss campion cushion, covered -with delicate pink flowers, grows to about -one-third of a meter across and only 3 -to 5 centimeters high. Spreading out close -to the ground, the plant avoids the major -violence of the wind and hoards moisture -like a sponge.</p> -<p>The dryad, growing abundantly on the -windy sweep of Siyeh Pass, shows alpine -adaptations in several ways. The energy of -the mature plant is channeled primarily into -reproduction: its large flower, supported by -a short stem, matures quickly; and it produces -many seeds, ensuring germination of a -few. An evergreen, it begins to synthesize -water and carbon dioxide into food as soon -as the snow is gone; and its rolled leaves prevent -rapid evaporation. It grows as a low and -woody mat that year by year extends itself -through the production of new shoots that -carpet the rock. Mat growth has the advantage -<span class="pb" id="Page_113">113</span> -of retaining dead plant material and -capturing wind-blown grains of soil, allowing -the plant slowly to enlarge its soil base.</p> -<p>Compared to the forest, the heartbeat -of the tundra is painfully slow. Here a plant -may grow for a quarter of a century before -it has acquired the reserves necessary for -flowering. Contrasted with the progress on -the tundra, forest succession races by with -dizzying speed. Yet imperceptible as the -change may be the alpine plant community -also passes from pioneer to climax.</p> -<p>Beyond the limit of other plants, lichens -thrive, encrusting rocks with their rainbow -colors. A lichen is actually a primitive and -highly successful association between a -fungus and an alga, working together for -mutual benefit. The fungus protects the -delicate alga, trapping and holding moisture; -the green alga, in turn, produces enough -food to sustain the needs of the fungus.</p> -<p>Generating rock-disintegrating acids -that help secure this partnership to the rock, -lichens, along with physical weathering, -help break down the rocks into soil particles. -Collected in pockets by run-off or -wind, rudimentary soil is slowly invaded by -cushion plants. After centuries of colonization -by these, while the meager soil is deepened -and enriched and moisture retention is -increased, other plants move in, climaxing -at last in hardy grasses and sedges. As in the -forest, pioneer species change the environment -to their detriment, creating a habitat -better suited to other species.</p> -<p>Although it will progress with geologic -slowness, the rocky ground of Siyeh Pass—its -plant cover presently scant and wind-rowed -by frost-heave and relentless wind—will -in time develop grasses and sedges, the -climax vegetation of the alpine meadows.</p> -<p class="tb">■<br />Simplicity rules the alpine zone. Here life is -reduced to bare essentials. Chief controlling -force is climate; but the plants and animals -that live here are well adapted. Compared -to the lower realms, where both -competition and predation are fierce, life -here looks secure.</p> -<p>There is a penalty to simplicity. In the -lowland, the long food chains and diversity -of species, the long growing season, and the -abundant food supply give the forest an -adjustment mechanism and healing power -not found on the critically balanced tundra. -The greater the variety in a plant and animal -community, the greater the stability. So -in the alpine world there exists a paradox: the -most durable life forms constitute the most -fragile community.</p> -<div class="pb" id="Page_114">114</div> -<h3 id="c11">The Water Communities</h3> -<p>Snowfields begin again their summer-long -melt. The alpine stream, vocal again, collects -its water from a thousand places. Miniature -gorges drain the meadow, gurgling -with the sparkle and rush of meltwater in -the lengthening spring days.</p> -<p>Gathering volume, the stream seems to -hurry faster; at the first rock staircase, it -begins to sing. I follow the gully downward, -drawn like the water. There is excitement -in the growing dash and roar, a wind-gust -sweeping spray into the air. A rainbow appears, -holding steady to the swirling cloud -of spray, then doubles and abruptly disappears.</p> -<p>At the first great plunge the water -lunges outward over the lip. Like glass at -shattering, long shards lance out. But the -wind feathers the sharp edges as they fall.</p> -<p>The close thunder of a waterfall beats -at your head, and your mind must shout to -think. Here is water, a most amazing and -most important substance. Perhaps some -of this same water was once part of the -ancient sea in which was laid down the mudstone -of this ledge; was once drunk by -dinosaurs; has coursed the globe countless -times; and has flowed in this very stream -before. In solid, liquid, or gaseous form, -it goes through its own cycle. Together with -sunlight, water makes possible and maintains -all life on Earth.</p> -<h4>Ouzel Music</h4> -<p>A glacier might cling to a winter snow a -hundred years and turn it to ice, a blue -tool to rasp and pluck at rocks, before -letting it go. Lingering summer snowfields -might delay its passage for a time. But the -water always wins at last, becoming, in one -decisive instant, liquid again, and beginning -its long journey to the sea. Plants and dry -air will intercept some of its molecules, sending -them back into the atmosphere to bloom -as fog and cloud; but as rain, snow, or dew, -these are soon commissioned to the land -again.</p> -<p>Water is so familiar to us that we -seldom think about it. We know that fish -swim in the lower lakes, and we are vaguely -aware of the bewildering assortment of life-forms -abounding in a pond. But life begins -in the streams.</p> -<p>Even cups of cold meltwaters, scooped -out of a rivulet only a few meters away from -its snowbank source, contain some life. -Snow algae, which grow on the snowbank -surface, often sufficiently dense to give the -snow a distinctive red complexion, are released -into the meltwater. In summer, small -invertebrate life can be discovered in the -standing pools of even the highest cirque.</p> -<p>But conditions are not good for the -development of complete aquatic food -chains in the streams and lakes of higher -elevations. Alpine lakes, or tarns, support -little visible life. Often flanked by high -ridges and peaks, many tarns receive scant -<span class="pb" id="Page_115">115</span> -direct sunlight during the day. Since these -lakes occupy basins that capture tremendous -amounts of snowfall, the snowbanks persist -in the mountain shadows, and summer -makes little progress in warming the water. -Iceberg Lake, for example, is seldom free -of floating ice, and its temperature never -rises above 4° C in summer, even at the -surface.</p> -<p>Moving out of the cirque lakes, water is -soon churning again, dashing downward -many hundreds of meters to the valleys -below, in rapids, cascades, and breathless -waterfalls. Not surprisingly, few plants and -animals are adapted to life in fast-moving -water.</p> -<p>Algae can be found covering streambed -rocks and stranded, water-polished tree -trunks. Securely attached by holdfasts, these -small plant forms survive the rigorous -stream flow that would destroy the larger -vascular plants. Several species exist, from -microscopic forms to branched filamentous -algae whose long hairlike strands wave in -the current.