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+The Project Gutenberg EBook of Wonders of Creation, by Anonymous
+
+Copyright laws are changing all over the world. Be sure to check the
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+**Welcome To The World of Free Plain Vanilla Electronic Texts**
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+**eBooks Readable By Both Humans and By Computers, Since 1971**
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+*****These eBooks Were Prepared By Thousands of Volunteers!*****
+
+
+Title: Wonders of Creation
+
+Author: Anonymous
+
+Release Date: July, 2004 [EBook #6131]
+[Yes, we are more than one year ahead of schedule]
+[This file was first posted on November 17, 2002]
+
+Edition: 10
+
+Language: English
+
+Character set encoding: Unicode UTF-8
+
+*** START OF THE PROJECT GUTENBERG EBOOK WONDERS OF CREATION ***
+
+
+
+
+Produced by Curtis A. Weyant, Juliet Sutherland, Charles Franks
+and the Online Distributed Proofreading Team.
+
+
+
+
+
+
+[Illustration: Mount Vesuvius]
+
+[Illustration: Marvels of Creation]
+
+
+
+ WONDERS OF CREATION:
+
+ A DESCRIPTIVE ACCOUNT OF
+
+ VOLCANOES AND THEIR PHENOMENA.
+
+ "The mountains quake at Him and the hills melt and the earth is
+ burned at His presence"--NAHUM 1:5
+
+ 1872
+
+
+
+PREFACE
+
+
+Being intended for the Young, this work treats of Volcanoes only in
+a popular way. Scientific details and philosophical speculations
+are accordingly avoided. Nevertheless, a perusal of the following
+pages may so stimulate the curiosity of youthful minds, that some,
+on attaining to riper years and more mature understanding, may be
+inspired with a longing to inquire more deeply into this
+interesting subject. They may be stimulated to investigate, in a
+philosophical spirit, all the marvellous facts and phenomena
+connected with volcanic agency, and to speculate on their causes
+and modes of operation. Some also, on reaching their manhood, may
+be induced to ascend one or more of the nearer active volcanoes,
+and examine their phenomena for themselves. The facilities of
+travel are now so great, that a visit to Vesuvius or Etna is no
+longer beyond the limits of a holiday trip. Even the more remote
+Hecla with the playful Geysers may be reached within a reasonable
+time. Perhaps a very few, who are now scientific travellers in
+embryo, may call to remembrance what they may have read in these
+pages, when, many years hence, they may be climbing the cone of
+Cotopaxi, or peering into the crater of Kilauea.
+
+Apart from these considerations, a perusal of this work may enable
+the young mind to form a more lively idea of the tremendous energy
+of the forces which are imprisoned in the bowels of the earth. Such
+a vivid conception will naturally lead to a higher appreciation of
+the wisdom and power of Him who guides the operation of those
+forces by his laws, and has set bounds to their activity which they
+cannot overpass.
+
+
+
+CONTENTS.
+
+
+CHAPTER I.
+
+Volcanoes in general--Origin of the Name--General Aspect--Crater--
+Cone--Subordinate Cones and Craters--Peak of Teneriffe--Lava-
+Streams--Cascades and Jets of Lava--Variations in its Consistency--
+Pumice--Different Sorts of Lava--Obsidian--Olivine--Sulphur--Dust,
+Ashes, &c.--Volcanic Silk--Volcanic Islands--Volcanic Fishes--Hot
+Water, Mud, Vapours, &c.--Volcanic Storm--Explosions--Number of
+Volcanoes--King of the Volcanoes--Artificial Volcano
+
+
+CHAPTER II.
+
+Volcanoes of Iceland--Mount Hecla--Earliest Eruption--Great
+Eruption in 1845--Skaptàr Yökul--Terrible Eruption in 1783--Rise
+and Disappearance of Nyoë--Katlugaia--The Geysers--A very hot Bath
+--Californian Geysers--Iceland-spar--Jan Mayen
+
+
+CHAPTER III.
+
+Mount Vesuvius--Origin of Name--Former Condition--Eruption of A.D.
+79--Death of Pliny--Destruction of Pompeii and Herculaneum--
+Appearance of the Mountain before and after Eruption--Formation of
+Monte Nuovo--Eruption of Boiling Water--Coloured Vapours--Cascade
+of Lava--Discovery of Remains of Herculaneum and Pompeii--The
+Buildings of Pompeii--Street of Tombs--Skeletons--Sundry Shops--
+Ascents of Vesuvius--Crater--Temple of Serapis
+
+
+CHAPTER IV.
+
+Mount Etna--Its Appearance and Height--Ancient Eruptions--Pindar's
+Allusion--Virgil's Description--Subordinate Cones and Craters--
+Caverns--Val de Bove--Formation of Monti Rossi--Eruption of 1852--
+Whirlwinds--Lava Torrents--Cascades of Lava--Description of Crater
+--Empedocles--Enceladus--Craters of 1865--Cyclopean Isles--Homer's
+Legend--Volcanic Origin--Other Basaltic Groups
+
+
+CHAPTER V.
+
+Lipari Islands--Stromboli--Origin of Name--Position of Crater--
+Description of Crater--New Volcanic Island named Julia--Phenomena
+preceding its Elevation--Description of Island and Crater--Its
+Disappearance--Rise of Islands at Santorin
+
+
+CHAPTER VI.
+
+Peak of Teneriffe--Its Crater--Eruption of Chahorra--Palma--Great
+Caldera--Lancerote--Great Eruption--Sudden Death--Fuego, Cape de
+Verde Islands--Cotopaxi--Its Appearance--Great Eruptive Force--
+Tunguragua--Great Eruption of Mud and Water--Fish thrown out--
+Quito--Its Overthrow--Pichinca--Humboldt's Ascent--Narrow Escape--
+Antisana--Sangay--Rancagua--Chillan--Masaya
+
+
+CHAPTER VII.
+
+Jorullo--Great Monument--Jorullo's Estate--Interruption to his
+Quiet--His Estate Swells--Swallows Two Rivers--Throws up Ovens--
+Becomes a Burning Mountain--Popocatepetl--Spanish Ascents--Orizaba
+--Muller's Ascent--Morne Garou--Pelée--La Soufriere
+
+
+CHAPTER VIII.
+
+Hawaii, Sandwich Islands--Crater of Kilauea--Its awful Aspect--
+Fiery Lake and Islands--Jets of Lava--Depth of Crater and Surface
+of Lake--Bank of Sulphur--Curious Rainbow--Mouna Kaah and Mouna Loa
+--Eruption of the Latter in 1840--Recent Eruption--Great Jet and
+Torrent of Lava--Burning of the Forests--Great Whirlwinds--
+Underground Explosions--Other Volcanoes in the Pacific
+
+
+CHAPTER IX.
+
+Atolls, or Coral Islands--Their strange Appearance--Their Connexion
+with Volcanoes--Their Mode of Formation--Antarctic Volcanoes-
+Diatomaceous Deposits
+
+
+CHAPTER X.
+
+Volcanoes of Java--Papandayang--Mountain Ingulfed--Great
+Destruction of Life and Property--Galoen gong--Destructive
+Eruption--Mount Merapia--Great Eruption, with Hurricane--Another,
+very destructive---Mud Volcano--Crater of Tankuban Prahu--Island of
+Sumbáwa--Volcano of Tomboro--Terrific Eruption--Timor--A Volcano
+quenches itself--Cleaving of Mount Machian--Sangir--Destructive
+Eruption--Bourbon
+
+
+CHAPTER XI.
+
+Mud and Air Volcanoes--Luss--Macaluba--Taman--Korabetoff New Island
+in the Sea of Azof--Jokmali--Fires of Baku--Mud Volcano in Flank of
+Etna--Air Volcanoes of Turbaco, Cartagena, and Galera Zamba
+
+
+CHAPTER XII.
+
+New Zealand--Boiling Fountains and Lakes
+
+
+CHAPTER XIII.
+
+Underground Sounds--Quito--Rio Apure--Guanaxuato--Melida--Nakous
+
+
+CHAPTER XIV.
+
+Extinct Volcanoes--Auvergne--Vienne--Agde--Eyfel--Italy--Lacus
+Cimini--Grotto del Cane--Guevo Upas--Talaga Bodas--The Dead Sea
+
+
+
+
+ WONDERS OF CREATION:
+
+
+ VOLCANOES AND THEIR PHENOMENA.
+
+
+
+
+CHAPTER I.
+
+Volcanoes in general--Origin of the Name--General Aspect--Crater--
+Cone--Subordinate Cones and Craters--Peak of Teneriffe--Lava-
+Streams--Cascades and Jets of Lava--Variations in its Consistency--
+Pumice--Different Sorts of Lava--Obsidian--Olivine--Sulphur--Dust,
+Ashes, &c.--Volcanic Silk--Volcanic Islands--Volcanic Fishes--Hot
+Water, Mud, Vapours, &c--Volcanic storm--Explosions--Number of
+Volcanoes--King of the Volcanoes--Artificial Volcano.
+
+
+Among the many wonderful works of God, none exhibits so much of
+awful grandeur as an active volcano. This name for a burning
+mountain was first applied to that which exists in the island
+anciently called Hiera, one of the Lipari group. It is derived from
+the name of the heathen god Vulcan, which was originally spelt with
+an initial B, as appears from an ancient altar on which were
+inscribed the words BOLCANO SAC. ARA. This spelling indicates the
+true derivation of the name, which is simply a corruption of Tubal-
+cain, who was "an instructer of every artificer in brass and iron"
+(Gen. iv. 22). The ancient heathen, having deified this personage,
+imagined, on first seeing a burning mountain, that Tubal-cain, or
+Vulcan, must have established his forge in the heart of it, and so,
+not unnaturally, named it Volcano--an appellation which the Island
+of Hiera retains to the present day.
+
+The Cyclops--the supposed descendants of Vulcan, who were fabled to
+have been of gigantic stature, and to have had each only one eye in
+the centre of the forehead--were imagined to be the workmen who
+laboured in these underground forges. The noises, proceeding from
+the heart of the mountain, were attributed to their operations. It
+is to the Island of Hiera that Virgil alludes in the Æneid, lib.
+viii. 416. The passage is thus rendered by Dryden:--
+
+ "Sacred to Vulcan's name, an isle there lay,
+ Betwixt Sicilia's coasts and Lipare,
+ Raised high on smoking rocks, and deep below,
+ In hollow caves the fires of Etna glow.
+ The Cyclops here their heavy hammers deal;
+ Loud strokes and hissings of tormented steel
+ Are heard around; the boiling waters roar,
+ And smoky flames through fuming tunnels soar."
+
+A volcano generally presents itself to the imagination as a
+mountain sending forth from its summit great clouds of smoke with
+vast sheets of flame, and it is not unfrequently so described. The
+truth is, however, that a real volcano seldom emits either true
+smoke or true flame. What is mistaken for smoke consists merely of
+vast volumes of fine dust, mingled with much steam and other
+vapours--chiefly sulphurous. What appears like flames is simply the
+glare from the glowing materials which are thrown up towards the
+top of the mountain--this glare being reflected from the clouds of
+dust and steam.
+
+[Illustration: Peak of Teneriffe.]
+
+The most essential part of a volcano is the crater, a hollow basin,
+generally of a circular form. It is often of large dimensions, and
+sometimes of vast depth. Some volcanoes consist of a crater alone,
+with scarcely any mountain at all; but in the majority of cases the
+crater is situated on the top of a mountain, which in some
+instances towers to an enormous height. The part of the mountain
+which terminates in the principal crater is usually of a conical
+form--much like a glass-house chimney, and is therefore named the
+cone. It is generally composed of loose ashes and cinders, with
+here and there masses of stone, which have been tossed into the air
+by the volcanic forces. In some mountains the cone rises out of a
+hollow at a considerable height from the base. A hollow of this
+kind is generally regarded as having been a former crater, which
+had become extinct before the existing cone was raised. There are
+sometimes formed lower down the mountain subordinate craters,
+smaller than that which occupies the summit of the cone. Within the
+crater itself there are frequently numerous little cones, from
+which vapours are continually issuing, with occasional volleys of
+ashes and stones.
+
+One of the largest and most perfect of the volcanic cones in the
+world is that of the Peak of Teneriffe, of which you have here a
+representation. It conveys a good idea of the general form of the
+cone, and has long been a conspicuous and useful landmark to
+mariners. It is upwards of twelve thousand feet in height, and is
+said to be visible in very clear weather at a distance of a hundred
+miles.
+
+The most interesting products of an active volcano are the streams
+of lava which it pours forth--sometimes from the principal crater
+on the summit--sometimes from the smaller craters lower down. This
+lava consists of melted stone. When it issues from the mountain its
+heat is intense and it glows like a furnace, so that, during the
+night especially, these fiery rivers present a grand yet awful
+spectacle. The streams spread themselves till they sometimes attain
+a breadth of several miles, with a depth of several hundred feet,
+and they flow onward till their length sometimes reaches fifty
+miles.
+
+Lava, not being so liquid as water, does not flow so rapidly:
+nevertheless, when it is careering down the sides of a mountain, or
+where the slope of the ground is considerable, it advances with
+great speed. Even when at its hottest, it is somewhat viscid, like
+treacle, and this viscidness increases as it cools. Hence on a
+level plain, and at some distance from its source, the lava-stream
+advances at a leisurely pace. In such circumstances the cooling
+proceeds so quickly that a crust of considerable thickness is soon
+formed on the top of the current, and persons who are bold enough
+may cross the stream by means of this natural bridge. Even where
+the current continues flowing rapidly, this crust may be formed on
+its surface; and a man, whose curiosity exceeds his prudence, may
+stand on the top of it, bore a hole through the crust, and see the
+lava flowing underneath his feet!
+
+Nothing can resist the progress of the lava-flood; trees, houses,
+everything yields to its massive assault, The trees take fire
+before its approach, and when it reaches them they emit a hissing
+noise almost amounting to a shriek, and then plunging into the
+molten flood are seen no more. Even the sea cannot withstand the
+lava-stream, but retires on its approach; so that promontories
+stretching to a considerable distance from the shore are formed in
+this manner, when the molten matter hardens into stone.
+
+The eruptions of lava are sometimes attended by peculiarities which
+impart to them much additional grandeur. Instances have occurred in
+which the fiery stream has plunged over a sheer precipice of
+immense height, so as to produce a glowing cascade exceeding in
+breadth and perpendicular descent the celebrated Falls of Niagara.
+In other cases, the lava, instead of at once flowing down the sides
+of the mountain, has been first thrown up into the air as a fiery
+fountain several hundred feet in height. This happens when the
+great crater at the summit of the cone is full of liquid lava but
+does not overflow. Then, on the formation of an opening in the side
+of the cone, a good way down, the lava issuing from it is projected
+upwards to nearly the same height that it occupies in the interior
+of the crater at the top of the cone. It is hardly possible for the
+fancy to picture to itself anything so magnificent as such a
+fountain of liquid fire must be. A simple jet of water of
+considerable volume, thrown into the air to the height of a hundred
+feet, is itself a beautiful spectacle. What then must be a huge jet
+of glowing white lava projected to the height of several hundred
+feet, and with what an awful thundering sound must it come tumbling
+to the ground, thence to rush as a roaring torrent down the
+mountain's side!
+
+Lava, when congealed, differs in its consistency according as it is
+near the top or near the bottom of the stream. When near the top it
+is porous, owing to its rapid cooling; when near the bottom it is
+dense, owing to its slow cooling and the great pressure to which it
+is subjected. When the lighter superficial lava is brought suddenly
+into contact with water, as when a lava-stream enters the sea, it
+becomes still lighter and more porous--forming the well-known
+substance called pumice, so much used for polishing. It may be
+regarded as the solidified froth of lava, and is so light that it
+floats on the surface of water.
+
+The lavas of different mountains, when cooled and hardened, differ
+much in their appearance and composition. Among those of Iceland is
+found the beautiful black volcanic glass named obsidian. It is a
+good deal used for ornamental purposes; for it possesses the
+peculiar property of presenting a different appearance according to
+the manner in which it is cut. When cut in one direction it is of a
+beautiful jetty black; when cut across that direction it is
+glistering gray. The lavas of Vesuvius are generally of a brown
+colour, and are also used in the arts. In them are found the
+beautiful olive-green crystals of the mineral called olivine,
+sometimes used by jewellers. But the most useful of all volcanic
+productions is native sulphur, in which Mount Etna has been very
+prolific. It is to this mountain chiefly, therefore, that we are
+indebted for our beautiful fire-works--our squibs, crackers, Roman
+candles, serpents, Catherine-wheels, and sky-rockets. Would it had
+produced nothing more harmful than these! But it has also supplied
+one of the ingredients of that villainous gunpowder, which has been
+the means of thrusting so many of our fellow-creatures prematurely
+out of the world. Etna, however, can hardly be held responsible for
+this sad misuse of the valuable substance which it affords; while
+even gunpowder itself has, on the whole, been of vast benefit to
+mankind. Could we only refrain from shooting each other with it, we
+might regard it as an almost unmixed good; for it has helped us
+greatly in forming our roads, railways, and tunnels, and in working
+our quarries and mines.