</p> -<p>A surprising number of insects live on -the stream bottom, finding a measure of -protection from the current in the jumble -of rocks. Underwater beetles live under the -gravel or among the debris at the stream-edge, -or cling to stones and sticks. Scurrying -and creeping among the rock-crannies -are the larvae of stoneflies, mayflies, and -caddisflies. These and the small fish that -venture up from lower lakes are the food -of the water ouzel, a creature that loves the -places where the waters thunder.</p> -<p class="tb">■<br />The noise of the water is overpowering. A -slip into this boiling rage would mean quick -death. Looking 10 meters across the dim, -mist-slippery, water-scoured canyon, I see a -young water ouzel peering out of its unique -nest, on the lookout for its parents. Clouds -of spray keep the nest of living moss continually -wet; but this bird is waterproofed -with an oily plumage and keeps its vigil -at the nest opening. Peering into the torrent -below, then upstream and downstream, it -awaits patiently the delivery of the next -meal.</p> -<p>With the approach of one of the adults, -three other heads crowd the opening, begging -yellow mouths agape. Flying low, the -ouzel parent zeros through the heavy spray, -alighting on a slippery boulder below the -nest ledge. Preparing to fly up to the nest -with its load of insect larvae, the ouzel -spots me across the water. At its sharp -<i>jigic, jigic</i> alarm, the bills of the young -snap instantly shut. Nervously the bird regards -my close presence, dipping its entire -body rapidly up and down, as if keeping -time with the surging torrent.</p> -<p>Discovering no danger, the dusky blue-grey -bird bobs more slowly. The other adult, -returning from an upstream forage, alights -on the same rock, occasioning a new outcry -from the fledglings. Each in turn, the parent -<span class="pb" id="Page_116">116</span> -birds fly up to feed their young, beating -their wings to maintain their position at the -perchless nest. Not pausing to regard me -further, they split the stream between them -again, one flying upstream and one down, to -continue the hunt. Blinking and shaking -the collected mist from its bill, the single -young sentry renews its watch.</p> -<h4>In Shallow Waters</h4> -<p>Life abounds in the shallow lakes and ponds. -Calm, protected John’s Lake offers a -fine example of how a complex aquatic -plant-and-animal community can exist in -balance in a confined space. The water -teems with the microscopic algae, protozoans, -and rotifers that sustain the barely -visible zooplankton. Dancing, flitting, hopping, -and swaying through the water, these -zooplankton in turn support the larger -plankton-eating animals.</p> -<p>Dragonflies and damselflies shoot past, -crackling their wings, and perch in the bog -grass. Looking into the shallow water, you -will see a wealth of small animal life. A -spotted frog swims into view, floating to the -surface beside a lily pad so that its eyes -protrude above the water.</p> -<p>The ribbonlike form of a leech swims -across the bottom toward deeper water. -Looking closer, you see that the water -swarms with bizarre shapes—water boatmen -propelling themselves with oarlike -appendages, a gliding mayfly nymph, then -a predacious diving beetle surfacing, grasping -a bubble of air beneath its shiny brown -wing plates and disappearing downward -again—the bubble’s edge shining silver—into -the brown bottom debris. Suddenly a -whirligig beetle sets the surface to spinning, -wrinkling the view below.</p> -<p>Everywhere in the water there is animal -life, forms that are attached, free-swimming, -crawling on the bottom, and clinging to or -swimming on the surface film. The gray, -slimy encrustation on a sunken log looks -like a covering of lichen but is really a -freshwater sponge, a colonial animal that -feeds by filtering minute plankton from the -water. Another attached creature is the -barely visible hydra; this twig-shaped predator, -related to marine jellyfish, captures -water fleas and other small animals in its -several poisonous tentacles.</p> -<p>Water beetles, backswimmers, water -boatmen, and many other creatures move -about more or less freely in the water, propelling -themselves along with jerky movements. -Suspended between surface and bottom -are the zooplankton, the tiny water -fleas, cyclops, daphnia, and others, which -feed by filtering minute algae. On the bottom -and below live scavenging worms. -Water striders skate on the surface film.</p> -<p>Along the shore, frogs, salamanders, -garter snakes, and water shrews are hunting. -Dabbling and diving ducks patrol about, -tipping or submerging for the bottom -plants. Moose tracks circle the muddy shore. -<span class="pb" id="Page_117">117</span> -Because it produces vegetation abundantly, -John’s Lake sustains a great diversity of -animal life.</p> -<h4>Beaver Ponds</h4> -<p>Fully 10 percent of all the present meadow -area in the Rocky Mountains is estimated -to have been created by beaver, the only -animal besides man that engineers extensive -changes in the environment to suit its own -needs.</p> -<p>When beavers dam a stream, they set -in motion another form of succession. If -the resulting backwater floods a forest area, -the trees are soon killed, creating a broad -opening in the forest canopy. Water-associated -plants and shrubs quickly invade the -pond and shoreline, creating favorable habitat -for waterfowl, moose, blackbirds, amphibians, -wading birds, warblers, marsh -hawks, and a score of other animals.</p> -<p>After many years the water becomes -shallow, filling in with silt and plant debris. -When the beavers abandon the site, the dam -may rupture for lack of maintenance and -the pond will rapidly drain. Or it may continue -to hold, delaying for several more -years its slow conversion to meadow. Stimulated -by the nutrient-rich mud, the water -grasses, sedges, and shrubs finally choke the -water with their accumulating debris, transforming -the area into a bog.</p> -<p>Gradually the ground firms as more -humus is created and more silt is trapped. -The area becomes meadow, supporting -grasses, sedges, and other flowering plants. -Trees begin to reinvade the drier ground, -and eventually the meadow reverts to -forest. Centuries may be required to see -this cycle through, from forest to pond, to -bog, to meadow, to forest again. At each -stage many of the animal inhabitants -change: the song of the western robin and -the chatter of a red squirrel in the original, -pre-beaver forest give way to the croak -of a heron; the heron is replaced by the -insect-and-berry-eating cedar waxwing; the -waxwing is followed by the tree-dwelling -western robin and red squirrel.</p> -<h4>Lakes Cold and Deep</h4> -<p>Seeming to skate on its own reflection, a -spotted sandpiper comes in low over the -quiet water, wingtips almost touching the -surface of the lake. It alights at the shore -and folds its wings. Amid the rounded -rocks, this plain but elegant little shorebird -is all but swallowed up. Teetering constantly -on long legs, it sets off along the water’s -edge, pecking here and there, coming -closer and closer, never forgetting to stop -and curtsy, as if acknowledging, while -hurrying offstage, the applause of an -audience.</p> -<p>As it draws near, several water striders -skate away from the shore. A stonefly, -scuttling between two rocks, is deftly -speared. So large a morsel makes the bird -<span class="pb" id="Page_118">118</span> -pause and rough its feathers, then scamper -into the water to take a drink. Teetering -again, it passes in front of me and continues -down the shore, where I soon lose sight of -it rounding a rocky point.</p> -<p>I am sitting at the foot of Lake McDonald, -watching the darkness gather over -the valley, seeing the last light slide upward -to the tips of the distant mountains. As -daylight dissolves, this long fleet of familiar -peaks seems almost to glide toward darkness, -slow and silent as sailing ships.</p> -<p>The sheet of motionless water stretches -many kilometers away between tree-covered -moraines. The water is deep and cold. No -emergent plants line the barren shore. It -would seem that no life, except for the -single gull that rests on the water far away, -exists in this nearly thousand-meter-high -lake.</p> -<p class="tb">■<br />Considering the great volume of Glacier’s -large, deep lakes, the life they support is -indeed meager. A large part of the reason -lies with the nature of their shores, where -almost no plants grow. A combination of -factors prevents the development of a lush -shoreline growth.</p> -<p>Contoured like bathtubs, these steep-sided -lakes exhibit narrow or non-existent -shoreline shallows, which are vital for the -production of rooted plants. Strong wave -action and extensive seasonal fluctuations in -the level of these natural reservoirs prevent -the development of emergent water plants -in locations where they might otherwise -be expected.</p> -<p>Since sunlight cannot penetrate to the -bottom of these deep lakes, they are deprived -of bottom-anchored plants in midlake -as well. As a result, herbivorous animal life -must depend almost wholly on algal growth. -Wave action inhibits the spread of free-floating -algae by washing much of it onto -the shore. Deep lakes are also low in available -oxygen, preventing the development of -bottom decomposers, which would rapidly -release nutrients as they break down the -accumulating debris washed into the lake. -Without a steady supply of nutrients, plant -growth is retarded.</p> -<p>Since the food chain depends upon -green plants, the ability of a lake to support -higher animals such as fish depends upon its -ability first to produce adequate plant -growth. The production of one kilo of trout -requires that a lake produce about 1,000 -kilos of plants to support 100 kilos of -herbivorous invertebrates, which are eaten -by 10 kilos of carnivorous insects, on which -the trout feed.</p> -<p>Compared to smaller shallow lakes, -which teem with visible life, cold, deep, -nutrient-poor lakes such as McDonald appear -to be watery deserts. Yet because of -their great volume—Lake McDonald contains -5 or 6 cubic kilometers of water—these -large lakes do sustain significant numbers -of fish. Of the 22 kinds of fishes found -<span class="pb" id="Page_119">119</span> -within the park, most are coldwater species. -Trout, whitefish, grayling, suckers, minnows, -and carp fill the roles of herbivore, carnivore, -and scavenger. Agile, highly mobile, and -acutely sensitive, fish represent the most -successful total adaptation to the aquatic environment.</p> -<p>Through the stocking of nonnative -species, including plantings in formerly fish-free -lakes, the natural aquatic communities -of many of Glacier’s lakes and streams have -been permanently modified.</p> -<p>Aquatic food chains are not confined -to the water. Ospreys, ducks, mergansers, -otter, mink, and many other semi-aquatic -or terrestrial birds and mammals utilize the -plants and animals of the water. In fall, a -remarkable spectacle occurs along the outlet -of Lake McDonald. Attracted to the kokanee -salmon concentrations, which run -from Flathead Lake to spawn and die in -these clear, shallow waters, bald eagles -collect to exploit the vulnerable fish. In -1977, 444 eagles were counted in one census. -This food resource is also exploited by -grizzlies, coyotes, skunks, gulls, loons, and -other animals. On occasion, even white-tail -deer have been observed swallowing -salmon!</p> -<div class="pb" id="Page_120">120</div> -<div class="img"> -<img src="images/p043.jpg" alt="Sunset" width="700" height="775" /> -</div> -<div class="pb" id="Page_121">121</div> -<h2 id="c12"><span class="small">Shooting Stars</span></h2> -<div class="pb" id="Page_122">122</div> -<p>This park is very special. The people who -know it well feel proprietary toward its -mountains, scattered lakes, and glaciers. Perhaps -it is the arrangement of the land, an -unsurpassed concentration of American -wilderness. Time and again I have thought, -as I regarded some aspect of this country, -<i>yes, this is exactly right</i>—almost, it would -seem, as if some magic existed that could -translate thought and emotion into rock and -bark.</p> -<p>Glacier remains largely unexploited, -bearing still the aspect of the Earth the -Indians knew for 500 generations—a land -where it is yet possible to feel a sense of -discovery, sense that a single man matters. -On too many mountains, man has tarnished -whatever he has touched; but here the land -has shed, as a fir sloughs snow, a long succession -of traders, trappers, explorers, -hunters, surveyors, prospectors, loggers, -settlers, and tourists.</p> -<p>You may walk the same trail a dozen -times and not tire of the view. I have given -up wondering why. I know only that these -are mountains a man might grow old with, -and that mountain-fever never diminishes -but only changes its look, as a forest does -over many years.</p> -<p>Repeatedly I have noticed that this park -creates an instant bond between strangers. -A certain pause intrudes at the first mention -of Glacier National Park, and a look of -distance comes, as Red Eagle becomes real -again, or the wind at Firebrand is remembered, -or the flowers of Fifty-Mountain -converge once more upon the senses.</p> -<p>Never are we quenched. If a goshawk -rushes past, straining upward with its -squirming load of ground squirrel, forever -afterward our blood demands more. The -sight of a wolverine running is not enough. -Nor the magnificent assemblage of bald -eagles feasting on November salmon. More -days of this: mountain goats leaping impossible -ledges, wave tracks from a beaver -reaching out on dawn water. There are -messages here, loud as kingfishers. The land -has languages, stories to tell.</p> -<p>But in wilderness there is no moral, -save that it must continue. For all our probings -and plottings we discover no adequate -interpretation of the forces we find swirling -about us. A larch you must touch to know; -your neck must feel the ache of too much -looking up. Watch its treepoint pirouette. -Then, looking back at the world level, you -will find that you have lost all answers. We -have learned the art of building bridges, -cataloging plants, predicting what a shrew -might do. Of the essential mystery, we know -nothing.</p> -<p>For nature assigns no “roles” to its -creatures; there is no “reason” for a forest -fire, which burns mightily but with no intent. -Life’s only “purpose” is the feeding of -life, and the beauty we see therein is but -its lack of guarantee: for the chipmunk -and the weasel, and the man who measures -his life to theirs, no assurance of long days -<span class="pb" id="Page_123">123</span> -and tempered seasons, abundant seeds, -ample meat. In wilderness there is mystery -yet, unsimplified, not reduced, resplendent -and immense.</p> -<p>Whatever the conclusion of this planet, -however many the acts to follow in this -consuming drama—mountains coming up, -mountains going down, forests, lakes, and -seas skimming past like wind-driven scud -clouds before a storm—at least in the scant -shadow of this present age there is an -achievement of sorts. For now, with this -creature man, such things as mountains can -be loved. And men have memories to fill.