+
+In all great eruptions the flow of the lava is preceded by the
+ejection of vast quantities of volcanic dust, ashes, dross, slag,
+and loose stones. These are tossed into the air with tremendous
+violence, consequently, to a great height. The stones thus ejected
+are sometimes of immense size. A rock, whose weight is estimated at
+two hundred tons, was thrown from the summit of Cotopaxi to the
+distance of more than ten miles. Large stones have been tossed up
+by Vesuvius to the estimated height of three thousand six hundred
+feet. The dust of the volcano of St. Vincent was carried more than
+two hundred miles to the eastward in the teeth of the trade wind;
+consequently it must have been thrown to an enormous height, in
+order to its falling at so vast a distance from its source.
+
+Besides the usual volcanic dust and ashes, there is sometimes
+thrown from the crater of a volcano a substance resembling spun-
+glass or asbestos. It possesses the flexibility and lustre of silk.
+The volcano of Salazes, in the Island of Bourbon, is remarkable for
+this substance, and it has there been seen to form a cloud covering
+the entire surface of the mountain. But it has also been found in
+other places. How curious it would be to have this volcanic silk
+spun into threads, and knitted into stockings or woven into a
+garment! Who can tell what may happen in these days of adventure
+and invention? Who knows but what some young reader, whose eye is
+now resting on this page, may yet live to present his ladylove with
+a pair of knitted gloves composed of the volcanic silk of Salazes?
+
+Great as the contrast is between this filmy material and the
+ponderous blocks tossed into the air by Cotopaxi and Etna, it is
+not greater than that between the latter and other masses which
+have from time to time been upheaved by volcanic forces. Instances
+have occurred of whole islands having been raised from the bed of
+the ocean, or whole mountains upreared on the surface of the land,
+far away from the sea, and that too in the short space of a few
+hours. But of such we shall have occasion to speak more at large in
+the sequel.
+
+Of all the extraordinary productions that have ever been thrown up
+by volcanoes, the strangest of all are fishes. How droll to dine
+upon fish cooked in a volcano! A queer fish it must be that likes
+to dwell in the bowels of a mountain--more especially of one whose
+entrails are mostly of liquid fire. But of this also more fully
+anon.
+
+In addition to the solid materials thrown out by volcanoes, there
+are sometimes poured forth torrents of boiling water and liquid
+mud. More frequently, however, the water issues in the form of vast
+columns of steam and sulphurous vapour. These ascend to great
+heights in the air, and becoming gradually chilled, they form
+immense masses of dark heavy clouds, similar to those we observe
+before a thunderstorm. Nor is this resemblance apparent only. For
+the clouds that overhang an active volcano during an eruption of
+its vapours are, in reality, thunderclouds highly charged with
+electricity. They accordingly produce what Baron Humboldt calls the
+volcanic storm. It includes all the most terrible of atmospheric
+phenomena--lightnings of extraordinary vividness; thunders that
+peal and reverberate as if they would rend the echoes asunder;
+torrents of rain that pour down upon the mountain and its
+neighbourhood, hissing like thousands of serpents when they fall on
+the glowing lava-torrent; and whirlwinds that sweep the volcanic
+ashes round and round in vast eddies, and before whose violence no
+man of mortal mould is able for a moment to stand.
+
+Beyond and above this din of contending elements are heard the
+hoarse bellowings of the mountain itself, which, meanwhile,
+trembles to its very core. The detonations from the volcano far
+exceed in loudness any other earthly noise. Compared with these,
+the pealing of the loudest thunder is but as the report of a musket
+contrasted with the simultaneous discharge of a thousand pieces of
+heavy ordnance. The explosions of Tomboro, and the vibrations
+accompanying them, have been heard and felt at almost incredible
+distances. Judge, then, of the immensity of the forces which are
+thus brought into play, and the overwhelming grandeur of the scene
+which such an eruption, with all its accompaniments of storm and
+tempest, must present to the bewildered eye and ear. Even to read
+of it sends a thrill through the nerves: what, then, must it be to
+listen and behold?
+
+So far do we dwell from the nearest volcanoes, and so little are we
+familiar with the names except of a few, that not many persons are
+aware of the large number of burning mountains on the face of our
+globe. The total number, however, of those which are known to have
+been active within historic times is fully two hundred. Of these,
+the most familiar to us for its classic fame and its restless
+activity is Mount Vesuvius, which stands alone in its grandeur on
+the continent of Europe. The most violent in its activity is
+Tomboro, in the island of Sumbáwa. The highest is Cotopaxi, in the
+range of the Andes, which rises far into the region of perpetual
+snow. Its height is 16,800 feet above the level of the sea. Strange
+it seems, that volcanic fires should glow at such a height in the
+midst of snow and ice. But in this particular Cotopaxi does not
+stand alone. The Peak of Teneriffe, Mount Etna, and several others,
+also rise above the snow-line; while the burning mountains of
+Iceland, Greenland, and Kamtschatka, with those which rear their
+heads in the frozen regions near the South Pole, are for the most
+part enveloped in ice and snow from head to foot.
+
+Before proceeding to describe to you some of the more interesting
+of the individual volcanoes and volcanic groups, it may be well to
+let you into a secret worth knowing. You would doubtless like to
+have a volcano all to yourself. Here is the receipt: Buy several
+pounds of clean iron filings, and a somewhat larger quantity of the
+flowers of sulphur. Mix the two together and knead them well with
+water into a stiffish paste. Then wrap this pudding in a cloth, and
+put another cloth about it, which has been smeared with common or
+coal-tar. Dig a hole in some quiet corner of your garden, pop your
+dumpling into it, and cover it well up with earth, treading it down
+firmly with your feet. Not many hours will elapse before you will
+see the ground swell like a molehill; an eruption will ensue, and
+you will be the happy possessor of a Stromboli of your own!
+
+
+
+
+CHAPTER II.
+
+Volcanoes of Iceland--Mount Hecla--Earliest Eruption--Great
+Eruption in 1845--Skaptàr Yökul--Terrible Eruption in 1783--Rise
+and Disappearance of Nyoë--Katlugaia--The Geysers--A very hot Bath
+--Californian Geysers--Iceland-spar--Jan Mayen
+
+
+We shall begin with the volcanoes of Iceland, of which the most
+interesting and active is Mount Hecla. The annexed woodcut will
+give you an idea of its appearance. You will observe the column of
+volcanic vapour ascending from the snow-clad summit of the cone,
+and how dreary and desolate is the aspect of the country at its
+base.
+
+The earliest recorded eruption of Mount Hecla took place in the
+ninth century of the Christian era; but probably there had been
+many before that date. Since then there have been between twenty
+and thirty considerable eruptions of this mountain, and it has
+sometimes remained in a state of activity for upwards of six years
+with little intermission. It took a long rest, however, of more
+than sixty years' duration, prior to the year 1845, when it again
+burst forth. After a violent storm on the night of the 2nd of
+September in that year, the surface of the ground in the Orkney
+Islands was found strown with volcanic dust. There was thus
+conveyed to the inhabitants of Great Britain an intimation that
+Hecla had been again at work. Accordingly, tidings soon after
+arrived of a great eruption of the mountain. On the night of the
+1st of September, the dwellers in its neighbourhood were terrified
+by a fearful underground groaning, which continued till mid-day on
+the 2nd. Then, with a tremendous crash, there were formed in the
+sides of the cone two large openings, whence there gushed torrents
+of lava, which flowed down two gorges on the flanks of the
+mountain. The whole summit was enveloped in clouds of vapour and
+volcanic dust. The neighbouring rivers became so hot as to kill the
+fish, and the sheep fled in terror from the adjoining heaths, some
+being burnt before they could escape.
+
+On the night of the 15th of September, two new openings were
+formed--one on the eastern, and the other on the southern slope--
+from both of which lava was discharged for twenty-two hours. It
+flowed to a distance of upwards of twenty miles, killing many
+cattle and destroying a large tract of pasturage. Twelve miles from
+the crater, the lava-stream was between forty and fifty feet deep
+and nearly a mile in width. On the 12th of October a fresh torrent
+of lava burst forth, and heaped up another similar mass. The
+mountain continued in a state of activity up to April 1846; then it
+rested for a while, and began again in the following month of
+October. Since then, however, it has enjoyed repose.
+
+The effects of these eruptions were disastrous. The whole island
+was strown with volcanic ashes, which, where they did not smother
+the grass outright, gave it a poisonous taint. The cattle that ate
+of it were attacked by a murrain, of which great numbers died. The
+ice and snow, which had gathered about the mountain for a long
+period of time, were wholly melted by the heat. Masses of pumice
+weighing nearly half a ton were thrown to a distance of between
+four and five miles.
+
+[Illustration: Mount Hecla]
+
+Mount Hecla is not the only volcano in Iceland. There are several
+others; and from one of them, named Skaptàr Yökul, there was, in
+the year 1783, an eruption still more violent than that from Hecla
+above described. It began on the 8th of June, and raged with little
+abatement till the end of August, whence onward it continued, but
+with less violence, till the following year. The lava, in this
+case, poured from numerous openings; but these rivulets ultimately
+united themselves into two large currents, which flowed onwards to
+the sea. In their progress, these burning torrents filled up the
+beds of two considerable rivers. The greater of the two streams,
+after it had ceased to flow and had become a solid mass of rock,
+measured fifty miles in length, and between twelve and fifteen
+miles in breadth. Its average depth on the plains was about a
+hundred feet; but in the bed of the river, which it had filled, it
+was not less than six hundred feet. The snow and ice, which had
+previously covered the mountain, were not only melted, but the
+water that flowed from them was raised to the boiling point, and
+poured down with destructive effect on the plains. The dust and
+ashes thrown into the air darkened the sun; and they were then
+strown over the surface of the island, destroying all the pastures,
+so that many thousands of cattle, horses, and sheep perished. But
+worse than that, upwards of nine thousand persons lost their lives
+by this dreadful catastrophe.
+
+About a month before this great eruption of Skaptàr Yökul, a
+volcanic island was thrown up from the sea, at a distance of about
+seventy miles from Iceland. So great was the quantity of ashes and
+dross ejected from its crater, that it overspread the sea to a
+distance of a hundred and fifty miles, forming a crust which
+obstructed the progress of ships. Portions of this crust floated as
+far as the Shetland and Orkney islands. The King of Denmark named
+this fiery apparition "Nyoë," or "New Island," and doubtless prided
+himself not a little on this addition to his limited dominions.
+But, alas, for human ambition! About a year after the date of its
+first appearance, Nyoë sank into the depths out of which it arose,
+and its position is now marked only by a moderate shoal.
+
+It is not by their ejected lavas alone that the volcanoes of
+Iceland produce their destructive effects. Disastrous consequences
+have frequently resulted from the sudden melting of their snows and
+glaciers, on which the volcanic fires operate far more rapidly than
+does the heat of the sun. It is chiefly by the vast quantities of
+earth, sand, stones, and broken fragments of rock, which they hurry
+along with them in their wild career, that the waters, so suddenly
+freed, produce the greatest amount of damage. During an eruption of
+Katlugaia, one of the southern Icelandic volcanoes, in 1756, the
+mass of material thus carried down by the melted snows and glaciers
+was so great, that, advancing several leagues into the sea, it
+formed three parallel promontories, which rose above the sea-level,
+where there had formerly been a depth of forty fathoms of water.
+Vast ravines were, at the same time, scooped out of the sides of
+the mountain by the erosion of the waters. Another eruption of this
+volcano in 1860 produced similar results.
+
+Still more interesting than the volcanic mountains of Iceland are
+its Geysers, or intermittent springs of boiling water. The chief of
+these is the Great Geyser. A jet rises to a vast height, and is
+accompanied by much steam. Indeed, it is quite at the boiling-
+point.
+
+The little mound, from the top of which the jet appears to rise, is
+composed of a substance named siliceous sinter, and is a deposit
+from the water of the fountain. At the top of this mound, which is
+between six and seven feet in height, there is an oval basin,
+measuring about fifty-six feet in one direction, and about forty-
+six in the other; its average depth is about three feet. In the
+centre of this basin is a round hole, about ten feet in diameter,
+out of which the water springs. This hole is the mouth of a
+circular well, between seventy and eighty feet in depth. It is down
+this well that the jet retires on its disappearance; and it drags
+along with it all the water out of the basin, leaving both basin
+and well quite empty, without even a puff of steam coming out of
+the hole. In this state of emptiness the basin and well remain for
+several hours. Suddenly the water begins to rise in the well,
+overflowing till it fills the basin. Loud explosions are heard from
+below, and the ground trembles. Then, with amazing violence, up
+springs a vast column of boiling water, surmounted by clouds of
+steam, which obscure the air. This first jet is followed by several
+others in rapid succession, to the number of sixteen or eighteen;
+the last jet being usually the greatest of all, and attaining a
+height of nearly a hundred feet. In some instances it has risen to
+a height of a hundred and fifty feet; and one particular jet was
+measured which rose to the amazing height of two hundred and twelve
+feet.
+
+The action of the fountain seldom continues more than about five
+minutes at a time, and then a repose of several hours ensues. If
+left to itself, the periods of the fountain's activity, though not
+quite regular, generally recur at intervals of six or seven hours.
+But they may be hastened by throwing big stones down the well. This
+not only hurries the eruption of the jet, but increases its energy,
+and the stones are thrown out with great force by the column of
+boiling water; the loudness of the explosions being also
+considerably augmented.
+
+There are several other geysers in the island besides this big one.
+Their jets are smaller, but to compensate this deficiency, they are
+more frequent in their ascent; so that travellers who are too
+impatient to await the eruptions of the Great Geyser, content
+themselves with visiting the little ones.
+
+Would it not be very convenient to live near a geyser? We might
+have our victuals cooked by it, and have pipes led from it all
+round our house, to keep us comfortable in winter; and we might
+have nice hot baths in our dressing-rooms, arid even a little
+steam-engine to roast our meat and grind our coffee. But perhaps
+you may think it might not be altogether pleasant to be kept so
+continually in hot water.
+
+Were any of the water from the geyser to fall on your hands, you
+would doubtless feel it rather sore; still more so, were you to be
+so rash as to thrust your hand fairly into the jet of boiling
+water, as it ascends into the air. Nevertheless, strange as it may
+seem, it would be possible for you, without feeling any pain or
+sustaining any injury, to thrust your hand right into the glowing
+lava as it flows from the crater of Hecla. The only precaution
+needful to be observed, is first to plunge the hand into cold
+water, and then dry it gently with a soft towel, but so as to leave
+it still a little moist. This discovery was made by a French
+philosopher, M. Boutigny, and has been practically proved both by
+him and M. Houdin, the celebrated conjuror, by thrusting their
+hands into molten iron, as it flowed from the furnace. The latter
+describes the sensation as like what one might imagine to be felt
+on putting the hand into liquid velvet.[1] The reason why this
+experiment proves so harmless is that between the skin and the
+glowing substance there is formed a film of vapour, which acts as a
+complete protection. It is this elastic cushion of vapour which
+imparts that feeling of softness described by M. Houdin; for it is
+with it alone that the hand comes into contact.
+
+[1. Houdin's Autobiography, ii 270]
+
+Geysers have been recently discovered in California; but the jets
+do not rise higher than twenty or thirty feet. They are, however,
+very numerous, there being upwards of a hundred openings within a
+space of half a mile square. The vapour from the whole group rises
+to upwards of a hundred and fifty feet into the air. The boiling
+water issues from conical mounds, with great noise. The whole
+ground around them is a mere crust, and when it is penetrated the
+boiling water is seen underneath. The Californian geysers, however,
+are impregnated, not with silica, like those of Iceland, but with
+sulphur, of which they form large deposits. The sulphurous vapours
+from the water corrode the rocks near the fountains; nevertheless
+trees grow, without injury to their health, at a distance from them
+of not more than fifty feet.
+
+Besides obsidian, already mentioned as a product of its volcanoes,
+Iceland is famed for another mineral of great scientific value. It
+is that fine variety of carbonate of lime named Iceland-spar.
+Transparent and colourless, like glass, this mineral possesses the
+property of double refraction--any small object viewed through it
+in a particular direction appearing double. It is much used for
+optical purposes--especially for obtaining polarized light.