</p> -<p>Tomorrow I will look for shooting -stars—purple spring flowers that point their -fire down, always down toward the center of -the Earth, as if to give in their brief term -beneath the sun a tribute to this most excellent -mystery.</p> -<p>Today I can say nothing more, neck-sore -now from looking at larchtops swaying -with the wind of this splendid morning.</p> -<div class="img" id="fig76"> -<img src="images/p044.jpg" alt="" width="449" height="799" /> -<p class="pcap">Shooting star.</p> -</div> -<div class="pb" id="Page_124">124</div> -<div class="img"> -<img src="images/p045.jpg" alt="Mountain goats." width="645" height="700" /> -</div> -<div class="pb" id="Page_125">125</div> -<h2 id="c13"><span class="small">Appendix</span></h2> -<div class="pb" id="Page_126">126</div> -<h3 id="c14">Mammals of Glacier National Park</h3> -<p>Distribution information was obtained from -<i>Meet the Mammals of Waterton-Glacier International -Peace Park</i>, by Robert C. Gildart -(see Reading List). Nomenclature follows, for -the most part, <i>a Field Guide to Mammals</i>, by -William H. Burt and Richard P. Grossenheider.</p> -<dl class="undent pcap"><dt><b>Key to symbols:</b></dt> -<dt>E—occurs east of Continental Divide (spruce-fir forest; aspen; bunchgrass meadows)</dt> -<dt>W—occurs west of Continental Divide (redcedar-hemlock-lodgepole-fir-larch forest; some meadows)</dt> -<dt>A—occurs in alpine areas (above upper edge of continuous forest)</dt> -<dt>R—rare in Glacier National Park</dt></dl> -<dl class="undent pcap"><dt><b>Shrews</b></dt> -<dt>Masked shrew, <i>Sorex cinereus</i></dt> -<dt>E, W, coniferous forests, meadows, pond and stream edges</dt> -<dt>Vagrant shrew, <i>Sorex vagrans</i></dt> -<dt>E, W, A, moist forests and grasslands, marsh and stream edges</dt> -<dt>Northern water shrew, <i>Sorex palustris</i></dt> -<dt>E, W, stream edges</dt></dl> -<dl class="undent pcap"><dt><b>Bats</b></dt> -<dt>Little brown myotis, <i>Myotis lucifugus</i></dt> -<dt>E, W, coniferous forests, often around buildings, caves; nocturnal</dt> -<dt>Long-eared myotis, <i>Myotis evotis</i></dt> -<dt>E, W, A, R, coniferous forests, meadows; nocturnal</dt> -<dt>Long-legged myotis, <i>Myotis volans</i></dt> -<dt>E, W, A, coniferous forests, meadows; nocturnal</dt> -<dt>Big brown bat, <i>Eptesicus fuscus</i></dt> -<dt>E, W, coniferous forests; often around buildings, caves; nocturnal</dt> -<dt>Silver-haired bat, <i>Lasionycteris noctivagans</i></dt> -<dt>E, W, coniferous forests; meadows; nocturnal</dt> -<dt>Hoary bat, <i>Lasiurus cinereus</i></dt> -<dt>E, W, coniferous forests; mostly nocturnal</dt></dl> -<div class="img" id="fig77"> -<img src="images/p046.jpg" alt="" width="492" height="210" /> -<p class="pcap">Cougar</p> -</div> -<dl class="undent pcap"><dt><b>Cats</b></dt> -<dt>Bobcat, <i>Lynx rufus</i></dt> -<dt>E, open forests, brushy areas</dt> -<dt>Lynx, <i>Lynx canadensis</i></dt> -<dt>E, W, coniferous forests</dt> -<dt>Cougar, <i>Felis concolor</i></dt> -<dt>E, W, coniferous forests</dt></dl> -<dl class="undent pcap"><dt><b>Raccoon, bears</b></dt> -<dt>Raccoon, <i>Procyon lotor</i></dt> -<dt>E, W, R, open forests, stream bottoms</dt> -<dt>Black bear, <i>Ursus americanus</i></dt> -<dt>E, W, A, forests, slide areas, alpine meadows</dt> -<dt>Grizzly, <i>Ursus arctos</i></dt> -<dt>E, W, A, forests, slide areas, alpine meadows</dt></dl> -<div class="img" id="fig78"> -<img src="images/p046a.jpg" alt="" width="278" height="166" /> -<p class="pcap">Coyote</p> -</div> -<dl class="undent pcap"><dt><b>Canines</b></dt> -<dt>Red Fox, <i>Vulpes vulpes</i></dt> -<dt>E, grasslands, open forest</dt> -<dt>Coyote, <i>Canis latrans</i></dt> -<dt>E, W, A, forests, grasslands</dt> -<dt>Gray wolf, <i>Canis lupus</i></dt> -<dt>E, W, R, coniferous forests</dt></dl> -<div class="img" id="fig79"> -<img src="images/p046b.jpg" alt="" width="454" height="205" /> -<p class="pcap">Wolverine</p> -</div> -<div class="img" id="fig80"> -<img src="images/p046c.jpg" alt="" width="389" height="219" /> -<p class="pcap">Longtail weasel</p> -</div> -<dl class="undent pcap"><dt><b>Mustelids</b></dt> -<dt>Striped skunk, <i>Mephitis mephitis</i></dt> -<dt>E, W, open forests, grasslands</dt> -<dt>Badger, <i>Taxidea taxus</i></dt> -<dt>E, W, grasslands</dt> -<dt>River otter, <i>Lutra canadensis</i></dt> -<dt>E, W, R, rivers, lakes</dt> -<dt>Wolverine, <i>Gulo gulo</i></dt> -<dt>E, W, A, coniferous forests, alpine meadows</dt> -<dt>Least weasel, <i>Mustela rixosa</i></dt> -<dt>E, R, open forests, grasslands</dt> -<dt>Shorttail weasel, <i>Mustela erminea</i></dt> -<dt>E, W, A, coniferous forests, meadows</dt> -<dt>Longtail weasel, <i>Mustela frenata</i></dt> -<dt>E, W, A, open forests, meadows</dt> -<dt>Mink, <i>Mustela vison</i></dt> -<dt>E, W, creek and lake edges</dt> -<dt>Marten, <i>Martes americana</i></dt> -<dt>E, W, A, coniferous forests</dt> -<dt>Fisher, <i>Martes pennanti</i></dt> -<dt>E, W, R, coniferous forests</dt></dl> -<div class="pb" id="Page_127">127</div> -<dl class="undent pcap"><dt><b>Lagomorphs</b></dt> -<dt>Pika, <i>Ochotona princeps</i></dt> -<dt>E, W, A, rockslides</dt> -<dt>Snowshoe hare, <i>Lepus americanus</i></dt> -<dt>E, W, coniferous forests</dt> -<dt>Whitetail jackrabbit, <i>Lepus townsendii</i></dt> -<dt>E, W, R, grasslands</dt></dl> -<dl class="undent pcap"><dt><b>Squirrels</b></dt> -<dt>Hoary marmot, <i>Marmota caligata</i></dt> -<dt>E, W, A, rocky areas, alpine meadows</dt> -<dt>Richardson ground squirrel, <i>Spermophilus richardsonii</i></dt> -<dt>E, R, grasslands</dt> -<dt>Columbian ground squirrel, <i>Citellus columbianus</i></dt> -<dt>E, W, A, open woodlands, grasslands, alpine meadows</dt> -<dt>Thirteen-lined ground squirrel, <i>Spermophilus tridecemlineatus</i></dt> -<dt>E, R, grasslands</dt> -<dt>Golden-mantled squirrel, <i>Spermophilus lateralis</i></dt> -<dt>E, W, A, high, open forests; rocky areas</dt> -<dt>Least chipmunk, <i>Eutamias minimus</i></dt> -<dt>E, W, A, high, open forests; brushy, rocky areas; alpine meadows</dt> -<dt>Yellow pine chipmunk, <i>Eutamias amoenus</i></dt> -<dt>E, W, open forests; brushy, rocky areas</dt> -<dt>Redtail chipmunk, <i>Eutamias ruficaudus</i></dt> -<dt>E, W, open forests; brushy, rocky areas</dt> -<dt>Red squirrel, <i>Tamiasciurus hudsonicus</i></dt> -<dt>E, W, coniferous forests</dt> -<dt>Northern flying squirrel, <i>Glaucomys sabrinus</i></dt> -<dt>E, W, coniferous forests; nocturnal</dt></dl> -<dl class="undent pcap"><dt><b>Pocket gophers</b></dt> -<dt>Northern pocket gopher, <i>Thomomys talpoides</i></dt> -<dt>E, W, A, meadows</dt></dl> -<div class="img" id="fig81"> -<img src="images/p046f.jpg" alt="" width="341" height="151" /> -<p class="pcap">Beaver</p> -</div> -<dl class="undent pcap"><dt><b>Beaver</b></dt> -<dt>Beaver, <i>Castor canadensis</i></dt> -<dt>E, W, streams, lakes</dt></dl> -<dl class="undent pcap"><dt><b>Voles and kin</b></dt> -<dt>Deer mouse, <i>Peromyscus maniculatus</i></dt> -<dt>E, W, A, forests, grasslands, alpine meadows</dt> -<dt>Bushytail woodrat, <i>Neotoma cinerea</i></dt> -<dt>E, W, A, rocky areas, old buildings</dt> -<dt>Northern bog lemming, <i>Synaptomys borealis</i></dt> -<dt>W, R, coniferous forests</dt> -<dt>Mountain phenacomys, <i>Phenacomys intermedius</i></dt> -<dt>E, W, A, coniferous forests, alpine meadows</dt> -<dt>Boreal redback vole, <i>Clethrionomys gapperi</i></dt> -<dt>E, W, coniferous forests</dt> -<dt>Meadow vole, <i>Microtus pennsylvanicus</i></dt> -<dt>E, W, open forests, meadows; along streams; marshy areas</dt> -<dt>Longtail vole, <i>Microtus longicaudus</i></dt> -<dt>E, W, coniferous forests, grasslands</dt> -<dt>Water vole, <i>Arvicola richardsoni</i></dt> -<dt>E, W, A, high-elevation stream and lake edges</dt> -<dt>Muskrat, <i>Ondatra zibethica</i></dt> -<dt>W, streams, lakes, marshy areas</dt> -<dt>Western jumping mouse, <i>Zapus princeps</i></dt> -<dt>E, W, A, grasslands, alpine meadows</dt></dl> -<div class="pb" id="Page_128">128</div> -<dl class="undent pcap"><dt><b>Deer</b></dt> -<dt>Wapiti (American elk), <i>Cervus canadensis</i></dt> -<dt>E, W, A, open forests, meadows</dt> -<dt>Mule deer, <i>Odocoileus hemionus</i></dt> -<dt>E, W, A, open forests, meadows, often at high elevations</dt> -<dt>Whitetail deer, <i>Odocoileus virginianus</i></dt> -<dt>E, W, coniferous forests, meadows, creek and river bottoms</dt> -<dt>Moose, <i>Alces alces</i></dt> -<dt>E, W, coniferous forests, lakes, slow streams, marshy areas</dt></dl> -<div class="img" id="fig82"> -<img src="images/p047.jpg" alt="" width="242" height="200" /> -<p class="pcap">Mountain goat</p> -</div> -<dl class="undent pcap"><dt><b>Bovids</b></dt> -<dt>Mountain goat, <i>Oreamnos americanus</i></dt> -<dt>E, W, A, high peaks and meadows</dt> -<dt>Bighorn, <i>Ovis canadensis</i></dt> -<dt>E, A, open mountainous areas</dt></dl> -<h3 id="c15">Reptiles and Amphibians of Glacier National Park</h3> -<p>Note: This check list is based upon actual -specimens in the Park and other collections, -according to Dr. Royal Brunson, Montana -State University.</p> -<dl class="undent pcap"><dt><b>Reptiles</b></dt> -<dt>Great Basin Garter Snake, <i>Thamnophis elegans vagrans</i></dt> -<dt>A large garter snake of mountainous areas, usually with large spots.</dt></dl> -<dl class="undent pcap"><dt>Great Plains Red-sided Garter Snake, <i>Thamnophis ordinoides parietalis</i></dt> -<dt>Dorsal stripes varying from yellow to blue or black. Usually found near water.</dt></dl> -<dl class="undent pcap"><dt><b>Hypothetical List:</b></dt> -<dt>Rubber Boa, <i>Charina bottae utahensis</i></dt> -<dt>May occur in rock slides or, possibly, in forested areas, on either side of the Divide.</dt></dl> -<dl class="undent pcap"><dt>Gopher Snake, <i>Pituophis catenifer sayi</i></dt> -<dt>May occur along eastern boundary (Great Plains).</dt></dl> -<dl class="undent pcap"><dt>Yellow-bellied Blue Racer, <i>Coluber constrictor mormon</i></dt> -<dt>May occur on eastern boundary of Park along border of Great Plains.</dt></dl> -<dl class="undent pcap"><dt>Painted Turtle, <i>Chrysemys picta</i></dt> -<dt>May occur in ponds and sluggish waters from Upper Sonoran Zone to Canadian Zone.</dt></dl> -<dl class="undent pcap"><dt>Western Skink, <i>Eumeces skiltonianus</i></dt> -<dt>May occur in Transition Zone along western border of Park.</dt></dl> -<div class="img" id="fig83"> -<img src="images/p047a.jpg" alt="" width="321" height="141" /> -<p class="pcap">Northern Alligator Lizard</p> -</div> -<dl class="undent pcap"><dt>Northern Alligator Lizard, <i>Gerrhonotus coeruleus principis</i></dt> -<dt>May occur in Transition Zone along western border of Park.</dt></dl> -<dl class="undent pcap"><dt><b>Amphibians</b></dt> -<dt>Tiger Salamander, <i>Ambystoma tigrinum melanostrictum</i></dt> -<dt>Ground color either black or bluish-black, with large spots or blotches of yellow.</dt></dl> -<dl class="undent pcap"><dt>Long-toed Salamander, <i>Ambystoma macrodactylum</i></dt> -<dt>Ground color black or dark brown; wide band of yellow extends from back of head to tip of tail.</dt></dl> -<dl class="undent pcap"><dt>Northwestern Toad, <i>Bufo boreas boreas</i></dt> -<dt>Widely distributed over entire Park. (Also known as Columbian, Northern, or Western Toad.)</dt></dl> -<div class="img" id="fig84"> -<img src="images/p047b.jpg" alt="" width="209" height="247" /> -<p class="pcap">Western Spotted Frog</p> -</div> -<dl class="undent pcap"><dt>Western Spotted Frog, <i>Rana pretiosa pretiosa</i></dt> -<dt>Widely distributed over entire Park. (Also known as Western or Pacific Frog.)</dt></dl> -<dl class="undent pcap"><dt>Green Frog, <i>Rana clamitans</i></dt> -<dt>One specimen, from Bowman Lake. (Chicago Natural History Museum)</dt></dl> -<div class="pb" id="Page_129">129</div> -<dl class="undent pcap"><dt>Tailed Frog, <i>Ascaphus truei</i></dt> -<dt>Should be fairly common, although it is not often taken.</dt></dl> -<dl class="undent pcap"><dt>Pacific Tree-toad, <i>Hyla regilla</i></dt> -<dt>Small size and disks on fingers and toes identify this species. Common throughout Park.</dt></dl> -<h3 id="c16">Fishes of Glacier National Park</h3> -<p>Classification and common scientific names -are from: “A List of Common and Scientific -Names of Fishes from the United States and -Canada,” American Fisheries Society -Publication No. 2, 1960.</p> -<dl class="undent pcap"><dt><b>Key to symbols:</b></dt> -<dt>N Species native to at least one major drainage of the Park.</dt> -<dt>I Non-native species, having been introduced into Park waters by man.</dt> -<dt>S A species of sporting qualities and valued for recreational angling.</dt> -<dt>1 Waterton Drainage</dt> -<dt>2 Belly River Drainage</dt> -<dt>3 Swiftcurrent Drainage</dt> -<dt>4 St. Mary Drainage</dt> -<dt>5 Two Medicine Drainage</dt> -<dt>6 Middle Fork Flathead River Drainage (exclusive of McDonald Valley)</dt> -<dt>7 McDonald Valley Drainage</dt> -<dt>8 North Fork Flathead River Drainage</dt></dl> -<div class="img" id="fig85"> -<img src="images/p047c.jpg" alt="" width="331" height="209" /> -<p class="pcap">Lake Trout</p> -</div> -<dl class="undent pcap"><dt><b>Family <i>Salmonidae</i> (trouts, whitefishes, and grayling)</b></dt> -<dt>Lake Whitefish, <i>Coregonus clupeaformis</i> (I) (1, 2, 3, 4, 7)</dt> -<dt>Pygmy Whitefish, <i>Prosopium coulteri</i> (N) (7)</dt> -<dt>Mountain Whitefish, <i>Prosopium williamsoni</i> (N) (S) (1, 2, 3, 4, 5, 6, 7, 8)</dt> -<dt>Kokanee (Sockeye) Salmon, <i>Oncorhyncus nerka</i> (I) (S) (3, 7, 8)</dt> -<dt>Cutthroat Trout, <i>Salmo clarki</i> (N) (S) (1, 2, 3, 4, 5, 6, 7, 8)</dt> -<dt>Rainbow Trout, <i>Salmo gairdneri</i> (I) (S) (1, 2, 3, 4, 5, 7)</dt> -<dt>Brook Trout, <i>Salvelinus fontinalis</i> (I) (S) (1, 2, 3, 4, 5, 6, 7)</dt> -<dt>Dolly Varden, <i>Salvelinus malma</i> (N) (S) (1, 2, 3, 4, 6, 7, 8)</dt> -<dt>Lake Trout, <i>Salvelinus namaycush</i> (N) (S) (1, 2, 4, 5, 7, 8)</dt> -<dt>Arctic Grayling, <i>Thymallus arcticus</i> (I) (S) (2, 8)</dt></dl> -<dl class="undent pcap"><dt><b>Family <i>Esocidae</i> (pikes)</b></dt> -<dt>Northern pike, <i>Esox lucius</i> (N) (S) (1, 2, 3)</dt></dl> -<div class="img" id="fig86"> -<img src="images/p047d.jpg" alt="" width="217" height="92" /> -<p class="pcap">Redside Shiner</p> -</div> -<dl class="undent pcap"><dt><b>Family <i>Cyprinidae</i> (minnows and carps)</b></dt> -<dt>Longnose Dace, <i>Rhinichthys cataractae</i> (N) (2, 3, 4, 5, 6, 7, 8)</dt> -<dt>Northern Pearl Dace, <i>Margariscus margarita</i> (N) (3, 5)</dt> -<dt>Redside Shiner, <i>Richardsonius balteatus</i> (N) (7, 8)</dt> -<dt>Streamline Chub, <i>Hybopsis dissimilis</i> (N) (1, 3)</dt> -<dt>Northern Squawfish, <i>Ptychocheilus oregonensis</i> (N) (7, 8)</dt></dl> -<div class="img" id="fig87"> -<img src="images/p047e.jpg" alt="" width="375" height="160" /> -<p class="pcap">White Sucker</p> -</div> -<dl class="undent pcap"><dt><b>Family <i>Catostomidae</i> (suckers)</b></dt> -<dt>White Sucker, <i>Catostomus commersoni</i> (N) (1, 2, 3, 4, 5)</dt> -<dt>Largescale Sucker, <i>Catostomus macrocheilus</i> (N) (6, 7, 8)</dt> -<dt>Longnose Sucker, <i>Catostomus catostomus</i> (N) (1, 2, 3, 4, 5, 6, 7, 8)</dt></dl> -<div class="pb" id="Page_130">130</div> -<dl class="undent pcap"><dt><b>Family <i>Gadidaie</i> (codfishes and hakes)</b></dt> -<dt>Burbot, <i>Lota lota</i> (N) (S) (1, 4)</dt></dl> -<dl class="undent pcap"><dt><b>Family <i>Cottidae</i> (sculpins)</b></dt> -<dt>Mottled sculpin, <i>Cottus bairdi</i> (N) (5, 6, 7, 8)</dt> -<dt>Spoonhead sculpin, <i>Cottus ricei</i> (N) (1, 2, 3, 4)</dt></dl> -<h3 id="c17">Birds of Glacier National Park</h3> -<dl class="undent pcap"><dt><b>Key to symbols:</b></dt> -<dt>E—occurs on east side of the park (east of the Divide)</dt> -<dt>W—occurs on west side of the park (west of the Divide)</dt> -<dt>A—occurs in alpine areas</dt> -<dt>ab—abundant</dt> -<dt>c—common</dt> -<dt>u—uncommon</dt> -<dt>r—rare</dt> -<dt>i—introduced</dt> -<dt>a—accidental</dt></dl> -<div class="img" id="fig88"> -<img src="images/p048.jpg" alt="" width="311" height="188" /> -<p class="pcap">Common Loon</p> -</div> -<dl class="undent pcap"><dt><b>Loons</b></dt> -<dt>Common Loon E, W, ab</dt> -<dt>Arctic Loon?