+
+There is another volcano lying far to the northward of Iceland. It
+is in the island of Jan Mayen, off the coast of Greenland, and has
+on its summit a vast crater, 2000 feet in diameter, and 500 in
+depth.
+
+
+
+
+CHAPTER III.
+
+Mount Vesuvius--Origin of Name--Former Condition--Eruption of A D
+79--Death of Pliny--Destruction of Pompeii and Herculaneum--
+Appearance of the Mountain before and after Eruption--Formation of
+Monte Nuovo--Eruption of Boiling Water--Coloured Vapours--Cascade
+of Lava--Discovery of Remains of Herculaneum and Pompeii--The
+Buildings of Pompeii--Street of Tombs--Skeletons--Sundry Shops--
+Ascents of Vesuvius--Crater--Temple of Serapis.
+
+
+Mount Vesuvius is the only active volcano on the continent of
+Europe, and it is highly interesting both from its historical
+associations and the frequency of its eruptions. It is situated on
+the coast of the Bay of Naples, about six miles to the eastward of
+the city and at a short distance from the shore. It forms a
+conspicuous feature in the beautiful landscape presented by that
+bay, when viewed from the sea, with the city in the foreground.
+
+Mount Vesuvius was in ancient times held sacred to the deified hero
+Hercules, and the town of Herculaneum, built at its base, was named
+after him. So also, it is said, was the mountain itself, though in
+a more round-about way. Hercules, as you will doubtless learn, was
+feigned to have been the son of the heathen god Zeus and Alcmena, a
+Theban lady. Now one of the appellations of Zeus was Υης,
+which was applied to him as being the god of rains and dews--the
+wet divinity. Thus Hercules was Υησουυιος, the son of Ves. How
+this name should have become corrupted into "Vesuvius," you can be
+at no loss to perceive.
+
+Vesuvius was not always a volcano. It was for many ages a very
+peaceable and well-behaved mountain. Ancient writers describe it as
+having been covered with gardens and vineyards, except at the top
+which was craggy. Within a large circle of nearly perpendicular
+cliffs, was a flat space sufficient for the encampment of an army.
+This was doubtless an ancient crater; but nobody in those times
+knew anything of its history. So little was the volcanic nature of
+the mountain suspected, that the Roman towns of Stabiæ, Pompeii,
+and Herculaneum had been erected at its base, and their inhabitants
+dwelt in fancied security.
+
+In the year A.D. 63, however, the dwellers in the cities got a
+great fright; for the mountain shook violently, and a good many
+houses were thrown down. But soon all became quiet again, and the
+people set about rebuilding the houses that had fallen. They
+continued to live in apparent safety for some time longer. They
+danced, they sung, they feasted; they married, and were altogether
+as merry a set of citizens as any in southern Italy. But the 24th
+of August A.D. 79 at length arrived. Then, woe to Stabiæ! woe to
+Pompeii! woe to Herculaneum!
+
+Pliny the elder was that day in command of the Roman fleet at
+Misenum, which was not far off. His family were with him, and,
+among others, his nephew, Pliny the younger, who has left an
+interesting account of what happened on the occasion. He observed
+an extraordinary dense cloud ascending in the direction of
+Vesuvius, of which he says:--"I cannot give you a more exact
+description of its figure, than by resembling it to that of a pine
+tree; for it shot up to a great height in the form of a tall trunk,
+which spread out at the top into a sort of branches. It appeared
+sometimes bright, and sometimes dark and spotted, as it was either
+more or less impregnated with earth and cinders"
+
+On seeing this remarkable appearance, the elder Pliny, who was a
+great naturalist and a man of inquiring mind, resolved to go ashore
+and inspect more narrowly what was going on. But a rash resolve it
+proved. Steering towards Retina (now Resina), a port at the foot of
+the mountain, he was met, on his approach, by thick showers of hot
+cinders, which grew thicker and hotter as he advanced--falling on
+the ships along with lumps of pumice and pieces of rock, black but
+burning hot. Vast fragments came rolling down the mountain and
+gathered in heaps upon the shore. Then the sea began suddenly to
+retreat, so that landing at this point became impracticable. He
+therefore steered for Stabiæ, where he landed, and took up his
+abode with Pomponianus--an intimate friend.
+
+Meanwhile, flames appeared to issue from several parts of the
+mountain with great violence--the darkness of the night heightening
+their glare. Pliny nevertheless went to sleep. Soon, however, the
+court leading to his chamber became almost filled with stones and
+ashes; so his servants awoke him, and he joined Pomponianus and his
+household. The house now began to rock violently to and fro; while
+outside, stones and cinders were falling in showers. They,
+notwithstanding, thought it safer to make their way out from the
+tottering mansion; so, tying pillows upon their heads with napkins,
+they sallied forth. Although it was now day, the darkness was
+deeper than that of the blackest night. By the aid of torches and
+lanterns, however, they groped their way towards the beach, with a
+view to escape by sea; but they found the waves too high and
+tumultuous. Here Pliny, having drunk some cold water, lay down upon
+a sailcloth which was spread for him; when almost immediately
+flames, preceded by a strong smell of sulphur, issuing from the
+ground, scattered the company and forced him to rise. With the help
+of two of his servants he succeeded in raising himself; but, choked
+by some noxious vapour, he instantly fell down dead.
+
+[Illustration: Vesuvius Before the Eruption of A.D. 79.]
+
+Nor was he alone in his death; for although many of the inhabitants
+of the devoted cities were able to effect their escape; yet, so
+suddenly did the overwhelming shower of ashes, cinders, and stones
+fall upon them, that not a few of them perished in their dwellings
+or their streets. As for the cities themselves, they were utterly
+buried completely out of sight, and, like other things that are
+long out of sight, they soon became also buried out of mind. For
+many centuries they remained entirely forgotten.
+
+You will doubtless like to know how Vesuvius looked, after doing so
+much mischief. Here is a picture showing what like it was
+immediately before the eruption; and one showing its appearance
+soon after the event. On comparing the two, you will observe the
+mountain had undergone a great change. It was no longer flat on the
+top, but had formed for itself a large cone, from the summit of
+which dense vapours ascended. This cone was composed entirely of
+the ashes, cinders, and loose stones, thrown up during the
+eruption. It had become separated by a deep ravine from the
+remainder of the former summit, which afterwards came to be
+distinguished by the name Monte Somma. The whole of the forests,
+vineyards, and other luxuriant vegetation, which had covered that
+portion of the sides of Vesuvius where the eruption took place,
+were destroyed. Nothing could be more striking than the contrast
+between the beautiful appearance of the mountain before this
+catastrophe, and its desolate aspect after the sad event. This
+remarkable contrast forms the subject of one of Martial's Epigrams,
+lib. iv. Ep. 44. It is thus rendered by Mr. Addison:--
+
+[Illustration: Vesuvius after the Eruption of A.D. 79.]
+
+ "Vesuvius covered with the fruitful vine
+ Here flourished once, and ran with floods of wine.
+ Here Bacchus oft to the cool shades retired,
+ And his own native Nysa less admired.
+ Oft to the mountain's airy tops advanced,
+ The frisking Satyrs on the summit danced.
+ Alcides [1] here, here Venus graced the shore,
+ Nor loved her favourite Lacedaemon more.
+ Now piles of ashes, spreading all around,
+ In undistinguished heaps deform the ground.
+ The gods themselves the ruined seats bemoan,
+ And blame the mischiefs that themselves have done."
+
+[1. Hercules]
+
+Since the eruption of A.D. 79, Vesuvius has had many fits of
+activity with intervals of rest. In A.D. 472, it threw out so great
+a quantity of ashes, that they overspread all Europe, and filled
+even Constantinople with alarm. In A.D. 1036 occurred the first
+eruption in which there was any ejection of lava. This eruption was
+followed by five others, the last of which occurred in 1500. To
+these succeeded a long rest of about a hundred and thirty years,
+during which the mountain had again become covered with gardens and
+vineyards as of old. Even the inside of the crater had become
+clothed with shrubbery.
+
+In this interval, however, there was an extraordinary eruption--not
+of Vesuvius itself, but at no great distance from it, in the Bay of
+Baiæ, on the opposite shore of the Bay of Naples. The whole of
+this neighbourhood is a volcanic country, and was anciently named
+the Phlegræan Fields. It contains a crater in a state of subdued
+activity, called the Solfatara; an extinct volcano having a large
+crater called Monte Barbaro; and Lake Avernus, also supposed to be
+an extinct volcanic crater. Between Monte Barbaro and the sea,
+there was formerly a fiat piece of ground bordering on the Lucrine
+Lake, which is separated from the Bay of Baiæ by a narrow strip of
+shingle. On the 29th of September 1538, the flat piece of ground
+above mentioned became the scene of a great eruption, which
+resulted in the throwing up of a new elevation to the height of
+four hundred and thirteen feet, and with a circumference of eight
+thousand feet. It received the name of Monte Nuovo, and is now
+covered with a luxuriant vegetation.
+
+In 1631 there was another dreadful eruption of Mount Vesuvius,
+which covered with lava most of the villages at the foot of the
+mountain. To add to the calamity, torrents of boiling water were,
+on this occasion, thrown out by the volcano, producing awful
+destruction.
+
+There have been since that time numerous eruptions, which it would
+be tedious to mention in detail; but two of them are worthy of
+notice. During an eruption in February 1848, a column of vapours
+arose from the crater about forty feet high, presenting a variety
+of colours; and a short time afterwards there arose ten circles,
+which were black, white, and green, and which ultimately assumed
+the form of a cone. A similar appearance had been observed in 1820.
+More recently, in May 1855, a great stream of glowing lava, about
+two hundred feet in breadth, flowed towards a vast ravine nearly a
+thousand feet in depth. The first descent into this chasm is a
+sheer precipice, over which the lava dashed heavily, forming a
+magnificent cascade of liquid fire.
+
+Of the buried cities of Herculaneum and Pompeii no traces were
+discovered till the year 1713, when some labourers, in digging a
+well, came upon the remains of Herculaneum about twenty-four feet
+underground. Little attention, however, was paid to the discovery
+at that time; but in 1748 a peasant, digging in his vineyard,
+stumbled on some ancient works of art. On sinking a shaft at this
+spot to the depth of twelve feet, the remains of Pompeii were
+found. This discovery led to further researches, and the exact
+positions of the two cities were erelong ascertained. The work of
+disinterment has continued with little interruption from that to
+the present time, and many valuable specimens of ancient art have
+been brought to light.
+
+The greatest progress has been made at Pompeii; because the stuff,
+in which it was buried, is far looser than that which covers
+Herculaneum. In the former city, although it was anciently reckoned
+only a third-rate place, there have already been discovered eight
+temples, a forum, a basilica, two theatres, a magnificent
+amphitheatre, and public baths. The ramparts, composed of huge
+blocks of stone, have also been exposed. One of the most remarkable
+places is the Cemetery. It consists of a broad path covered with
+pavement, and bordered on either side with stately monuments,
+placed over the tombs of the wealthy citizens of the place, and in
+which whole families have been interred.
+
+The houses were found filled with elegant furniture, the walls of
+the apartments adorned with beautiful paintings. Numerous statues,
+vases, lamps, and other elegant works of art, have been recovered.
+Many skeletons have also been found, in the exact positions in
+which the living men were caught by the deadly shower of
+suffocating ashes. The excavators came upon the skeleton of a
+miser, who had been attempting to escape from his house, and whose
+bony fingers were still clutching the purse which contained the
+treasure he loved. There were also found in the barracks at Pompeii
+the skeletons of two soldiers chained to the stocks; and the
+writings scribbled by the soldiers on the walls are still quite
+legible. In the vaults of a villa in the suburbs were discovered
+the skeletons of seventeen persons, who had probably sought refuge
+there, and been entombed. The stuff in which they were imbedded had
+been originally soft, but had become hardened through time. In this
+substance was found a cavity, containing the skeleton of a female
+with an infant in her arms. Although nothing but the bones
+remained, the cavity contained a perfect cast of the woman's
+figure--thus showing that she must have been imbedded in the
+substance while alive. Round the neck of this skeleton there was a
+gold chain, and on the fingers jewelled rings.
+
+In many of the houses the names of the owners over the doors are
+still legible, and the fresco-paintings on the inner walls are
+still quite fresh and beautiful. The public fountains are adorned
+with shells formed into patterns; and in the room of a painter
+there was found a collection of shells in perfectly good order. A
+large quantity of fishing-nets was found in both the cities, and in
+Herculaneum some pieces of linen retaining its texture. There also
+was discovered a fruiterer's shop, with vessels full of almonds,
+chestnuts, carubs, and walnuts. In another shop stood a glass
+vessel containing moist olives, and a jar with caviare--the
+preserved roe of the sturgeon. In the shop of an apothecary stood a
+box that had contained pills, now reduced to powder, which had been
+prepared for a patient destined never to swallow them--a happy
+circumstance for him, if he eventually escaped from the city. Very
+recently there has been laid open a baker's shop, with the loaves
+of bread on the shelves, all ready for his customers, but doomed
+never to be eaten. These loaves are of the same form as those still
+made in that country, and on being analyzed were found to consist
+of the same ingredients as modern bread.
+
+Mount Vesuvius rises rather abruptly from the plain on which it
+stands. The circuit of the base is about twelve miles, and the
+height of the summit above the level of the sea about three
+thousand feet. This latter measurement, however, alters from time
+to time, owing to the variable height of the cone. Its moderate
+elevation, and the ease with which it may be approached, have
+induced many travellers to ascend the mountain; and not a few have
+recorded their experiences. So frequent are the eruptions of the
+volcano, however, and so much do they change the aspect of the
+crater, that any description remains correct for only a limited
+time.
+
+Within the last hundred years the crater has been five times wholly
+altered, in consequence of its interior having been completely
+blown out, and its walls having crumbled down. When Sir William
+Hamilton ascended the mountain in 1756, it had no less than three
+craters and cones, one within another. The outermost was a very
+wide-mouthed cone. Within it rose centrically another, smaller in
+size and narrower in the mouth; and within that again was the third
+and highest, having a smaller base and still narrower opening at
+the top, whence the greatest volume of vapour ascended. In 1767
+this innermost cone merged in the second, which was greatly
+enlarged; and by a subsequent eruption the interval between the
+first and second was obliterated, so that only a single cone
+remained. In 1822 the whole interior of the cone was blown out, and
+its walls crumbled down, so as to lower the height of the mountain
+several hundred feet. But within the vast gulf, nearly a mile in
+diameter, which was thus left yawning open, there soon began to be
+formed a new cone, which showed itself erelong above the jagged
+edge of the crater. Eventually this cone increased, by the
+accumulation of ejected matters, to such an extent as to obliterate
+the division between it and the rim of the former crater--thus once
+more establishing a continuous cone. Since that time, the cone and
+crater have twice undergone similar changes.
+
+The most usual appearance of the crater, when in comparative
+repose, is that of a vast circular or oval hollow basin, with
+nearly perpendicular walls, broken in their continuity, every here
+and there, by large projecting dykes, formed by the injection of
+more recent lavas into fissures rent in those which had previously
+become consolidated. Below the perpendicular walls is a rapid
+slope, composed of fine ashes or sand, descending to the floor of
+the crater, which is, for the most part, nearly flat. It is much
+rent by fissures, which during the night are seen to glow with a
+ruddy glare, emanating from the hot materials beneath, and giving
+to the floor the appearance of being overspread with a fiery
+tissue, like a spider's web. From the bottom there usually rise one
+or two small craters of eruption, whence continually issue
+sulphurous fumes, and which, at pretty regular intervals, discharge
+showers of stones heated to whiteness.
+
+The exterior of the cone is composed entirely of loose cinders,
+ashes, and stones, so that the ascent is very laborious. The region
+of the mountain beneath the cone presents no difficulties, and that
+part of the ascent may be performed on donkeys or mules. The view
+from the top is magnificent. The contrast between the desolate
+aspect of the interior of the crater, and the smiling prospect
+which may be seen from its edge, has been well compared to looking
+out of Tartarus into Paradise.
+
+Near Puzzuoli, in the Bay of Baiæ, and not far from Monte Nuovo,
+stand the ruins of the Temple of Serapis, so interesting to
+geologists. These remains, consisting chiefly of the shafts of
+three marble columns, still erect, though with a slight inclination
+sea-ward, afford distinct proofs, confirmed by other phenomena in
+the neighbourhood, that, since the beginning of the Christian era,
+the level of the coast in relation to that of the sea has changed
+twice--the land having first sunk and been then raised again, each
+time to the extent of upwards of 20 feet. The evidence of the
+submergence of the pillars consists mainly of a zone commencing at
+the height of about 12 feet above their pedestals, and extending 9
+feet upwards, in which are numerous perforations, made by a marine
+bivalve mollusc. The upraising again of the ground on which the
+temple stands, to nearly its original height, appears to have
+occurred about the time of the formation of Monte Nuovo.