</dt> -<dt>Red-throated Loon?</dt></dl> -<div class="img" id="fig89"> -<img src="images/p048a1.jpg" alt="" width="367" height="193" /> -<p class="pcap">Western Grebe</p> -</div> -<dl class="undent pcap"><dt><b>Grebes</b></dt> -<dt>Red-necked Grebe E, W, c</dt> -<dt>Horned Grebe E, W, ab</dt> -<dt>Eared Grebe E, W, c</dt> -<dt>Western Grebe E, W, u</dt> -<dt>Pied-billed Grebe E, W, r</dt></dl> -<dl class="undent pcap"><dt><b>Pelicans, Cormorants</b></dt> -<dt>White Pelican E, W, u</dt> -<dt>Double-crested Cormorant E, r</dt></dl> -<div class="img" id="fig90"> -<img src="images/p048a2.jpg" alt="" width="258" height="333" /> -<p class="pcap">Great Blue Heron</p> -</div> -<div class="img" id="fig91"> -<img src="images/p048b.jpg" alt="" width="202" height="222" /> -<p class="pcap">American Bittern</p> -</div> -<dl class="undent pcap"><dt><b>Herons, Bitterns</b></dt> -<dt>Great Blue Heron E, W, c</dt> -<dt>Black-crowned Night Heron a</dt> -<dt>American Bittern, W, r</dt></dl> -<div class="img" id="fig92"> -<img src="images/p048c.jpg" alt="" width="389" height="291" /> -<p class="pcap">Mallard</p> -</div> -<div class="img" id="fig93"> -<img src="images/p048d.jpg" alt="" width="281" height="239" /> -<p class="pcap">Wood Duck</p> -</div> -<div class="img" id="fig94"> -<img src="images/p048e.jpg" alt="" width="315" height="257" /> -<p class="pcap">Ruddy Duck</p> -</div> -<dl class="undent pcap"><dt><b>Swan, Geese, Ducks</b></dt> -<dt>Whistling Swan E, W, ab</dt> -<dt>Trumpeter Swan E, W, r</dt> -<dt>Canada Goose E, W, c</dt> -<dt>Snow Goose E, W, c</dt> -<dt>Ross’ Goose E, W, r</dt> -<dt>Mallard E, W, ab</dt> -<dt>Gadwall E, W, r</dt> -<dt>Pintail E, W, c</dt> -<dt>Green-winged Teal E, W, c</dt> -<dt>Blue-winged Teal E, W, u</dt> -<dt>Cinnamon Teal E, W, u</dt> -<dt>European Widgeon E, W, c</dt> -<dt>American Widgeon E, W, ab</dt> -<dt>Northern Shoveler E, W, c</dt> -<dt>Wood Duck E, W, r</dt> -<dt>Redhead E, W, c</dt> -<dt>Ring-necked Duck E, W, u</dt> -<dt>Canvasback E, W, u</dt> -<dt>Lesser Scaup E, W, c</dt> -<dt>Greater Scaup?</dt> -<dt>Common Goldeneye E, W, c</dt> -<dt>Barrow’s Goldeneye E, W, ab</dt> -<dt>Bufflehead E, W, u</dt> -<dt>Harlequin Duck E, W, c</dt> -<dt>White-winged Scoter E, W, r</dt> -<dt>Ruddy Duck E, W, c</dt> -<dt>Hooded Merganser E, W, u</dt> -<dt>Common Merganser E, W, ab</dt> -<dt>Red-breasted Merganser, E, W, u</dt></dl> -<div class="img" id="fig95"> -<img src="images/p048f.jpg" alt="" width="246" height="309" /> -<p class="pcap">Cooper’s Hawk</p> -</div> -<div class="img" id="fig96"> -<img src="images/p048g.jpg" alt="" width="507" height="374" /> -<p class="pcap">Marsh Hawk</p> -</div> -<dl class="undent pcap"><dt><b>Vultures, Hawks, Eagles</b></dt> -<dt>Turkey Vulture E, W, r</dt> -<dt>Goshawk E, W, c</dt> -<dt>Sharp-shinned Hawk E, W, u</dt> -<dt>Cooper’s Hawk E, W, u</dt> -<dt>Red-tailed Hawk E, W, c</dt> -<dt>Red-shouldered Hawk a</dt> -<dt>Swainson’s Hawk E, W, c</dt> -<dt>Rough-legged Hawk E, W, r</dt> -<dt>Ferruginous Hawk E, W, u</dt> -<dt>Golden Eagle, E, W, A, c</dt> -<dt>Bald Eagle, E, W, ab</dt> -<dt>Marsh Hawk E, W, ab</dt> -<dt>Osprey E, W, ab</dt> -<dt>Prairie Falcon E, W, A, r</dt> -<dt>Peregrine Falcon E, W, r</dt> -<dt>American Kestrel E, W, c</dt></dl> -<div class="pb" id="Page_131">131</div> -<div class="img" id="fig97"> -<img src="images/p048h.jpg" alt="" width="344" height="341" /> -<p class="pcap">Sharp-tailed Grouse</p> -</div> -<dl class="undent pcap"><dt><b>Grouse, Ptarmigans</b></dt> -<dt>Blue Grouse, E, W, ab</dt> -<dt>Spruce Grouse E, W, ab</dt> -<dt>Ruffed Grouse E, W, ab</dt> -<dt>Sharp-tailed Grouse E, r</dt> -<dt>White-tailed Ptarmigan A, c</dt> -<dt>Willow Ptarmigan ?</dt> -<dt>Ring-necked Pheasant E, W, r, i</dt> -<dt>Gray Partridge E, W, r, i</dt></dl> -<dl class="undent pcap"><dt>Cranes</dt> -<dt>Sandhill Crane E, r</dt></dl> -<div class="img" id="fig98"> -<img src="images/p048i.jpg" alt="" width="248" height="170" /> -<p class="pcap">American Coot</p> -</div> -<dl class="undent pcap"><dt><b>Rails, Coots</b></dt> -<dt>Sora E, W, r</dt> -<dt>American Coot E, W, ab</dt></dl> -<div class="img" id="fig99"> -<img src="images/p048j.jpg" alt="" width="253" height="251" /> -<p class="pcap">Greater Yellowlegs</p> -</div> -<dl class="undent pcap"><dt><b>Shorebirds</b></dt> -<dt>Killdeer E, W, c</dt> -<dt>Black-bellied Plover E, r</dt> -<dt>Common Snipe E, W, c</dt> -<dt>Long-billed Curlew E, r</dt> -<dt>Upland Sandpiper E, r</dt> -<dt>Spotted Sandpiper E, W, A, ab</dt> -<dt>Solitary Sandpiper E, r</dt> -<dt>Willet, E, r</dt> -<dt>Pectoral Sandpiper E, r</dt> -<dt>Baird’s Sandpiper E, W, r</dt> -<dt>Lesser Yellowlegs, E, W r</dt> -<dt>Greater Yellowlegs E, W, r</dt> -<dt>American Avocet E, W, u</dt> -<dt>Northern Phalarope E, W, r</dt> -<dt>Wilson’s Phalarope E, W, u</dt> -<dt>Black Turnstone ?</dt> -<dt>Long-billed Dowitcher E, W, r</dt></dl> -<div class="img" id="fig100"> -<img src="images/p048k.jpg" alt="" width="305" height="391" /> -<p class="pcap">Herring Gull</p> -</div> -<dl class="undent pcap"><dt><b>Gulls, Terns</b></dt> -<dt>Herring Gull E, W, r</dt> -<dt>California Gull E, W, ab</dt> -<dt>Ring-billed Gull E, W, c</dt> -<dt>Franklin’s Gull E, W, c</dt> -<dt>Bonaparte’s Gull E, u</dt> -<dt>Forster’s Tern E, W, u</dt> -<dt>Common Tern E, r</dt> -<dt>Caspian Tern a</dt> -<dt>Black Tern E, W, u</dt></dl> -<div class="img" id="fig101"> -<img src="images/p048l.jpg" alt="" width="336" height="321" /> -<p class="pcap">Mourning Dove</p> -</div> -<dl class="undent pcap"><dt><b>Doves, Pigeons</b></dt> -<dt>Band-tailed Pigeon E, W, r</dt> -<dt>Mourning Dove E, W, c</dt> -<dt>Rock Dove E, W, r, i</dt></dl> -<div class="img" id="fig102"> -<img src="images/p048m.jpg" alt="" width="473" height="254" /> -<p class="pcap">Great Horned Owl</p> -</div> -<dl class="undent pcap"><dt><b>Owls</b></dt> -<dt>Screech Owl E, W, r</dt> -<dt>Great Horned Owl E, W, ab</dt> -<dt>Snowy Owl E, W, u</dt> -<dt>Hawk Owl E, W, u</dt> -<dt>Pygmy Owl E, W, ab</dt> -<dt>Barred Owl E, W, c</dt> -<dt>Great Gray Owl E, W, u</dt> -<dt>Long-eared Owl E, W, r</dt> -<dt>Short-eared Owl, E, W, c</dt> -<dt>Boreal Owl E, W, r</dt> -<dt>Saw-whet Owl E, W, u</dt></dl> -<div class="img" id="fig103"> -<img src="images/p048n.jpg" alt="" width="284" height="313" /> -<p class="pcap">Common Nighthawk</p> -</div> -<dl class="undent pcap"><dt><b>Nighthawks, Swifts</b></dt> -<dt>Common Nighthawk E, W, ab</dt> -<dt>Black Swift E, W, u</dt> -<dt>Vaux’s Swift E, W, ab</dt> -<dt>White-throated Swift W, A, r</dt></dl> -<dl class="undent pcap"><dt><b>Hummingbirds</b></dt> -<dt>Broad-tailed Hummingbird E, W, r</dt> -<dt>Rufous Hummingbird E, W, A, ab</dt> -<dt>Calliope Hummingbird E, W, A, ab</dt> -<dt>Black-chinned Hummingbird E, W, r</dt></dl> -<div