+
+
+
+
+CHAPTER IV.
+
+Mount Etna--Its Appearance and Height-Ancient Eruptions-Pindar's
+Allusion--Virgil's Description--Subordinate Cones and Craters-
+Caverns--Val del Bove--Formation of Monti Rossi--Eruption of 1852--
+Whirlwinds--Lava Torrents--Cascades of Lava--Description of Crater
+--Empedocles--Enceladus--Craters of 1865-Cyclopean Isles--Homer's
+Legend-Volcanic Origin--Other Basaltic Groups
+
+
+Mount Etna may well be called the Queen of European Volcanoes, so
+majestic does she look, with her lofty summit glistening in the
+sunbeams white with snow, yet pouring forth volumes of vapour. This
+mountain, as you will observe from the annexed woodcut, is
+altogether more massive in its appearance than Vesuvius. It is
+about three times higher, rising to nearly eleven thousand feet
+above the level of the sea, and it has a circuit of about eighty-
+seven miles at its base.
+
+Etna has been a volcano from time immemorial; but of its more
+ancient eruptions only vague traditions have survived. The Greek
+poet Pindar is the earliest writer who makes mention of its
+activity. He refers to it in his first Pythian Ode, Strophe B, 1.
+1. The passage is thus rendered by Carey--
+
+ "From whose caverned depths aspire,
+ In purest folds upwreathing, tost
+ Fountains of approachless fire--
+ by day a flood of smouldering smoke
+ With sullen gleam the torrents pour"
+
+[Illustration: Mount Etna.]
+
+The ode in which this allusion occurs is said to have been written
+about B.C. 470; and the eruption to which it refers probably took
+place shortly before that date.
+
+Virgil also describes the mountain very forcibly in the Æneid,
+lib. iii. 570. Dryden renders the passage thus:--
+
+ "The port capacious, and secure from wind,
+ Is to the foot of thund'ring Etna joined.
+ By turns a pitchy cloud she rolls on high:
+ By turns hot embers from her entrails fly,
+ And flakes of mounting flames, that lick the sky.
+ Oft from her bowels massy rocks are thrown,
+ And shivered by the force come piece-meal down.
+ Oft liquid lakes of burning sulphur flow,
+ Fed from the fiery springs that boil below."
+
+Since the one to which Pindar alludes, there have been recorded
+about sixty eruptions; but in the present century Etna has been
+less frequently active than Vesuvius.
+
+Owing to the great height of Mount Etna, the lava seldom rises so
+far as to flow from the summit. It more frequently bursts forth
+from the flanks of the mountain; and in this manner there have been
+formed numerous smaller cones, of which several have craters of
+their own. Hence Etna is rather a group of volcanoes than a single
+cone; but all these subordinate volcanic hills cluster round the
+flanks of the great central summit. Etna may thus be regarded as a
+fertile mother of mountains, with all her children around her. Some
+of these hills, her offspring, are covered with forests and rich
+vegetation--such having enjoyed a lasting repose. Others are still
+arid and bare, having been more recently formed. Owing to this
+peculiarity in its structure, Etna does not present that conical
+aspect which characterizes most other volcanoes. Strange as it may
+seem, there are, on the sides of the mountain, caverns which the
+Sicilians use for storing ice. Some of these caverns are of vast
+extent. One called Fossa della Palomba measures, at its entrance,
+625 feet in circumference, and has a depth of about 78 feet. This
+great cavity, however, forms merely the vestibule to a series of
+others, which are perfectly dark.
+
+Another striking feature of Mount Etna is the Val del Bove. It is a
+deep valley, presenting, when viewed from above, somewhat of the
+appearance of an amphitheatre, It stretches from near the summit
+down to the upper limit of the wooded region of the mountain, and
+has a remarkably desolate aspect--presenting a vast expanse of bare
+and rugged lava.
+
+Of the numerous eruptions of Etna, one of the most memorable was
+that of 1669, when on the flank of the mountain above Nicolosi,
+about half way between Catania and the top of the great crater,
+there was formed an immense rent about twelve miles long, from
+which a vast torrent of lava descended. After flowing for several
+miles, and destroying a part of Catania in its course, it entered
+the sea, and formed a small promontory, which has since proved very
+useful as a breakwater. But besides this stream, there were at the
+same time thrown up such immense quantities of ashes, cinders,
+stones, and other matters, that they formed two conical hills, more
+than three hundred feet in height above the slope of the mountain
+from which they rose, and measuring nearly two miles in
+circumference at their base. These hills were named Monti Rossi.
+
+Mount Etna was in activity as lately as 1865; but a previous
+eruption in 1852 was of greater violence. It began, as usual, with
+hollow underground rumblings, and the ascent of dense columns of
+vapour, mingled with dust and ashes, high into the air. These were
+speedily whirled into enormous eddies by fierce whirlwinds. Two new
+mouths were formed on the side of the mountain, and these vomited
+forth immense streams of lava, which rushed with the vehemence of a
+torrent down the steep. The violence of the commotion increasing,
+the two mouths were, by the crumbling of the intervening rocks,
+blended into one, and then huge fragments of the broken rock were
+hurled to a great height, along with vast quantities of hot stones,
+cinders, and black sand. Increasing quantities of lava were now
+poured from the greatly enlarged opening, and these formed on the
+plains below a great river of liquid fire, nearly two miles in
+breadth, and between seven and eight feet in depth, which advanced
+at the rate of upwards of a hundred feet in an hour, carrying
+before it devastation and ruin. Its course being through a highly
+cultivated country, the damage it inflicted was immense. This
+eruption continued for several months, with only short intervals of
+rest.
+
+[Illustration: Crater of Etna.]
+
+It has more than once happened, that the lava-streams of Etna, in
+their descent from the crater of eruption, have come to a
+precipitous wall of rock, over which they have plunged in a cascade
+similar to that formed by the lava of Vesuvius in 1855, but on a
+less magnificent scale, as respects the height of the fall. One of
+these occasions was during the eruption of 1771, and another during
+that of 1819.
+
+The principal cone of Mount Etna was ascended in 1834 by Messrs.
+Elie de Beaumont and Leopold von Buch. The former describes what
+they saw in the following terms:--"It was to us a moment of
+surprise difficult to describe, when we found ourselves
+unexpectedly on the margin--not, indeed, of the great crater--but
+of an almost circular gulf, nearly three hundred feet in diameter,
+which does not touch the great crater save at a small part of its
+circumference. We peered eagerly into this nearly cylindrical
+funnel; but vain was our search into the secret of its volcanic
+action. From the almost horizontal tops of the nearly vertical
+steeps, nothing can be descried but the upper cone. On trying to
+reckon those one below another, vision becomes gradually lost in
+the perfect darkness beneath. No sound issues from this darkness.
+There are only exhaled slightly sulphurous white vapours, chiefly
+steam. The dismal aspect of this black and silent gulf, in which
+our view was lost--its dark moist sides, along which crept, in a
+languid and monotonous manner, long flakes of vapour of a sombre
+gray--the great crater to which this narrow gulf is attached, with
+its confused heap of diverse substances, coloured yellow, gray,
+red, like the image of chaos--all presented around us an aspect
+quite funereal and sepulchral."
+
+The French geologist, in having escaped from his visit to the
+crater with nothing worse than a fit of the vapours, came off
+better than Empedocles, the Sicilian philosopher, in the days of
+old: for, as the story goes, this inquisitive sage, being very
+anxious to have a peep into the crater, and venturing too near,
+toppled in altogether, and nothing more was seen of him, except one
+of his sandals, which was vomited up by the volcano--thus conveying
+to his friends an intimation of the manner of his death.
+
+Some incredulous persons allege that this story has no better
+foundation than the fable of the poets, that the giant Enceladus,
+son of Titan and Terra, having offended Jupiter, the infuriated god
+first felled him with a thunderbolt, and then put Mount Etna as a
+sort of extinguisher on the top of him--his restlessness underneath
+fully accounting for all the commotions of the mountain.
+
+Soon after the eruption which took place towards the end of January
+1865, the craters then opened were visited by M. Fouqué, a French
+geologist. At the time of his visit, 10th March, they were seven in
+number, and he thus describes their modes of action:--
+
+"The three upper craters produced two or three times a minute,
+powerful detonations like thunderclaps. The lower craters, on the
+contrary, incessantly gave forth a succession of reports too rapid
+to be reckoned. These sounds, although unremitting, were clear and
+distinct, the one from the other. I can find no better comparison
+for them than the strokes of a hammer falling on an anvil. Had the
+ancients heard a similar noise, I can readily conceive whence arose
+the idea of their imagining a forge in the centre of Etna, with the
+Cyclops for workmen."
+
+Off the eastern coast of Sicily, and not far from Mount Etna, lie
+the Cyclopean Isles, of one of which the annexed woodcut gives a
+representation. You will observe what a singular appearance it
+presents, with its rows of basaltic columns piled one above
+another. The other isle is close by, and there is an ancient
+tradition that they at one time formed part of the mainland of
+Sicily. Homer has a curious story about the manner in which they
+became detached. The passage occurs towards the end of the ninth
+book of the Odyssey. He tells that, at the time Ulysses visited
+Sicily, it was inhabited by the Cyclops, who, as already mentioned,
+were said to have had each only one eye, situated in his forehead.
+Their king's name was Polyphemus, a huge giant who beguiled Ulysses
+and a portion of his crew into a cave, where he killed some of the
+crew and devoured them for his supper. Ulysses, fearing his turn
+might come next, persuaded Polyphemus to taste some strong wine he
+had with him, and filled him so tipsy that he fell fast asleep.
+While he was in this state, Ulysses burnt out his one eye with a
+red-hot iron. The giant awoke in agony, but Ulysses contrived to
+escape from his clutches, and, after getting into his ship, began
+taunting and jeering the monster. Thereupon Homer says:--
+
+[Illustration: Cyclopean Isle]
+
+ "These words the Cyclops' burning rage provoke:
+ From the tall hill he rends a pointed rock;
+ High o'er the billows flew the massy load,
+ And near the ship came thund'ring on the flood.
+ It almost brushed the helm, and fell before:
+ The whole sea shook, and refluent beat the shore."
+
+ Pope's _translation_.
+
+The huge missile having thus missed its mark, Ulysses, with great
+impudence, renewed his jeers, taunting the giant, and telling him
+who it was that had poked out his eye; whereupon Polyphemus invokes
+the vengeance of Neptune upon him, and--
+
+ "A larger rock then heaving from the plain,
+ He whirled it round--it rung across the main:
+ It fell and brushed the stern: the billows roar,
+ Shake at the weight, and refluent beat the shore."
+
+ Pope's _translation_.
+
+The rocks of which the Cyclopean Isles are composed are entirely of
+volcanic origin, and it is far from improbable that they may have
+at one time been attached to Sicily, and severed from it by some
+great volcanic convulsion. A careful examination of these large
+piles of basaltic columns led Dr. Daubeny to the conclusion, that
+the lavas from which they have been formed were consolidated under
+great pressure, and probably at the bottom of the sea, whence they
+have been afterwards upheaved. He also concludes, from certain
+appearances, that the two islands were at one time united.
+
+The Cyclopean Isles strongly resemble, in their general aspect, the
+well-known Giant's Causeway on the northern coast of Ireland, and
+the Isle of Staffa off the western coast of Scotland. The latter,
+which, around its whole sea-girt outline, presents ranges of
+basaltic columns, some of them disposed in curious fantastic
+groups, most nearly resembles the Sicilian pair. These differ from
+it chiefly in their having the columns piled in terraces, one above
+another. Staffa, however, can boast of a far more striking feature
+--the celebrated Cave of Fingal--its stately basaltic columns
+inspiring every beholder with admiration, not unmixed with awe,
+while its brightly-tinted floor rivals in brilliancy of colouring
+the most beautiful mosaics.
+
+In the Island of Iceland, also, there are some remarkable ranges of
+basaltic columns. One in particular, named the Ruins of
+Dverghamrar, is in the form of a semicircle skirting the sea-coast.
+Another group, still more wonderful, forms a curious natural Gothic
+arch, surmounted by pinnacles. It is so picturesque that an
+architect might study it with advantage, and derive from it
+valuable hints in designing the entrance to a cathedral.
+
+
+
+
+CHAPTER V.
+
+Lipan Islands--Stromboli--Origin of Name--Position of Crater--
+Description of Crater--New Volcanic Island named Julia--Phenomena
+preceding its Elevation--Description of Island and Crater--Its
+Disappearance--Rise of Islands at Santorin
+
+
+The Lipari Islands are all of volcanic origin. The most interesting
+among them, for the length of time it has been in action and the
+constancy of its activity, is Stromboli. This name is a corruption
+of the ancient Greek name Στρογγυλη which was given to it
+because of its round swelling form. This is a very fussy little
+volcano, for it keeps perpetually puffing, growling, and fuming. It
+throws out columns of steam, and at intervals stones, cinders, and
+ashes, which are for the most part drifted by the wind into the
+sea. This restless volcano has been in almost uninterrupted
+activity since at least the third century before the Christian era
+--however much further back.
+
+Several enterprising travellers have ascended to the crater of
+Stromboli. It was examined with great care in 1828 by M. Hoffmann,
+a celebrated Prussian geologist, who, while being held fast by his
+companions, leant over the crag immediately above the crater, and
+looked right down into one of its active mouths. He thus describes
+what he saw:--
+
+"Three active mouths were seen at the bottom of the crater. The
+principal one, in the middle, was about two hundred feet in
+diameter; it shows nothing remarkable, only fuming slightly; and
+numerous yellow incrustations of sulphur coat the walls of its
+chimney. Close by this mouth is another, somewhat nearer the
+precipice, only twenty feet wide, in which I could observe the play
+of the column of liquid lava, which at intervals poised itself at a
+level. This lava did not look like a burning mass vomiting flames,
+but as glossy as molten metal--like iron issuing from the smelting
+furnace, or silver at the bottom of a crucible.
+
+"This melted mass rose and fell--evidently urged by the powerful
+tension of elastic vapours pressing it upwards from beneath; and it
+was easy to perceive the balance of effect between the weight of
+the molten masses and the pressure of the steam which resisted
+them. The surface rose and fell rhythmically: there was heard a
+peculiar sound, like the crackling of air from bellows entering the
+door of a furnace. A bubble of white vapour issued at each crack,
+raising the lava, which fell down again immediately after its
+escape. These bubbles of vapour dragged to the surface of the lava
+red-hot cinders, which danced as if tossed by invisible hands in
+rhythmic sport above the brink of the opening.
+
+"This play, so regular and attractive, was interrupted, every
+quarter of an hour or so, by more tumultuous movements. The mass of
+whirling vapour then rested motionless for a moment--even making a
+jerking motion of return, as if inhaled by the crater, from the
+bottom of which the lava rose more strongly as if to encounter it.
+Then the ground trembles, and the walls of the crater starting
+bend. It was quite an earthquake. The mouth of the crater uttered a
+loud rolling bellow, which was followed by an immense bubble of
+vapour, bursting at the surface of the lava with a loud thundering
+report. The whole surface of the lava, reduced to glowing
+splinters, was then tossed into the air.
+
+[Illustration: Julia, or Graham's Island, in August 1831.]
+
+"The heat struck our faces forcibly; while a flaming sheaf rose
+right into the air, and fell back in a shower of fire all around.
+Some bombs ascended to a height of about 1200 feet, and in passing
+over our heads described parabolas of fire. Immediately after such
+an eruption, the lava withdrew to the bottom of the chimney, which
+then yawned black and gaping. But erelong there was seen re-
+ascending the shining mirror of the surface of lava, which then
+recommenced the rhythmic play of its ordinary less violent
+bubblings."
+
+What an agreeable visit this must have been! Don't you think,
+between ourselves, that the German philosopher must, on this
+occasion, have greatly resembled an Irishman in love, seeing he was
+so eager to reach the mouth of the _crater?_
+
+Before passing on to the description of other existing volcanoes,
+it may entertain you to hear something about Julia. This
+interesting _crater_ had a short and troubled existence. She
+was not born like others of her name, but rose suddenly and
+majestically out of the sea, as the poets feign that Venus did of
+old. She did not, however, keep her head long above water, but
+after raging and fuming for about a couple of months, she plunged
+again under the waves. This happened in the year 1831.
+
+On page 57 is a picture showing you how she looked in August of
+that year, about a month after she made her appearance. You see
+what a fury of a _crater_ she must have been. It was a French
+philosopher (Constant Prévost) who christened her Julia; but it is
+hard to divine what prompted him to act so ungallantly. Perhaps, at
+the moment, he may have had in his eye some Julia of his
+acquaintance, with very red hair and a very fiery temper.
+
+This volcanic island rose out of the Mediterranean, about midway
+between the Island of Pantellaria and the village of Sciacca on the
+southern coast of Sicily. From about the 28th of June to the 2nd of
+July 1831, the inhabitants of Sciacca felt several slight shocks,
+which they imagined to have proceeded from Etna. On the 8th of July
+the crew of a Sicilian ship, which was sailing at a distance of
+about six miles from Sciacca, suddenly observed in the sea a jet of
+water about 100 feet high. It rose into the air with a thundering
+noise, sustained itself for about ten minutes, and then fell down.
+Similar jets continued to rise in succession, at intervals of about
+a quarter of an hour, and produced a thick mist overspreading the
+surface of the sea, which was much agitated and covered with a
+reddish scum. Shoals of dead fishes were drifted on the waves. On
+the third day the jets were between 800 and 900 feet in diameter,
+and between 60 and 70 feet in height, while the steam from them
+rose to nearly 1800 feet.
+
+On the 12th of July the inhabitants of Sciacca had their nostrils
+assailed by a strong smell of sulphur, and beheld the surface of
+the sea covered with black porous cinders, which, being drifted
+ashore, formed a bed of some thickness on the beach. So great was
+the drift of volcanic ashes, that boats could hardly struggle
+through the water, and multitudes of dead fishes floated on its
+surface. Next morning they saw rising out of the sea a column of
+dark vapour, which, however, towards night became lurid red. From
+time to time, during both the day and night, they heard loud
+reports, and saw bright sparks of fire through the dusky vapour.
+
+[Illustration: Julia, or Graham's Island, on 29th September 1831.]
+
+On the 18th of July the captain of the Sicilian ship discovered
+that an island had arisen out of the sea at the spot whence the
+appearances before described had proceeded. It had already attained
+a height of nearly twelve feet, and had in its centre a crater,
+which vomited forth immense jets of steam, along with ashes,
+cinders, stones, &c. The water which boiled in this crater was
+reddish, and the cinders, which covered the sea all round the
+island, were of a chocolate colour. The island subsequently
+attained a height of upwards of 90 feet at its highest point, and a
+circumference of about three-quarters of a mile. A channel of
+communication was also opened between the sea and the interior of
+the crater, which had a diameter of about 650 feet. The vapours and
+other matters thrown up from the mouth of the volcano formed a
+luminous column upwards of 200 feet in height.
+
+On the 29th of September it was visited by the French gentleman who
+gave it the name of Julia, and it then presented the appearance
+which we have sketched. He landed with a party and proceeded to
+examine the crater, in which he found a circular basin filled with
+reddish water, almost boiling hot, and fresh. This basin was nearly
+200 feet in diameter. There rose from the water bubbles of gas,
+which made it appear as if it were boiling. The water was not quite
+at the boiling point, however, yet the bubbles of gas were
+sufficiently hot to burn the fingers.
+
+[Illustration: Crater of Julia, or Graham's Island.]
+
+These bubbles rose from a great depth, and each, on bursting, which
+it did with a feeble report, threw out sand and cinders. At a short
+distance from the crater there rose sulphurous vapours, which
+deposited sulphur and salt. The loose dust and ashes forming the
+soil of the island were hot, and walking on them was difficult. The
+foregoing woodcut will give you an idea of the appearance which the
+crater presented to those visitors.
+
+In the following month of October nothing remained of this
+wonderful island but a hillock of sand and cinders; and at the end
+of six months it had quite vanished. Soundings taken a few years
+ago show ten feet of water over the spot, so that, although the
+island has disappeared, there is still a shoal left behind. This
+temporary volcano is best known in England under the name of
+Graham's Island; so called after an English naval officer of that
+name, who was the first to set foot on it, and who planted upon it
+the English flag, so claiming it for his sovereign. The Sicilians
+allege this to be the reason why it disappeared so soon--that it
+was in a hurry to escape from under the English yoke.
+
+Similar phenomena have been taking place during the past year,
+1866, in the Bay of Santorin, situated in the island of that name,
+which lies to the northward of Crete. There are several islands in
+the bay, all apparently of volcanic origin, and one of them was
+thrown up about three centuries before the beginning of the
+Christian era. Last year their number was increased by a series of
+eruptions similar in their attendant circumstances to those which
+accompanied the upheaval of Julia. The first warnings were given on
+the 30th of January 1866, by low underground rumblings, and slight
+movements of the ground at the south end of New Kammeni, one of the
+formerly upheaved islands in the bay. Next day these phenomena
+increased in violence, and quantities of gas bubbled up from the
+sea. On the 1st of February, reddish flames ascended from the
+water, and on the 2nd there rose, out of the harbour of Voulcano,
+an island, which was christened "George." The volcanic agitation
+was prolonged during February and March--the upheaval of other two
+islands being the result. Whether these additional islands will
+continue permanently above water remains to be seen.
+
+
+
+
+CHAPTER VI.
+
+Peak of Teneriffe--Its Crater--Eruption of Chahorra--Palma--Great
+Caldera--Lancerote--Great Eruption--Sudden Death--Fuego, Cape de
+Verde Islands--Cotopaxi--Its Appearance--Great Eruptive Force--
+Tunguragua--Great Eruption of Mud and Water--Fish thrown out--
+Quito--Its Overthrow--Pichinca--Humboldt's Ascent--Narrow Escape--
+Antisana--Sangay--Rancagua--Chillan--Masaya
+
+
+The Island of Teneriffe is celebrated for its magnificent snow-clad
+peak. On referring to the woodcut of this volcano at page 11, you
+will observe in what a sharp point the cone terminates, and how
+slender is the column of vapour at its summit. The crater at the
+top is comparatively small--its greatest diameter being 300, and
+its smallest 200 feet, while its depth is only about 100 feet. From
+this crater there has been no eruption since 1706, when the finest
+harbour in the island was destroyed. But from the side of the peak
+there rises a supplementary mountain named Chahorra, on the top of
+which there is also a crater, whence there was an eruption in 1798.
+So great was its violence, that masses of rock were thrown to a
+height of upwards of 3000 feet. In the neighbouring island of Palma
+there is a volcanic crater named the Great Caldera, whose depth is
+said to be upwards of 5000 feet.
+
+Almost due east of Palma, and much nearer the African coast, lies
+the Island of Lancerote, on which are a great many volcanic cones,
+arranged nearly in a straight line. These were for the most part
+formed by a long series of eruptions which took place during the
+years from 1730 to 1736. Such immense quantities of lava were
+poured forth in the course of those six years, that about a third
+of the surface of the island was covered by them, and many towns
+and villages were destroyed. St. Catalina, a populous and thriving
+town, was first overflowed by a lava-stream, and then a new crater
+burst forth on its very site, raising over it a hill 400 feet high.
+All the cattle in the island fell down dead in one day, and nearly
+about the same time--they were suffocated by deadly vapours that
+rose from the ground. The volcanic activity of this island was
+renewed in August 1824, when there was formed, near the port of
+Rescif, a new crater, which vomited forth such quantities of
+stones, ashes, and other volcanic matters, that in the short space
+of twenty-four hours they formed a hill of considerable height.
+
+The Cape de Verde Islands, lying to the south-westward of the
+Canaries, are also volcanic. In 1847 a volcano named Fuego,
+situated in one of them, after remaining at rest about fifty years,
+burst into fresh activity. No less than seven new vents were
+formed; and from these were poured forth great streams of lava,
+which wrought immense damage in the cultivated parts of the island.
+The inhabitants sustained great loss by the destruction of their
+cattle and crops.
+
+Passing over to the South American continent, we come to the range
+of the Andes, which contains numerous volcanoes. Among these the
+most conspicuous is Cotopaxi, the highest volcano in the world,
+situated in the territory of Quito. So perfect is the form of the
+cone, that it looks as if it had been turned in a lathe. Its
+coating of snow gives it a dazzling appearance, and so sharply is
+the snow-line defined that it seems almost as if the volcano-king
+wore a white night-cap instead of a crown.
+
+The eruptions of this mountain are rare. One of the greatest of
+them lasted for three years, and desolated an immense extent of
+country with floods of lava. On this occasion, it is said, columns
+of fire rose to the height of nearly 5000 feet, so great was the
+energy of the volcanic force.
+
+A little to the southward of Cotopaxi, but concealed from it by the
+intervening mass of Chimborazo, lies the volcano of Tunguragua,
+from which there was an extraordinary eruption in the year 1797,
+that proved very destructive to the cities in its neighbourhood.
+Indeed, so terrible was the convulsion of the ground, which lasted
+four minutes, that the cities of Riobamba and Quero were reduced to
+heaps of ruins. Then the base of Tunguragua was rent, and from
+numerous apertures there were poured out streams of water and mud,
+the latter gathering in the valleys to the depth of 600 feet. This
+mud spread itself far and wide, blocking up the channels of rivers,
+and forming lakes, which remained upwards of two months. But,
+strangest of all, quantities of dead fishes were found in the water
+which burst from the volcano. These fishes are supposed to have
+been bred in subterranean lakes contained in caverns in the
+interior of the mountain, considerably removed from the volcanic
+fires in the centre. It is probable that, when the rent was formed
+near the base, one of those caverns was broken open, and that the
+waters from it were discharged along with their finny inhabitants.
+
+Here is a picture of one of those fishes, which was taken by Baron
+Humboldt. When you see what a queer-looking fish it is, you will
+wonder the less at its having chosen so strange an abode.
+
+[Illustration: Pimelodus Cyclopum]
+
+Quito, the capital of the province of that name, is the highest of
+cities--being situated at an elevation of between nine and ten
+thousand feet above the level of the sea. It is built on a plain,
+lying on the flanks of the volcano Pichinca, of which a view is
+given in the annexed woodcut. Poor Quito has suffered severely from
+this dangerous neighbourhood; for, on the 22nd of March 1859, a
+violent shaking of the mountain laid the whole city in ruins.
+
+Pichinca, you will observe, has a most irregular outline, but very
+graceful withal. Instead of a single cone like Cotopaxi, it has a
+group of cones, some of which are very pointed. It has four
+principal summits, of which the most southerly contains the active
+crater. Here the celebrated traveller Baron Humboldt nearly lost
+his life. Having ascended the cone and approached the edge of the
+crater, he peered into the depths of the dark abyss, and there
+beheld the glowing lava boiling as if in a huge caldron. A thick
+mist coming on, he unwarily advanced to within a few feet of the
+rapid slope descending into the crater, and was within an ace of
+toppling over into the fiery gulf beneath. What a pity it would
+have been had he fallen in! We should have had no "Personal
+Narrative," no "Cosmos."
+
+[Illustration: Pichinca]
+
+There are in this region of South America other two great
+volcanoes, named Antisana and Sangay. The former has not been in
+action since 1718, but is remarkable for the immense beds of lava
+which it has amassed around it during its former eruptions. Sangay,
+again, has ever since 1728 been in a state of almost perpetual
+activity--in this respect resembling Stromboli, which, however, it
+far exceeds in height, its summit being nearly 18,000 feet above
+the level of the sea. The eruptions of this mountain are
+accompanied by loud explosions, which are heard at great distances,
+and they succeed each other with immense rapidity. The fumes
+emitted are sometimes gray, sometimes orange; and the matters
+ejected are cinders, dross, and spherical masses of stone. These
+last are often two feet in diameter, and in strong explosions as
+many as sixty of them may be thrown out at a time. They are glowing
+at a white heat, and for the most part they fall back into the vent
+of the crater. Sometimes, however, they alight on the edge of the
+cone--imparting to it a temporary brilliancy; but the mass of the
+cone, being composed of loose black cinders, has a most dismal
+aspect.
+
+Another very active South American volcano is Rancagua in Chili. It
+is, however, of moderate height, and thus in its general character
+resembles Stromboli, which it rivals in restlessness. Another of
+the volcanoes of Chili, named Chillan, which had long been in a
+state of repose, renewed its activity in November 1864. Its usually
+snow-clad summit became covered in a short time with a thick layer
+of volcanic ashes, which greatly altered its appearance. Streams of
+lava were also thrown out by the mountain on this occasion.
+
+There are several volcanoes in Central America. One of them, named
+Masaya, was very active during the sixteenth century. It is
+situated near the lake of Nicaragua, in the territory of that name.
+It was visited in 1529 by the Spanish historian Gonzales Fernando
+de Oviedo, from whose description it seems to have presented
+phenomena resembling those seen in the crater of Stromboli. "In its
+ordinary state," he says, "the surface of the lava, in the midst of
+which black scoriae are continually floating, remains several
+hundred feet below the edges of the water. But sometimes there is
+suddenly produced an ebullition so violent, that the lava rises
+almost to the very brim."
+
+
+
+
+CHAPTER VII.
+
+Jorullo--Great Monument--Jorullo's Estate--Interruption to his
+Quiet--His Estate Swells--Swallows Two Rivers--Throws up Ovens--
+Becomes a Burning Mountain--Popocatepetl--Spanish Ascents--Orizaba
+--Muller's Ascent--Morne-Garou--Pelée---La Soufriere
+
+
+What a fortunate man was Mr. Jorullo! Old Cheops, king of Egypt,
+spent vast sums of money, many long years, and the labour of
+myriads of his subjects, in erecting the Great Pyramid as a
+monument to his memory. But Mr. Jorullo, without his having to lay
+down a single Mexican dollar, and without any labour, either of his
+own or of his servants, had a magnificent monument raised to his
+memory in a single night. Jorullo's monument, too, is far bigger
+than the pyramid of Cheops--being nearly four times the height, and
+occupying a much larger extent of ground. Whether it will last as
+long as the pyramid has done, time only can show.
+
+You would doubtless like to know how this great monument was
+reared. Here is the story:--Don Pedro di Jorullo was a Mexican
+gentleman who lived about the middle of the last century. He was a
+landed proprietor--the owner of a nice little farm of great
+fertility, situated to the westward of the city of Mexico, and
+about ninety miles from the coast of the Pacific Ocean. The ground
+was well watered by artificial means, and produced abundant crops
+of indigo and sugar-cane. Thus Mr. Jorullo was a very thriving
+well-to-do sort of man.
+
+[Illustration: Jorullo]
+
+This gentleman's prosperity continued without interruption till the
+month of June 1759, when, to the great alarm of his servants
+dwelling on the estate, strange underground rumblings were heard,
+accompanied by frequent shakings of the ground. These continued for
+nearly two months; but at the end of that time all became quiet
+again, and Mr. Jorullo's servants slept in fancied security. On the
+night of the 28th of September, however, their slumbers were
+suddenly broken by a return of the horrible underground rumblings-
+thundering more loudly than before. The next night, these
+subterranean thunders became so loud, that the Indian servants
+started from their beds, and fled in terror to the mountains in the
+neighbourhood. Gazing thence, after day had dawned, they beheld to
+their astonishment that a tract of ground from three to four square
+miles in extent, with their master's farm in the middle of it, had
+been upheaved in the shape of an inflated bladder. At the edges
+this singular elevation rises only about thirty-nine feet above the
+old level of the plain; but so great is the general convexity of
+the mound, that towards the centre it swells up to five hundred and
+twenty-four feet above the original level.
+
+The Indians affirmed that they saw flames issue from the ground
+throughout an extent of more than half a square league, while
+fragments of burning rocks were thrown to enormous heights. Thick
+clouds of ashes rose into the air, illuminated by glowing fires
+beneath; and the surface of the ground seemed to swell into
+billows, like those of a tempestuous sea. Into the vast burning
+chasms, whence these ejections were thrown, two rivers plunged in
+cataracts; but the water only increased the violence of the
+eruption. It was thrown into steam with explosive force, and great
+quantities of mud and balls of basalt were ejected. On the surface
+of the swollen mound there were formed thousands of small cones,
+from six to ten feet in height, and sending forth steam to heights
+varying from twenty to thirty feet.
+
+Out of a chasm in the midst of these cones, or ovens, as the
+natives call them, there rose six large masses, the highest of
+which is sixteen hundred feet in height, and constitutes the
+volcano of Jorullo. The eruptions of this central volcano continued
+till February 1760 with extreme violence--the crater throwing out
+large quantities of lava; but in the succeeding years it became
+less turbulent in its activity. It still, however, continues to
+burn; and the mountain emits from the wide crater at its summit
+several jets of vapour. The foregoing woodcut gives a view of this
+volcano, and of the little steaming ovens which stud the whole
+ground around it, giving it at a distance the appearance of the sea
+in a storm. And now confess that Mr. Jorullo's monument is far
+grander than the pyramid of Cheops. Surely the loss of his farm was
+amply compensated to him, by the perpetuation of his memory and his
+name, through the rearing of such a marvellous cenotaph.