class="pb" id="Page_132">132</div> -<div class="img" id="fig104"> -<img src="images/p049.jpg" alt="" width="432" height="328" /> -<p class="pcap">Belted Kingfisher</p> -</div> -<dl class="undent pcap"><dt><b>Kingfishers</b></dt> -<dt>Belted Kingfisher E, W, ab</dt></dl> -<dl class="undent pcap"><dt><b>Woodpeckers</b></dt> -<dt>Common Flicker E, W, ab</dt> -<dt>Pileated Woodpecker E, W, ab</dt> -<dt>Red-headed Woodpecker E, W, r</dt> -<dt>Lewis’ Woodpecker E, W, c</dt> -<dt>Yellow-bellied Sapsucker E, W, ab</dt> -<dt>Williamson’s Sapsucker E, W, u</dt> -<dt>Hairy Woodpecker E, W, ab</dt> -<dt>Downy Woodpecker E, W, ab</dt> -<dt>Black-backed Three-toed Woodpecker E, W, ab</dt> -<dt>Northern Three-toed Woodpecker E, W, ab</dt></dl> -<div class="img" id="fig105"> -<img src="images/p049a.jpg" alt="" width="338" height="327" /> -<p class="pcap">Ash-throated Flycatcher</p> -</div> -<dl class="undent pcap"><dt><b>Flycatchers</b></dt> -<dt>Eastern Kingbird E, W, ab</dt> -<dt>Western Kingbird E, W, u</dt> -<dt>Ash-throated Flycatcher a</dt> -<dt>Say’s Phoebe E, W, r</dt> -<dt>Willow Flycatcher E, W, c</dt> -<dt>Hammond’s Flycatcher E, W, ab</dt> -<dt>Olive-sided Flycatcher E, W, ab</dt> -<dt>Western Flycatcher E, r</dt> -<dt>Western Wood Peewee E, W, c</dt></dl> -<dl class="undent pcap"><dt><b>Larks</b></dt> -<dt>Horned Lark E, W, A, ab</dt></dl> -<div class="img" id="fig106"> -<img src="images/p049b.jpg" alt="" width="410" height="411" /> -<p class="pcap">Barn Swallow</p> -</div> -<dl class="undent pcap"><dt><b>Swallows</b></dt> -<dt>Violet-green Swallow E, W, A, ab</dt> -<dt>Tree Swallow E, W, ab</dt> -<dt>Bank Swallow E, W, ab</dt> -<dt>Rough-winged Swallow E, W, u</dt> -<dt>Barn Swallow E, W, u</dt> -<dt>Cliff Swallow E, W, A, ab</dt></dl> -<div class="img" id="fig107"> -<img src="images/p049c.jpg" alt="" width="513" height="275" /> -<p class="pcap">Common Crow</p> -</div> -<dl class="undent pcap"><dt><b>Jays, Magpies, Crows</b></dt> -<dt>Gray Jay E, W, ab</dt> -<dt>Blue Jay E, W, r</dt> -<dt>Steller’s Jay E, W, ab</dt> -<dt>Black-billed Magpie E, W, ab</dt> -<dt>Common Raven E, W, A, ab</dt> -<dt>Common Crow E, W, ab</dt> -<dt>Clark’s Nutcracker E, W, A, ab</dt></dl> -<dl class="undent pcap"><dt><b>Chickadees</b></dt> -<dt>Black-capped Chickadee E, W, ab</dt> -<dt>Mountain Chickadee E, W, ab</dt> -<dt>Boreal Chickadee E, W, r</dt> -<dt>Chestnut-backed Chickadee E, W, u</dt></dl> -<dl class="undent pcap"><dt><b>Nuthatches, Creepers</b></dt> -<dt>White-breasted Nuthatch E, W, u</dt> -<dt>Red-breasted Nuthatch E, W, ab</dt> -<dt>Brown Creeper E, W, ab</dt></dl> -<div class="img" id="fig108"> -<img src="images/p049d.jpg" alt="" width="241" height="240" /> -<p class="pcap">Winter Wren</p> -</div> -<dl class="undent pcap"><dt><b>Dippers, Wrens</b></dt> -<dt>Dipper E, W, A, ab</dt> -<dt>House Wren E, W, u</dt> -<dt>Winter Wren E, W, ab</dt> -<dt>Long-billed Marsh Wren a</dt> -<dt>Rock Wren E, W, u</dt></dl> -<dl class="undent pcap"><dt><b>Catbirds, Thrashers</b></dt> -<dt>Gray Catbird E, W, u</dt></dl> -<div class="img" id="fig109"> -<img src="images/p049e.jpg" alt="" width="275" height="233" /> -<p class="pcap">Mountain Bluebird</p> -</div> -<dl class="undent pcap"><dt><b>Thrushes, Bluebirds, Solitaires</b></dt> -<dt>American Robin E, W, A, ab</dt> -<dt>Varied Thrush E, W, ab</dt> -<dt>Hermit Thrush E, W, ab</dt> -<dt>Swainson’s Thrush E, W, ab</dt> -<dt>Veery E, W, c</dt> -<dt>Western Bluebird E, W, r</dt> -<dt>Mountain Bluebird E, W, A, ab</dt> -<dt>Townsend’s Solitaire E, W, A, ab</dt></dl> -<dl class="undent pcap"><dt><b>Kinglets</b></dt> -<dt>Golden-crowned Kinglet E, W, ab</dt> -<dt>Ruby-crowned Kinglet E, W, ab</dt></dl> -<div class="pb" id="Page_133">133</div> -<dl class="undent pcap"><dt><b>Pipits</b></dt> -<dt>Water Pipit E, W, A, ab</dt></dl> -<div class="img" id="fig110"> -<img src="images/p049f.jpg" alt="" width="201" height="257" /> -<p class="pcap">Cedar Waxwing</p> -</div> -<dl class="undent pcap"><dt><b>Waxwings</b></dt> -<dt>Bohemian Waxwing E, W, ab</dt> -<dt>Cedar Waxwing E, W, ab</dt></dl> -<dl class="undent pcap"><dt><b>Shrikes</b></dt> -<dt>Loggerhead Shrike E, W, r</dt> -<dt>Northern Shrike E, W, r</dt></dl> -<div class="img" id="fig111"> -<img src="images/p049g.jpg" alt="" width="243" height="210" /> -<p class="pcap">Starling</p> -</div> -<dl class="undent pcap"><dt><b>Starlings</b></dt> -<dt>Starling E, W, c, i</dt></dl> -<div class="img" id="fig112"> -<img src="images/p049h.jpg" alt="" width="373" height="166" /> -<p class="pcap">Red-eyed Vireo</p> -</div> -<dl class="undent pcap"><dt><b>Vireos</b></dt> -<dt>Solitary Vireo E, W, ab</dt> -<dt>Red-eyed Vireo E, W, ab</dt> -<dt>Warbling Vireo E, W, ab</dt></dl> -<dl class="undent pcap"><dt><b>Warblers</b></dt> -<dt>Black and White Warbler W, r</dt> -<dt>Tennessee Warbler E, W, r</dt> -<dt>Orange-crowned Warbler E, W, r</dt> -<dt>Nashville Warbler E, W, r</dt> -<dt>Yellow Warbler E, W, ab</dt> -<dt>Yellow-rumped Warbler E, W, ab</dt> -<dt>Townsend’s Warbler E, W, ab</dt> -<dt>Northern Waterthrush E, W, ab</dt> -<dt>MacGillivray’s Warbler E, W, ab</dt> -<dt>Common Yellowthroat E, W, ab</dt> -<dt>Wilson’s Warbler E, W, ab</dt> -<dt>American Redstart E, W, ab</dt> -<dt>Yellow-breasted Chat ?</dt></dl> -<div class="img" id="fig113"> -<img src="images/p049i.jpg" alt="" width="454" height="250" /> -<p class="pcap">House Sparrow</p> -</div> -<dl class="undent pcap"><dt><b>Weaver Finches</b></dt> -<dt>House Sparrow E, W, r, i</dt></dl> -<dl class="undent pcap"><dt><b>Blackbirds, Orioles</b></dt> -<dt>Bobolink E, r</dt> -<dt>Western Meadowlark E, W, u</dt> -<dt>Red-winged Blackbird E, W, ab</dt> -<dt>Northern Oriole E, W, r</dt> -<dt>Brewer’s Blackbird E, W, u</dt> -<dt>Rusty Blackbird E, W, r</dt> -<dt>Yellow-headed Blackbird E, r</dt> -<dt>Common Grackle E, r</dt> -<dt>Brown-headed Cowbird E, W, c</dt></dl> -<div class="img" id="fig114"> -<img src="images/p049j.jpg" alt="" width="328" height="468" /> -<p class="pcap">Evening Grosbeak</p> -</div> -<dl class="undent pcap"><dt><b>Tanagers, Grosbeaks</b></dt> -<dt>Western Tanager E, W, ab</dt> -<dt>Evening Grosbeak E, W, ab</dt> -<dt>Pine Grosbeak E, W, ab</dt> -<dt>Black-headed Grosbeak E, W, r</dt></dl> -<div class="img" id="fig115"> -<img src="images/p049o.jpg" alt="" width="355" height="298" /> -<p class="pcap">American Goldfinch</p> -</div> -<dl class="undent pcap"><dt><b>Finches, Sparrows, Buntings</b></dt> -<dt>Lazuli Bunting E, W, c</dt> -<dt>Lark Bunting E, W, r</dt> -<dt>Snow Bunting E, W, c</dt> -<dt>Cassin’s Finch E, W, A, ab</dt> -<dt>Gray-crowned Rosy Finch E, W, A, ab</dt> -<dt>American Goldfinch E, W, u</dt> -<dt>Common Redpoll E, W, c</dt> -<dt>Pine Siskin E, W, A, ab</dt> -<dt>Red Crossbill E, W, ab</dt> -<dt>White-winged Crossbill E, W, u</dt> -<dt>Rufous-sided Towhee E, W, u</dt> -<dt>Green-tailed Towhee E, W, r</dt> -<dt>Savannah Sparrow E, W, c</dt> -<dt>LeConte’s Sparrow E, W, u</dt> -<dt>Vesper Sparrow E, W, ab</dt> -<dt>Tree Sparrow E, W, r</dt> -<dt>Chipping Sparrow E, W, A, ab</dt> -<dt>Brewer’s Sparrow E, W, r</dt> -<dt>Harris’ Sparrow E, W, r</dt> -<dt>White-crowned Sparrow E, W, A, ab</dt> -<dt>Fox Sparrow E, W, A, ab</dt> -<dt>Lincoln’s Sparrow E, W, A, c</dt> -<dt>Song Sparrow E, W, ab</dt> -<dt>Dark-eyed Junco E, W, c</dt> -<dt>McCown’s Longspur E, c</dt> -<dt>Lapland Longspur E, W, c</dt> -<dt>Chestnut-collared Longspur E, c</dt></dl> -<div class="pb" id="Page_134">134</div> -<h2 id="c18"><span class="small">Suggested Reading</span></h2> -<p class="book">Alexander, Taylor R. and George S. -Fichter, <i>Ecology</i> (a Golden guide). -Western Publishing Co., Inc., Racine, -Wis. 1973.