+
+For a long time after the first eruption, the ground for a great
+distance round the volcano was too hot to be habitable or capable
+of cultivation. It is now, however, so much cooled down, that it is
+once more covered with vegetation; and even some small portions of
+the raised ground containing the ovens have been again brought
+under culture.
+
+Besides this volcano, so recent in its origin, Mexico contains
+other five--Orizaba, Toluca, Tuxtla, Popocatepetl, and Colima. What
+is rather remarkable, these five, together with Jorullo, all lie
+nearly in a straight line running east and west. The tracts of
+country which these volcanoes have desolated with their lavas are
+called by the Mexicans the "Malpays."
+
+The most remarkable of these mountains is Popocatepetl. Although it
+has long remained in comparative quiet, it was very active at the
+time of the Spanish invasion under Cortés. Of the first approach of
+the Spaniards to this volcano, and of the attempts made by some of
+them to climb to the top, Mr. Prescott, in his history of the
+conquest of Mexico, gives the following graphic account:--
+
+"They were passing between two of the highest mountains on the
+North American continent, Popocatepetl, 'the hill that smokes' and
+Iztaccihuatl, or 'white woman;' a name suggested, doubtless, by the
+bright robe of snow spread over its broad and broken surface. A
+puerile superstition of the Indians regarded these celebrated
+mountains as gods, and Iztaccihuatl as the wife of her more
+formidable neighbour. A tradition of a higher character described
+the northern volcano as the abode of the departed spirits of wicked
+rulers, whose fiery agonies in their prison-house caused the
+fearful bellowings and convulsions in times of eruption. It was the
+classic fable of antiquity. These superstitious legends had
+invested the mountain with a mysterious horror, that made the
+natives shrink from attempting its ascent, which, indeed, was, from
+natural causes, a work of incredible difficulty.
+
+"The great _volcan_, as Popocatepetl was called, rose to the
+enormous height of 17,852 feet above the level of the sea; more
+than 2000 feet above the 'monarch of mountains'--the highest
+elevation in Europe. During the present century it has rarely given
+evidence of its volcanic origin, and 'the hill that smokes' has
+almost forfeited its claim to the appellation. But at the time of
+the conquest it was frequently in a state of activity, and raged
+with uncommon fury while the Spaniards were at Tlascala; an evil
+omen, it was thought, for the natives of Anahuac. Its head,
+gathered into a regular cone by the deposit of successive
+eruptions, wore the usual form of volcanic mountains, when not
+disturbed by the falling in of the crater. Soaring towards the
+skies, with its silver sheet of everlasting snow, it was seen far
+and wide over the broad plains of Mexico and Puebla; the first
+object which the morning sun greeted in his rising, the last where
+his evening rays were seen to linger, shedding a glorious
+effulgence over its head, that contrasted strikingly with the
+ruinous waste of sand and lava immediately below, and the deep
+fringe of funereal pines that shrouded its base.
+
+"The mysterious terrors which hung over the spot. and the wild love
+of adventure, made some of the Spanish cavaliers desirous to
+attempt the ascent, which the natives declared no man could
+accomplish and live. Cortés encouraged them in the enterprise,
+willing to show the Indians that no achievement was above the
+dauntless daring of his followers. One of his captains,
+accordingly, Diego Ordaz, with nine Spaniards, and several
+Tlascalans, encouraged by their example, undertook the ascent. It
+was attended with more difficulty than had been anticipated.
+
+"The lower region was clothed with a dense forest, so thickly
+matted, that in some places it was scarcely possible to penetrate
+it. It grew thinner, however, as they advanced, dwindling by
+degrees into a straggling stunted vegetation, till, at the height
+of somewhat more than 13,000 feet, it faded away altogether. The
+Indians, who had held on thus far; intimidated by the strange
+subterraneous sounds of the volcano, even then in a state of
+combustion, now left them. The track opened on a black surface of
+glazed volcanic sand and of lava, the broken fragments of which,
+arrested in its boiling progress in a thousand fantastic forms,
+opposed continual impediments to their advance. Amidst these, one
+huge rock, the Pico del Fraile, a conspicuous object from below,
+rose to the perpendicular height of 150 feet, compelling them to
+take a wide circuit. They soon came to the limits of perpetual
+snow, where new difficulties presented themselves, as the
+treacherous ice gave an imperfect footing, and a false step might
+precipitate them into the frozen chasms that yawned around. To
+increase their distress, respiration in these aerial regions became
+so difficult, that every effort was attended with sharp pains in
+the head and limbs. Still they pressed on, till, drawing nearer the
+crater, such volumes of smoke, sparks, and cinders were belched
+forth from its burning entrails, and driven down the sides of the
+mountain, as nearly suffocated and blinded them. It was too much
+even for their hardy frames to endure, and, however reluctantly,
+they were compelled to abandon the attempt on the eve of its
+completion. They brought back some huge icicles--a curious sight in
+those tropical regions--as a trophy of their achievement, which,
+however imperfect, was sufficient to strike the minds of the
+natives with wonder, by showing that with the Spaniards the most
+appalling and mysterious perils were only as pastimes. The
+undertaking was eminently characteristic of the bold spirit of the
+cavalier of that day, who, not content with the dangers that lay in
+his path, seemed to court them from the mere Quixotic love of
+adventure. A report of the affair was transmitted to the Emperor
+Charles V.; and the family of Ordaz was allowed to commemorate the
+exploit by assuming a burning mountain on their escutcheon.
+
+"The general was not satisfied with the result. Two years after he
+sent up another party, under Francisco Montano, a cavalier of
+determined resolution. The object was to obtain sulphur to assist
+in making gunpowder for the army. The mountain was quiet at the
+time, and the expedition was attended with better success. The
+Spaniards, five in-number, climbed to the very edge of the crater,
+which presented an irregular ellipse at its mouth, more than a
+league in circumference. Its depth might be from 800 to 1000 feet.
+A lurid flame burned gloomily at the bottom, sending up a
+sulphureous steam, which, cooling as it rose, was precipitated on
+the sides of the cavity. The party cast lots, and it fell on
+Montano himself to descend in a basket into this hideous abyss,
+into which he was lowered by his companions to the depth of 400
+feet! This was repeated several times, till the adventurous
+cavalier had collected a sufficient quantity of sulphur for the
+wants of the army."
+
+The more tranquil state of the volcano in modern times having
+rendered the summit no longer so difficult of access as it was in
+those days, the ascent has been several times achieved--twice in
+1827, and again in 1833 and 1834. The crater is now a large oval
+basin with precipitous walls, composed of beds of lava, of which
+some are black, others of a pale rose tint. At the bottom of the
+crater, which is nearly flat, are several conical vents, whence are
+continually issuing vapours of variable colour, red, yellow, or
+white. The beds of sulphur deposited in this crater are worked for
+economical purposes. Two snowy peaks tower above its walls.
+
+Not less magnificent in its proportions is the volcano of Orizaba,
+which is nearly of the same height as Popocatepetl. It was very
+active about the middle of the sixteenth century, having had
+several great eruptions between 1545 and 1560; but since then it
+has sunk into comparative repose. This mountain was ascended by
+Baron Muller in 1856. A first attempt proved unsuccessful; but by
+passing a night in a grotto near the limit of perpetual snow, he
+was able on the following day, after a toilsome ascent, to reach
+the edge of the crater--not, however, till near sunset. His
+experiences, and the scene which was presented to his wondering
+gaze, he describes in the following terms:--
+
+"I have achieved my purpose, and joy banishes all my griefs, but
+only for a moment; suddenly I fell to the ground, and a stream of
+blood gushed from my mouth.
+
+"On recovering, I found myself still close to the crater, and I
+then summoned all my strength to gaze and observe as much as
+possible. My pen cannot describe either the aspect of those
+regions, or the impressions they produced on me. Here seemed to be
+the gate of the nether world, enclosing darkness and horror. What
+terrible power must have been required to raise and shiver such
+enormous masses, to melt them and pile them up like towers, at the
+very moment of their cooling and acquiring their actual forms!
+
+"A yellow crust of sulphur coats in several places the internal
+walls, and from the bottom rise several volcanic cones. The soil of
+the crater, so far as I could see, was covered with snow,
+consequently not at all warm. The Indians however affirmed that, at
+several points, a hot air issues from crevices in the rocks.
+Although I could not verify their statement, it seemed to me
+probable; for I have often observed similar phenomena in
+Popocatepetl.
+
+"My original intention of passing the night on the crater had for
+overpowering reasons become impracticable. The twilight which, in
+this latitude, as every one knows, is extremely short, having
+already begun, it was necessary to prepare for our return. The two
+Indians rolled together the straw mats which they had brought, and
+bent them in front so as to form a sort of sledge. We sat down upon
+these, and stretching out our legs, allowed ourselves to glide down
+on this vehicle. The rapidity with which we were precipitated
+increased to such a degree, that our descent was rather like being
+shot through the air, than any other mode of locomotion. In a few
+minutes we dashed over a space which it had taken us five hours to
+climb."
+
+There are several of the West Indian islands of volcanic origin;
+and three of them--St. Vincent, Martinique, and Guadaloupe--contain
+active volcanoes. The most remarkable is the volcano of Morne-
+Garou, in St. Vincent, the eruptions from which have been
+particularly violent. In 1812 the ashes which it threw out were so
+great in quantity, and projected to so vast a height, that they
+were carried to a distance of two hundred miles in the teeth of the
+trade-wind. From Mount Pelée, in Martinique, there was an eruption
+in August 1851. La Soufriere, the volcano in Guadaloupe, is said to
+have been cleft in twain during an earthquake. Its activity has
+long been in a subdued state; but it is remarkable for its deposits
+of sulphur.
+
+
+
+
+CHAPTER VIII.
+
+Hawaii, Sandwich Islands--Crater of Kilauea--Its awful Aspect--
+Fiery Lake and Islands--Jets of Lava--Depth of Crater and Surface
+of Lake--Bank of Sulphur--Curious Rainbow--Mouna-Kaah and Mouna-
+Loa--Eruption of the Latter in 1840--Recent Eruption--Great Jet and
+Torrent of Lava--Burning of the Forests--Great Whirlwinds--
+Underground Explosions--Other Volcanoes in the Pacific.
+
+
+Hawaii is well known in history as being the island where the
+celebrated navigator Captain Cook was killed. The name used to be
+written Owhyhee; but a better apprehension of the native
+pronunciation has led to its being altered into Hawaii. No one who
+visits it in the present day need be afraid of sharing the fate of
+poor Captain Cook; for the descendants of the savages who, in his
+time, inhabited the island, have now, through the labours of
+Christian missionaries, become a very decent sort of quiet, well-
+behaved Christian people.
+
+Hawaii, which is the largest of a group called the Sandwich
+Islands, can boast of the greatest volcanic crater in the world. It
+is called sometimes Kirauea, sometimes Kilauea; for the natives
+seem not very particular about the pronunciation of their _l_
+and their _r_; but where one uses _l_ another as
+pertinaciously employs _r_, while a third set use a sound
+between the two, as you may have heard some people do at home.
+Situated on the lower slopes of a lofty mountain called Mouna-Roa,
+or Loa (for there is the same dubiety about the _l_ and the
+_r_ here as in the former case), the crater of Kilauea is a
+vast plain between fifteen and sixteen miles in circumference, and
+sunk below the level of its borders to a depth varying from two
+hundred to four hundred feet--the walls of rock enclosing it being
+for the most part precipitous. The surface of the ground is very
+uneven, being strown with huge stones and masses of volcanic rock,
+and it sounds hollow under the tramp of the foot.
+
+Towards the centre of the plain is a much deeper depression. Those
+who have ventured to approach it, and look down, describe it as an
+awful gulf, about eight hundred feet in depth, and presenting a
+most gloomy and dismal aspect. The bottom is covered with molten
+lava, forming a great lake of fire, which is continually boiling
+violently, and whose fiery billows exhibit a wild terrific
+appearance. The shape of the lake resembles the crescent moon; its
+length is estimated at about two miles, and its greatest breadth at
+about one mile. It has numerous conical islands scattered round the
+edge, or in the lake itself, each of them being a little
+subordinate crater. Some of them are continually sending out
+columns of gray vapour; while from a few others shoots up what
+resembles flame. It is, probably, only the bright glare of the lava
+they contain, reflected upwards. Several of these conical islands
+are always belching forth from their mouths glowing streams of
+lava, which roll in fiery torrents down their black and rugged
+sides into the boiling lake below. They are said sometimes to throw
+up jets of lava to the height of upwards of sixty feet. The
+foregoing woodcut can convey only an imperfect idea of this immense
+crater.
+
+[Illustration: Crater of Kilauea]
+
+The outer margin of the gulf all round is nearly perpendicular. The
+height of the bounding cliffs is estimated at about four hundred
+feet above a black horizontal ledge of hardened lava, which
+completely encircles it, and beyond which there is a gradual slope
+down into the burning lake. The surface of the molten lava is at
+present between three and four hundred feet below this horizontal
+ledge; but the lava is said sometimes to rise quite up to this
+level, and to force its way out by forming an opening in the side
+of the mountain, whence it flows down to the sea. An eruption of
+this kind took place in 1859. On one side of the margin of the lake
+there is a long pale yellow streak formed by a bank of sulphur. The
+faces of the rocks composing the outer walls of the crater have a
+pale ashy gray appearance, supposed to be due to the action of the
+sulphurous vapours. The surface of the plain itself is much rent by
+fissures. It is said that the glare from the molten lava in the
+lake is so great as to form rainbows on the passing rain-clouds.
+
+The entire Island of Hawaii is of volcanic origin; and besides this
+great crater it contains two other lofty mountains, whose summits
+are covered with snow, and whose height is estimated at fifteen or
+sixteen thousand feet above the level of the sea. The one is named
+Mouna-Kaah or Keah, the other is Mouna-Loa--the same on whose lower
+flanks the crater of Kilauea is situated. Mouna-Kaah has long been
+in a state of repose. So also was Mouna-Loa up to 1840, when it
+burst forth with great fury, and it has continued more or less in a
+state of activity ever since. There has been a grand eruption very
+lately, said by the natives to have been the greatest of any on
+record.
+
+A new crater opened near the top, at a height of about ten thousand
+feet, and for three days a flood of lava poured down the north-
+eastern slope. After a pause of about thirty-six hours, there was
+opened on the eastern slope, about half way down the mountain,
+another crater, whence there rose an immense jet of liquid lava,
+which attained a height of about a thousand feet, and had a
+diameter of about a hundred feet. This jet was sustained for twenty
+days and nights; but during that time its height varied from the
+extreme limit of a thousand, down to about a hundred feet. The play
+of this fiery fountain was accompanied by explosions so loud as to
+be heard at the distance of forty miles. Nothing could surpass the
+awful grandeur of this jet, which was at a white heat when it
+issued from its source, but, cooling as it ascended into the air,
+it became of a bright blood red, which, as the liquid fell,
+deepened into crimson.
+
+In a few days there was raised around this crater a cone of about
+three hundred feet in height, composed of the looser materials
+thrown out along with the lava. This cone continued to glow with
+intense heat, throwing out occasional flashes. The base of this
+cone eventually acquired a circumference of about a mile. But the
+fountain itself formed a river of glowing lava, which rushed and
+bounded with the speed of a torrent down the sides of the mountain,
+filling up ravines and dashing over precipices, until it reached
+the forests at the foot of the volcano. These burst into flames at
+the approach of the fiery torrent, sending up volumes of smoke and
+steam high into the air. The light from the burning forests and the
+lava together was so intense as to turn night into day, and was
+seen by mariners at a distance of nearly two hundred miles.
+
+During the day the air throughout a vast extent was filled with a
+murky haze, through which the sun showed only a pallid glimmer.
+Smoke, steam, ashes, and cinders were tossed into the air and
+whirled about by fierce winds--sometimes spreading out like a fan,
+but every moment changing both their form and colour. The stream of
+lava from the fountain flowed to a distance of about thirty-five
+miles. The scene was altogether terrific--the fierce red glare of
+the lava--the flames from the burning trees--the great volumes of
+smoke and steam--the loud underground explosions and thunderings,--
+all combined to overpower the senses, and fill the mind with
+indescribable awe.
+
+A remarkable volcanic chain runs along the northern and western
+margins of the Pacific Ocean. It embraces the Aleutian Islands, the
+peninsula of Kamtschatka, the Kurile, the Japanese, and the
+Philippine Islands. The most interesting are the volcanoes of
+Kamtschatka, in which there is an oft-renewed struggle between
+opposing forces--the snow and glaciers predominating for a while,
+to be in their turn overpowered by torrents of liquid fire.
+
+
+
+
+CHAPTER IX.
+
+Atolls, or Coral Islands--Their strange Appearance--Their
+Connexion with Volcanoes--Their Mode of Formation--Antarctic
+Volcanoes--Diatomaceous Deposits
+
+
+To the southward of the Sandwich Islands, on the other side of the
+equator, there is a large group of islands in the Pacific, which
+have a very peculiar appearance. They are called Atolls or Coral
+Islands. Although not exactly of volcanic origin, yet the manner in
+which they are formed has some connexion with submarine volcanic
+action.
+
+An atoll consists essentially of a ring of coral rocks but little
+elevated above the level of the sea, and having in its centre a
+lagoon or salt-water lake, which generally communicates by a deep
+narrow channel with the sea. The ring of rocks is flat on the
+surface, which is composed of friable soil, and sustains a
+luxuriant vegetation, chiefly of cocoa-nut palms. It is seldom more
+than half a mile in breadth between the sea and lagoon, sometimes
+only three or four hundred yards. The outer margin of the ring is
+the highest, and it slopes gradually down towards the lagoon; but
+on the outside of the ledge of rocks is a beach of dazzling
+whiteness, composed of powdered and broken coral and shells. The
+appearance they present is thus not less beautiful than singular.
+Some of these islands are of large size, from thirty to fifty miles
+long, and from twenty to thirty broad, but they are in general
+considerably smaller. Their most frequent form is either round or
+oval. The rocks composing them are all formed by different species
+of coral. The animal which constructs them is of the polyp tribe,
+and so small that it can be seen only under the higher powers of
+the microscope. It multiplies by means of buds like those of a
+tree, the individuals all combining to form a composite stony mass,
+which is called a polypidom. A number of such polypidoms growing
+close together form a coral reef. See woodcuts.
+
+[Illustration: Coral]
+
+[Illustration: Coral Polyp]
+
+It was at one time supposed that these coral reefs were erected on
+the edges of the craters of submarine volcanoes, an opinion to
+which their annular form, and the lagoon in the centre, lent some
+countenance; but the vast size of some of them, united to several
+other particulars connected with them, threw great doubts over this
+supposition.
+
+More recently it has been shown by Mr. Darwin that, while volcanic
+agency does perform a part in their formation, it is different from
+what had been formerly imagined. His supposition is, that these
+coral reefs were built round the coasts of islands which had once
+stood very much higher above water than they do now. He conceives
+that the bottom of the sea under them being very volcanic, and
+containing large collections of molten lava beneath a thin solid
+crust, the islands have gradually sunk down into the lava, until
+their central parts have become covered with a considerable depth
+of water. The central parts thus submerged, he imagines, form the
+lagoons in the middle of the islands, while the ring of coral reefs
+has gradually grown upwards, as the ground on which it rested sank
+downwards.
+
+[Illustration: Coral Reef.]
+
+The corals thus rise to near the surface, but immediately on their
+being uncovered by the water they die, and the reef ceases to grow.
+Then the waves by their action break the upper part of it into
+pieces, which thus become heaped up by degrees on the remainder,
+until the mass attain so great a height that the sea can no longer
+wash over it. Thus the curious ring of land is gradually formed,
+and affords a nutritive soil, in which cocoa-nuts, on being cast
+ashore, germinate and grow to be large trees. Other seeds, wafted
+by the waves or carried by birds, also begin to grow, until the
+whole surface becomes covered with vegetation. Then comes man and
+builds his habitation upon those fertile spots, and finds in them
+an agreeable and convenient abode, well suited to those who are
+accustomed to live by fishing and other simple means.
+
+You will thus perceive that the connexion between the atoll and the
+volcano consists in this--that while the coral builds up the reef,
+the volcano beneath ingulfs the island and causes it to sink down.
+In some instances, however, the volcano, after a while, reverses
+its action, and raises up the island with the reef upon it. In such
+cases, the coral reefs are seen standing out of the water, forming
+perpendicular cliffs several hundred feet in height. Then also the
+interior of the island becomes once more dry land, and that, too,
+of great fertility.
+
+[Illustration: Mount Erebus.]
+
+Almost due south of that region, in the Pacific, where the coral
+islands abound, but at a great distance from them, and considerably
+within the limits of the Antarctic zone, lies South Victoria. Here,
+in lat. 76 degrees S., Captain Ross discovered, in 1841, two
+volcanoes, which he called Erebus and Terror, after the names of
+his two ships. Of the former, which is the higher of the two, a
+view is given in the annexed woodcut. It is covered with perpetual
+snow from the bottom even to the tip of the summit. Nevertheless,
+it is continually sending forth vast columns of vapour, which glow
+with the reflection of the white hot lava beneath. These vapours
+ascend to a great height, more than two thousand feet above the top
+of the cone, which is itself twelve thousand feet above the level
+of the sea.
+
+There is found in these frozen regions a remarkable botanical
+curiosity, having a certain connexion with volcanoes. The waters of
+the ocean, all along the borders of the icy barrier, produce in
+amazing abundance the family of water-plants named Diatomaceae. The
+Diatoms are so called from their faculty of multiplying themselves
+indefinitely by splitting into two; and so rapidly is this process
+performed, that in a month a single diatom may produce a thousand
+millions. The quantity found in the Antarctic regions is so immense
+that, between the parallels of 60 degrees and 80 degrees of south
+latitude, they stain the whole surface of the sea of a pale olive-
+brown tint. These plants, which are so minute as to be individually
+invisible, save under the higher powers of the microscope, have the
+curious property of encrusting themselves with a sheath, or shell,
+of pure silica. These shells remain after the death of the plant,
+and are as indestructible as flint. They are marvellous objects,
+both as respects the elegance of their forms and the beauty of
+their markings. So great is the accumulation of these shells at the
+bottom of the sea, that they have formed an immense bank 400 miles
+in length by 120 in breadth, between the 76th and 78th degrees of
+south latitude. One portion of this bank rests on the coast at the
+foot of Mount Erebus.
+
+Now, it is remarkable that these microscopic shells of Diatoms are
+not unfrequently found in the ejections of volcanoes; while it is
+generally supposed that, in the case of those situated near the
+sea, eruptions are caused by the formation of explosive steam
+consequent on the access of sea-water to the reservoirs of molten
+lava lying underground. The proximity of this Diatomaceous bed to
+Mount Erebus would easily explain how these minute shells might be
+found abundant in the fine dust ejected from that volcano.
+
+
+
+
+CHAPTER X.
+
+Volcanoes of Java--Papandayang--Mountain Ingulfed--Great
+Destruction of Life and Property--Galoen-gong--Destructive
+Eruption--Mount Merapia--Great Eruption, with Hurricane--Another,
+very destructive--Mud Volcano Crater of Tankuban-Prahu--Island of
+Sumbáwa--Volcano of Tomboro--Terrific Eruption--Timor--A Volcano
+quenches itself--Cleaving of Mount Machian--Sangir--Destructive
+Eruption--Bourbon.
+
+
+One of the most marvellous volcanic regions in the world is that
+composed of the islands of the Malayan Archipelago in the Indian
+Ocean. They form a chain stretching from east to west, but curving
+up towards the north at the western extremity. The most easterly of
+the chain is Timor, the most westerly Sumatra.
+
+The most interesting of the group is Java, which is almost entirely
+of volcanic origin, and contains no less than thirty-eight
+mountains of that conical form which indicates their having at one
+time or other been active volcanoes. Only a few of them, however,
+have been in activity in more recent times. The most remarkable
+eruption was that of the mountain named Papandayang, which occurred
+in 1772. During this convulsion the greater part of the mountain,
+which was formerly one of the largest in the island, was completely
+swallowed up in some great underground gulf.
+
+On the night between the 11th and 12th of August of that year, the
+mountain appeared to be wholly enveloped in a remarkable luminous
+cloud. The inhabitants fled in consternation; but before they could
+all escape, the mountain began to totter, and the greater part of
+it tumbled down and disappeared. The crash with which it fell was
+dreadful, the noise resembling the discharge of volleys of
+artillery. Besides that part of the mountain which thus fell in, a
+large extent of ground in its neighbourhood was ingulfed. The space
+measured fifteen miles in length and six in breadth. The ground for
+many miles round this space was covered with immense quantities of
+ashes, stones, cinders, and other substances thrown out by the
+volcano. These were, on many parts of the surface, accumulated to
+the height of three feet; and even at the end of six weeks, the
+layers thus deposited retained so much heat as to render the
+mountain inaccessible. By this dreadful occurrence forty villages
+were destroyed, some ingulfed with the ground on which they stood,
+others buried under the loose materials which had been ejected. Not
+far short of three thousand of the inhabitants perished.
+
+Another of the volcanoes of Java, called Galoen-gong, burst into
+eruption in 1822, commencing with a terrible explosion of stones,
+ashes, &c., followed by a stream of hot mud, which overspread a
+large tract of ground. This eruption proved still more fatal to
+human life, about four thousand persons having been destroyed.
+
+So lately as September 1849, Mount Merapia, another volcano in this
+island, which had been supposed to be quite extinct, burst forth
+into an eruption, which lasted three days. It was accompanied by a
+violent hurricane. The bed of a river was filled up by the matter
+thrown out from the crater, and the destruction of property in
+crops, &c., was immense. Fortunately the inhabitants succeeded in
+making their escape, so that no lives were lost. A second eruption
+of this mountain however, in January 1864, was more disastrous,
+three hundred and fifty people having perished.
+
+Java likewise contains a remarkable mud volcano. When viewed from a
+distance, there are seen to rise from it large volumes of vapour,
+like the spray from the billows dashing against a rocky shore, and
+there is heard a loud noise like distant thunder. On a nearer
+approach, the source of these phenomena is seen to be a
+hemispherical mound of black earth mixed with water, about sixteen
+feet in diameter, and which at intervals of a few seconds is pushed
+upwards by a force acting from beneath to a height of between
+twenty and thirty feet. It then suddenly explodes with a loud
+noise, scattering in every direction a quantity of black mud, which
+has a strong pungent smell resembling that of coal-tar, and is
+considerably warmer than the air. With the mud thus thrown out
+there has been formed around the mound a large perfectly level and
+nearly circular plain, about half a mile in circumference. The
+water mixed with the mud is salt, and the salt is separated from it
+by evaporation for economical purposes. During the rainy season the
+action of this mud volcano becomes more violent, the explosions are
+louder, and the mud is thrown to a greater height.
+
+The crater of Tangkuban-Prahu, another of the volcanoes of Java,
+presents a remarkable appearance. On approaching its edge, nothing
+is seen but an abyss, from which dense clouds of vapour continually
+arise, with hideous sounds, like the steam rushing from the open
+valves of hundreds of steam-engines. This great abyss consists
+really of two craters, separated the one from the other by a narrow
+ridge of rock, to which it is possible to descend and view them
+both. Each of them is elliptical in form, and surrounded by a
+crater-wall. That of the western, which the natives call the
+poison-crater, is a rapid slope nearly a thousand feet in depth,
+and is densely covered with brushwood almost to the bottom. The
+flat floor of this deep basin is continually sending out vapours,
+and in its centre is a pool of boiling water of a sulphur yellow
+colour. The floor itself is nothing but a crust of sulphur full of
+rents and holes, whence vapours constantly arise. This crust covers
+a surface of boiling hot bitter water, and by breaking it beautiful
+crystals of sulphur may be obtained.
+
+The eastern is called by the natives the king's-crater; its walls
+are only between five and six hundred feet in depth, and are
+perfectly bare from top to bottom. The surfaces of the rocks
+composing them are grayish white, an effect produced upon them by
+the action of the vapours, to which they are continually exposed.
+The bottom of this crater consists of mud mixed with sulphur; but
+round the edges are some stones and hard masses. These are the
+remnants of an eruption which took place from this crater in 1846,
+when there was thrown up a great mass of sulphurous boiling mud,
+accompanied by quantities of sand and stones. This mountain,
+therefore, seems to be also more of the nature of a mud volcano,
+than of one which throws out burning lava.
+
+Nearly in a right line to the eastward of Java lies the Island of
+Sumbáwa, in which stands the volcano of Tomboro, the most violent
+in its eruptions of any in the world. One of the most remarkable
+occurred in the year 1815, beginning on the 5th of April and
+continuing till the middle of July. Its effects were felt over an
+immense tract of country, embracing the Molucca Islands, Java, and
+portions of Celebes, Sumatra, and Borneo. The concussions produced
+by its explosions were sensible at a distance of a thousand miles
+all round; and their sound is said to have been heard even at so
+great a distance as seventeen hundred miles. In Java the day was
+darkened by clouds of ashes, thrown from the mountain to that great
+distance (three hundred miles), and the houses, streets, and
+fields, were covered to the depth of several inches with the ashes
+that fell from the air. So great was the quantity of ashes ejected,
+that the roofs of houses forty miles distant from the volcano were
+broken in by their weight. The effects of the eruption extended
+even to the western coasts of Sumatra, where masses of pumice were
+seen floating on the surface of the sea, several feet in thickness
+and many miles in extent.
+
+From the crater itself there were seen to ascend three fiery
+columns, which, after soaring to a great height, appeared to unite
+in a confused manner at their tops. Ere long, the whole of the side
+of the mountain next the village of Sang'ir seemed like one vast
+body of liquid fire. The glare was terrific, until towards evening,
+when it became partly obscured by the vast quantities of dust,
+ashes, stones, and cinders thrown up from the crater. Between nine
+and ten o'clock at night the ashes and stones began to fall upon
+the village of Sang'ir, and all round the neighbourhood of the
+mountain. Then arose a dreadful whirlwind, which blew down nearly
+every house in the village, tossing the roofs and lighter parts
+high into the air. In the neighbouring sea-port the effects were
+even more violent, the largest trees having been torn up by the
+roots and whirled aloft. Before such a furious tempest no living
+thing could stand. Men, horses, and cattle were whirled into the
+air like so much chaff, and then dashed violently down on the
+ground. The sea rose nearly twelve feet above the highest tide-
+mark, sweeping away houses, trees, everything within its reach.
+
+This whirlwind lasted about an hour, and then commenced the awful
+internal thunderings of the mountain. These continued with scarcely
+any intermission until the 11th of July, when they became more
+moderate, the intervals between them gradually increasing till the
+15th of July, when they ceased. Almost all the villages for a long
+distance round the mountain were destroyed; and it is computed that
+nearly twelve thousand persons perished. By far the greatest part
+of this destruction was wrought by the violence of the whirlwind
+which accompanied the eruption.
+
+Considerably to the eastward of Sumbáwa lies the Island of Timor,
+in which there was for a long time a volcanic peak, whose perpetual
+fires served as a lighthouse to mariners navigating those seas. But
+in the year 1637 there took place a great eruption of the mountain,
+which ended in its being gobbled up whole and entire, leaving
+nothing behind it but a lake, in which its fires were quenched, and
+which now occupies its place.
+
+To the north of Timor lie the Molucca Islands, several of which are
+volcanic. In one of them, named Machian, there occurred in the year
+1646 an extraordinary event. A mountain was rent from top to
+bottom, sending out great columns of fire and dense vapours. The
+two parts now remain two distinct mountains.
+
+In the Island of Sangir, another of the Moluccas, there was a
+violent eruption in March 1856. A large portion of the mountain
+fell down, and tremendous floods of water issued forth. The
+destruction that ensued was dreadful, upwards of two thousand
+persons having perished.
+
+In another part of the Indian Ocean, near Madagascar, lies the
+little Isle of Bourbon, containing the volcano Salazes, which
+occasionally throws out the curious thready substance already
+mentioned, so strongly resembling spun glass.
+
+
+
+
+CHAPTER XI.
+
+Mud and Air Volcanoes--Luss--Macaluba--Taman--Korabetoff--New
+Island in the Sea of Azof--Jokmali--Fires of Baku--Mud Volcano in
+Flank of Etna--Air Volcanoes of Turbaco, Cartagena, and Galera-
+Zamba.
+
+
+The curious mud volcano in the Island of Java, described in
+the preceding chapter, although presenting some peculiar features,
+is not the only one of the kind in the world. Mud, as you have
+learned, is often thrown out in great quantities, along with
+boiling water, even by true volcanoes, which at other times eject
+ashes and lava. But there are some volcanoes that never throw out
+anything else than mud and water, gas and steam. Such are called
+mud volcanoes or salses.