</p> -<p class="book">Alt, David D. and Donald W. Hyndman, -<i>Rocks, Ice and Water, the Geology of -Waterton-Glacier Park</i>. Mountain Press -Publishing Co., Missoula, Mont. 1973.</p> -<p class="book">Baker, William, et. al., <i>Wildlife of the -Northern Rocky Mountains</i>. Naturegraph -Co., Healdsburg, Calif. 1961.</p> -<p class="book">Borland, Hal, <i>The History of Wildlife -in America</i>. National Wildlife Federation, -Washington, D.C. 1975.</p> -<p class="book">Brooks, Maurice, <i>The Life of The -Mountains</i>. McGraw-Hill, New York. 1967.</p> -<p class="book">Costello, David F., <i>The Mountain World</i>. -Thomas Y. Crowell Co., New York. 1975.</p> -<p class="book">Craighead, John J., et. al., <i>A Field Guide -to Rocky Mountain Wildflowers</i>. -Houghton Mifflin Co., Boston. 1963.</p> -<p class="book">Dobie, J. Frank, <i>The Voice of the Coyote</i>. -Little, Brown and Co., Boston. 1950.</p> -<p class="book">Farb, Peter, <i>Face of North America</i>. -Harper and Row, New York. 1963.</p> -<p class="book">Gildart, Robert C., <i>Meet the Mammals of -Waterton-Glacier</i>. Glacier Natural History -Association, Inc. Thomas Printing, Inc., -Kalispell, Mont. 1975.</p> -<p class="book">McCormick, Jack, <i>The Life of the Forest</i>. -McGraw-Hill, New York. 1966.</p> -<p class="book">Milne, Lorus and Margery Milne, <i>The -Balance of Nature</i>. Alfred A. Knopf, Inc., -New York. 1960.</p> -<p class="book">Nelson, Alan G., <i>Wildflowers of Glacier -National Park</i>. Nelson, Great Falls, -Mont. 1970.</p> -<p class="book">Peattie, Donald Culross, <i>A Natural -History of Western Trees</i>. Bonanza -Books, New York. 1953.</p> -<p class="book">Ruhle, George C., <i>Roads and Trails -of Waterton-Glacier Parks</i>. -John W. Forney, Minneapolis, Minn. 1972.</p> -<p class="book">Shea, David S., <i>Animal Tracks of Glacier -National Park</i>. Special Bulletin No. 11, -Glacier Natural History Association, Inc., -West Glacier, Mont., 1969.</p> -<p class="book">Storer, John H., <i>The Web of Life</i>. -Devin-Adair Co., Old Greenwich, Conn. -1953.</p> -<p class="book">Zwinger, Ann H. and Beatrice E. Willard, -<i>Land Above the Trees</i>. Harper and Row, -New York. 1972.</p> -<div class="pb" id="Page_135">135</div> -<div class="img" id="map1"> -<img src="images/map50_lr.jpg" alt="" width="728" height="800" /> -<p class="pcap">WATERTON LAKES NATIONAL PARK—GLACIER NATIONAL PARK</p><p class="center"><a class="ab1" href="images/map50_hr.jpg">High-resolution Map</a></p> -</div> -<div class="pb" id="Page_136">136</div> -<p class="pcap"><b>Using Metrics</b></p> -<p class="pcapc">As we go to press with this book, the -United States is in the early stages of -conversion to the metric system of -measurement, and though we urge you to -think metric—for most of the world does—we -provide this table to help you -understand the measurements given in -the book.</p> -<table class="center" summary=""> -<tr class="th"><th>To convert from </th><th>to </th><th>multiply by</th></tr> -<tr><td class="l">Millimeters </td><td class="l">Sixteenth-inches </td><td class="l">0.6301</td></tr> -<tr><td class="l">Centimeters </td><td class="l">Inches </td><td class="l">0.3937</td></tr> -<tr><td class="l">Meters </td><td class="l">Feet </td><td class="l">3.2808</td></tr> -<tr><td class="l">Kilometers </td><td class="l">Miles </td><td class="l">0.6214</td></tr> -<tr><td class="l">Hectares </td><td class="l">Acres </td><td class="l">2.4711</td></tr> -<tr><td class="l">Hectares </td><td class="l">Square miles </td><td class="l">0.00386</td></tr> -<tr><td class="l">Grams </td><td class="l">Troy Ounces </td><td class="l">0.0322</td></tr> -<tr><td class="l">Kilograms </td><td class="l">Pounds </td><td class="l">2.2046</td></tr> -<tr><td class="l">Degrees—Celsius </td><td class="l">Degrees—Fahrenheit </td><td class="l">1.8, and add 32</td></tr> -</table> -<div class="img" id="fig116"> -<img src="images/p051.jpg" alt="" width="185" height="599" /> -<p class="pcap">Temperature Conversion Chart</p> -</div> -<div class="img" id="fig117"> -<img src="images/p051a.jpg" alt="" width="800" height="99" /> -<p class="pcap">Length Conversion Chart</p> -</div> -<div class="pb" id="Page_137">137</div> -<p class="pcapc">Drawings from David S. Shea, <i>Animal Tracks of Glacier National Park</i></p> -<div class="img" id="fig118"> -<img src="images/p051b.jpg" alt="" width="324" height="325" /> -<p class="pcap">red fox, -<br />hind foot, in mud -<br />53 mm.</p> -</div> -<div class="img" id="fig119"> -<img src="images/p051c.jpg" alt="" width="430" height="436" /> -<p class="pcap">mule deer, -<br />adult buck, in snow -<br />72 mm.</p> -</div> -<div class="img" id="fig120"> -<img src="images/p051d.jpg" alt="" width="280" height="265" /> -<p class="pcap">badger, -<br />left front foot, in mud -<br />43 mm.</p> -</div> -<div class="img" id="fig121"> -<img src="images/p051e.jpg" alt="" width="351" height="389" /> -<p class="pcap">coyote, -<br />hind foot, in snow -<br />63 mm.</p> -</div> -<div class="pb" id="Page_138">138</div> -<p class="pcap"><b>About the Author</b></p> -<p class="pcapc">Greg Beaumont’s interest in Glacier -National Park dates from 1963, when he -was a summer employee at Lake -McDonald Lodge. In 1966 he and his wife -were fire-control lookouts on Numa Ridge -in the Bowman Valley. Now a free-lance -writer-photographer, he lives with his -family in Lincoln, Nebraska.</p> -<div class="pb" id="Page_139">139</div> -<p class="pcap"><b>National Park Service -<br />U.S. Department of the Interior</b></p> -<p class="pcapc">As the Nation’s principal conservation -agency, the Department of the Interior -has responsibility for most of our -nationally owned public lands and natural -resources. This includes fostering the -wisest use of our land and water -resources, protecting our fish and wildlife, -preserving the environmental and -cultural values of our national parks and -historical places, and providing for the -enjoyment of life through outdoor -recreation. The Department assesses our -energy and mineral resources and works -to assure that their development is in the -best interests of all our people. The -Department also has a major responsibility -for American Indian reservation -communities and for people who live in -Island Territories under U.S. -administration.</p> -<h2>Transcriber’s Notes</h2> -<ul> -<li>Retained publication information from the printed edition: this eBook is public-domain in the country of publication.</li> -<li>Corrected a few palpable typos.</li> -<li>Included a transcription of the text within some images.</li> -<li>In the text versions only, text in italics is delimited by _underscores_.</li> -</ul> - - - - - - - -<pre> - - - - - -End of the Project Gutenberg EBook of Many-Storied Mountains, by Greg Beaumont - -*** END OF THIS PROJECT GUTENBERG EBOOK MANY-STORIED MOUNTAINS *** - -***** This file should be named 55150-h.htm or 55150-h.zip ***** -This and all associated files of various formats will be found in: - http://www.gutenberg.org/5/5/1/5/55150/ - -Produced by Stephen Hutcheson, MFR and the Online -Distributed Proofreading Team at http://www.pgdp.net - -Updated editions will replace the previous one--the old editions will -be renamed. - -Creating the works from print editions not protected by U.S. copyright -law means that no one owns a United States copyright in these works, -so the Foundation (and you!) can copy and distribute it in the United -States without permission and without paying copyright -royalties. 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