+
+The most remarkable assemblage of mud volcanoes in the world exists
+in the district of Luss, lying at the south-east corner of
+Beloochistan. They extend over a very large area, and are
+exceedingly numerous. The cone of one of them is no less than four
+hundred feet high, and the crater at the top is ninety feet in
+diameter. The mud in the crater is quite liquid, and is constantly
+disturbed by bubbles of gas, and occasionally by jets of the mud
+itself.
+
+More familiarly known is the mud volcano of Macaluba, near
+Girgenti, in Sicily. It is situated in a country much impregnated
+with sulphur and other inflammable matters. The top of the hill is
+covered with dry clay, in which are numerous basins full of warmish
+water mixed with mud and bitumen. From these small craters bubbles
+of gas arise from time to time; but at long intervals they become
+much more active, and throw up jets of wet mud to the height of
+nearly two hundred feet. This mud smells strongly of sulphur.
+
+In the peninsula of Taman, near the entrance to the Sea of Azof,
+there is a group of mud volcanoes, from one of which there was a
+considerable eruption on the 27th of February 1793. It was preceded
+by underground detonations, and accompanied by a column of fire and
+dense vapour, which rose to the height of several hundred feet. The
+discharge of mud and gas was abundant. The accompaniment of fire
+and smoke makes this eruption more nearly resemble that of a true
+volcano.
+
+There is in the adjacent parts of the Crimea a mountain named
+Korabetoff, which also presents similar phenomena. On the 6th of
+August 1853, a column of fire and smoke was seen to rise from the
+top of this mountain to a great height, and it continued for five
+or six minutes. Two other similar but less violent ejections of
+fire and smoke followed at short intervals. These appearances were
+the accompaniments of an eruption of black fetid mud, which
+overspread the ground at the foot of the mountain to a considerable
+depth.
+
+A still more striking phenomenon occurred in the Sea of Azof, on
+the 10th of May 1814. On that day a column of flame and very thick
+smoke arose out of the water, with a loud report like that of a
+cannon, and masses of earth with large stones were tossed high up
+into the air. Ten eruptions of this kind succeeded each other at
+intervals of about a quarter of an hour; and after they had ceased
+for a time, they began again during the night. Next morning it was
+found that an island had risen out of the sea, between nine and ten
+feet in height, surrounded by a lower level of hardened mud. A
+strong fetid smell, probably that of petroleum, proceeded from the
+island, and extended for a considerable distance all round.
+
+[Illustration: Air Volcanoes of Turbaco]
+
+Another mud volcano, named Jokmali, near the Caspian Sea, was
+formed in November 1827. In this case, also, the ejection of mud
+was for several hours preceded by flames, rising to so great a
+height that they could be seen at a distance of twenty-four miles.
+Large pieces of rock were at the same time thrown up and scattered
+to considerable distances all round. The entire district in which
+this mountain is situated, has its soil copiously impregnated with
+petroleum, and numerous wells are formed for its collection.
+Quantities of this mineral oil are frequently found floating on the
+sea, along the neighbouring shores, where the sailors are in the
+habit of setting fire to this floating petroleum, while they
+dexterously steer their boats so as to avoid the flames. In this
+district also stands the city of Baku, held sacred by the Parsees,
+or fire-worshippers, who have here built a temple, in which are
+kept burning perpetual fires, fed by the naphtha springing from the
+ground.
+
+During the past year, 1866, a small mud volcano has been formed in
+the flanks of Mount Etna. It began with an outburst of strong jets
+of boiling water. First, one rose to the height of about six feet,
+then several others broke out, whereupon the height of the whole
+set diminished. There was much gas bubbling through the water, and
+some petroleum floated on its surface. It was very muddy, and left
+a thick deposit as it flowed away. Neither flames nor noise
+accompanied this eruption.
+
+There are also diminutive volcanoes, consisting of small conical
+hills, from which nothing seems to be emitted but various sorts of
+gas. These are called air volcanoes. Such are those of Turbaco in
+South America, discovered by Baron Humboldt, who has left us a
+picture of them, of which you here have a copy. These volcanic
+hillocks are truncated cones, eighteen or twenty in number,
+composed of hardened mud, from 18 to 24 feet in height, and from
+about 140 to about 180 feet in diameter at the base. The small
+craters at the top are filled with liquid mud, whence bubbles of
+gas, chiefly nitrogen, are being continually disengaged.
+
+There is a similar, but much larger, group in the neighbouring
+province of Cartagena. It consists of about one hundred cones
+spread over a district of nearly four hundred square leagues. There
+is also a group of about fifty cones within a range of four or five
+miles in the adjacent peninsula of Galera-Zamba. A sub-marine
+volcano, from which there have been several eruptions, is supposed
+to be connected with these numerous salses.
+
+
+
+
+CHAPTER XII.
+
+New Zealand--Boiling Fountains and Lakes
+
+
+In the eruptions of mud volcanoes, described in the foregoing
+chapter, a frequent ingredient is boiling water. There are,
+however, several instances in which there are thrown up jets of
+boiling water that are not intermingled with mud, but in which the
+water is either pure or impregnated with some mineral which it
+holds in perfect solution. Of this nature are the Geysers of
+Iceland and California, already described.
+
+In New Zealand there is another variety of this phenomenon, the
+boiling water issuing forth, not in intermittent jets, as in the
+Geysers, but in perpetually flowing springs, forming lakes, in
+which the water remains nearly at the boiling point. These springs
+and lakes occur at a place called Roto-Mahana. The annexed woodcut
+will convey an idea of their appearance.
+
+There are several basins raised one above another, and all higher
+than the level of the large lake. The highest is of an oval form,
+and about two hundred and fifty feet in circumference. It is filled
+from an opening at the height of about a hundred feet above the
+level of the lower lake. At various stages below this upper basin
+are numerous other springs, from which several similar basins are
+filled. The whole of these basins empty themselves into the large
+lake below, and the water in all of them is nearly boiling hot,
+giving forth, with a hissing sound, volumes of white vapour.
+
+[Illustration: Boiling Lakes of Roto Mahana]
+
+These waters are richly impregnated with carbonate of lime, which
+has formed all round the margins of the basins beautiful
+incrustations of snowy whiteness. The sand round the lake is very
+warm; and if a stick be thrust into it, jets of steam arise.
+
+Doubtless, some years hence, the enterprising English settlers will
+establish hot baths here. Not far from the lake there are smaller
+basins, in which the water is not beyond what would be agreeable
+for a warm bath; while it is of a blue colour and beautifully
+clear.
+
+On both banks of the river Waikato, also in this neighbourhood, are
+found numerous basins full of boiling mud or slime, which cannot be
+approached save with extreme care, owing to the softness and
+slipperiness of the soil. The largest of these basins is oval in
+form, 14 feet long by 8 feet wide, and about as much in depth. It
+contains hot mud of a bright red colour, being strongly impregnated
+with oxide of iron. Large viscous bubbles are continually rising to
+the top, and on bursting they emit a fetid, sulphureous smell.
+These phenomena are nearly akin to those of a mud volcano.
+
+
+
+
+CHAPTER XIII.
+
+Underground Sounds--Quito--Rio Apure--Guanaxuato--Melida--Nakous.
+
+
+Not the least remarkable among the phenomena produced by volcanic
+forces, are the strange underground noises which are occasionally
+heard. For the most part these are the preludes either of shocks of
+earthquake or of volcanic eruptions. Those which for months
+preceded the upheaval of the volcano of Jorullo, will recur to your
+remembrance. For about a month before the great mud eruption from
+Tunguragua on 4th February 1797, already described, there proceeded
+from the interior of that mountain noises of the most fearful kind.
+These would occur suddenly in the midst of perfect silence. They
+were heard by Antonio Pineda, the naturalist, who was there at the
+time, and they led him to foretell the approach of some great
+convulsion. Strange to say, however, the catastrophe itself was
+unaccompanied by underground noises any where near the volcano.
+But, stranger still, at Quito, which is distant about 200 miles, a
+short time after the eruption began, there were heard tremendous
+underground thunders. But this distance, between the site of the
+underground noises and the probable focus of disturbance, was far
+exceeded in another remarkable instance. It is stated by Humboldt
+that, in the grassy plains of Calaboso, on the banks of the Rio
+Apure, a tributary of the Orinoco, there were heard, over a large
+extent of country, loud underground thunders, unaccompanied by any
+shaking of the ground; while great streams of lava were being
+poured forth from the crater of Morne-Garou, in the Island of St.
+Vincent, at the distance of no less than 632 miles in a right line.
+This was as though an eruption of Mount Vesuvius were accompanied
+by underground thunders in Normandy.
+
+There have, nevertheless, been instances of the existence of such
+underground noises, without their having been followed either by an
+earthquake, by a volcanic eruption, or any other outward appearance
+whatever. One of the most remarkable cases of the kind, was that
+mentioned by Humboldt as having occurred at Guanaxuato in Mexico, a
+mountain-city situated far from any active volcano. This celebrated
+traveller states that these noises began on the 9th of January
+1784, and lasted above a month. The sounds were at first neither
+very loud nor very frequent; but from the 15th to the 16th of
+January they resembled continuous low rolling thunder, alternating
+with short loud thunder-claps. The sounds then gradually died away
+and nothing came of them, although they excited great terror among
+the inhabitants while they lasted. There are mines in the
+neighbourhood fifteen hundred and ninety-eight English feet in
+depth, yet neither in them nor at the surface could the least
+tremor be detected.
+
+A somewhat similar phenomenon occurred in the Island of Melida in
+the Adriatic, off the coast of Dalmatia, where underground
+rumblings were heard from March 1822 to September 1824; but in this
+case the sounds were sometimes accompanied by shocks.
+
+A still more singular phenomenon of this sort occurs on the borders
+of the Red Sea, at a place called Nakous, where intermittent
+underground sounds have been heard for an unknown number of
+centuries. It is situated at about half a mile's distance from the
+shore, whence a long reach of sand ascends rapidly to a height of
+about three hundred feet. This reach is about eighty feet wide, and
+resembles an amphitheatre, being walled in by low rocks. The sounds
+coming up from the ground at this place recur at intervals of about
+an hour. They at first resemble a low murmur; but ere long there is
+heard a loud knocking, somewhat like the strokes of a bell, and
+which, at the end of about five minutes, becomes so strong as to
+agitate the sand.
+
+The explanation of this curious phenomenon given by the Arabs, is,
+that there is a convent under the ground here, and that these
+sounds are those of the bell, which the monks ring for prayers. So
+they call it "Nakous," which means a bell. The Arabs affirm that
+the noise so frightens their camels when they hear it as to render
+them furious. Philosophers attribute the sounds to suppressed
+volcanic action--probably to the bubbling of gas or vapours
+underground.
+
+
+
+
+CHAPTER XIV.
+
+Extinct Volcanoes--Auvergne--Vienne--Agde--Eyfel--Italy--Lacus
+Cimini--Grotto del Cane--Guevo Upas--Talaga Bodas--The Dead Sea.
+
+
+There are two sorts of extinct volcanoes: _first_, those in
+which all evidences of activity have entirely ceased; and,
+_secondly_, those in which a subdued state of activity
+lingers. The former are more widely distributed than the latter;
+but sometimes both kinds occur in the same district of country.
+
+Extinct volcanoes are found in the district of Auvergne in France.
+Solidified streams of lava occur at Volvic near Riom; and the
+crater whence they descended is still visible on the top of the Puy
+de Nugere. It is an oblong basin, having its edge broken on the
+side down which the lava flowed. In its descent the fiery stream
+appears to have encountered a knoll of granite, by which it was
+divided into two branches. These seem to have reunited lower down,
+and thence to have overspread the valley beneath.
+
+The Puy de Côme, a mountain near Clermont, appears to have sent
+forth two streams of lava, which have effected considerable changes
+in the surface of the country--blocking up the courses of rivers
+diverting them into new channels, and forming swamps in the old. On
+the top of Puy Pariou, to the north of Clermont, there exists a
+perfect crater, quite round, and about two hundred and fifty feet
+deep, whence there has flowed a stream of lava, whose course can be
+distinctly traced. The summit of Puy Graveniere, a long round-
+backed hill also near Clermont, consists almost entirely of a heap
+of volcanic cinders, which have obliterated all traces of a crater;
+but two streams of lava appear to have flowed from the sides of the
+mountain. The Puy de Dôme, and the mountains in its neighbourhood,
+likewise appear to be of volcanic origin, and to have been upheaved
+somewhat in the same manner as Jorullo. Although the aspect of the
+mountains of Auvergne indicates so clearly their having been active
+since the surrounding country acquired its present general
+conformation, neither history nor tradition has preserved any
+record of their eruptions.
+
+There is extant, however, a letter from Sidonius Apollinaris, a
+cotemporary of Pliny, addressed to the Bishop of Vienne, in which
+he refers to forms of prayer which had been appointed by the bishop
+at the time when earthquakes demolished the walls of Vienne, and
+the mountains, opening, vomited forth torrents of inflamed
+materials. It hence appears that the extinct volcanoes in the
+neighbourhood of Vienne, and perhaps those of Le Puy, had been in a
+state of eruption not long after the beginning of the Christian
+era. To the westward of the latter town, there is a number of small
+volcanic craters, of which the two largest are the Lake de Bouchet
+and the Crater of Bar, which also appears to have been at one time
+a lake, but is now dry. The former has its greatest diameter about
+2300 feet, with a depth of about 90 feet. The latter is on the top
+of a mountain, which is composed entirely of such substances as are
+ejected by volcanoes. Its diameter is about 1660, and its depth
+about 130 feet; while it is almost perfect in its form. The
+mountains near Vienne exhibit streams of lava, which accommodate
+themselves to the existing valleys. Near Agde also, on the shores
+of the Gulf of Lions, on the top of a hill named St. Loup, there is
+an extinct crater, whence have descended two streams of lava
+apparently of recent origin. On one of them the town of Agde has
+been built; the other projects into the sea.
+
+The district of Eyfel, on the borders of the Rhine, is another in
+which extinct volcanoes abound. They occur mostly in the form of
+circular craters, which are now filled with water, their borders
+consisting of volcanic ejections. They also exhibit various
+superficial streams of lava. One of the most remarkable of these
+round craters lies near Andernuch, a little west of the Rhine. It
+is named the Lake of Laach, and is nearly two miles in circumference.
+On its margin are found numerous volcanic ejections, exactly
+resembling those of Mount Vesuvius. Notwithstanding these
+evidences that the extinct volcanoes of Eyfel have been in activity
+since the country acquired its present conformation, there are no
+historical records of their operations. There is, indeed, a passage
+in Tacitus referring to fires that issued from the earth near
+Cologne; but his description does not warrant the conclusion that
+the event to which he alludes was of the nature of a volcanic
+eruption. The Drachenfels on the eastern bank of the Rhine, and the
+other mountains in its neighbourhood, belong to the more ancient
+volcanic formations. The same may be affirmed of the other
+mountains scattered throughout Germany and central Europe
+generally, in which rocks of volcanic origin occur.
+
+There are a good many traces of extinct volcanoes in Italy, besides
+those of the Phlegræan fields already mentioned. In general
+character they resemble those previously described. The chief
+localities are certain lakes, near Volterra in Tuscany, which give
+forth very hot sulphurous and boracic acid vapours; a small
+sulphureous lake near Viterbo continually giving forth bubbles of
+gas; the Lake of Vico between Viterbo and Rome; the mountain and
+Lake of Albano near Rome; Mount Vultur in the Apennines, in the
+province of the Basilicata; and Lake Agnano near Naples. Of these,
+the Lakes of Vico and Agnano are the most interesting. The former
+is the ancient Lacus Cimini, and old authors state that its site
+was once occupied by a town, whose ruins used to be visible at the
+bottom of the lake when the water was clear. The ground, with the
+town upon it, is said to have been ingulfed during a volcanic
+convulsion, when the lake was formed in its place.
+
+The Lake Agnano is the site of an ancient volcanic crater, and on
+its margin is situated the Grotto del Cane, so famous for the
+deadly vapours it exhales. These consist of carbonic acid gas, in
+combination with watery vapour. This celebrated Grotto is thus
+described, in his work on volcanoes, by Dr. Daubeny, who visited
+the spot:--
+
+"The mouth of the cavern being somewhat more elevated than its
+interior, a stratum of carbonic acid goes on constantly
+accumulating at the bottom, but upon rising above the level of its
+mouth, flows like so much water over the brim. Hence the upper part
+of the cavern is free from any noxious vapour; but the air of that
+below is so fully impregnated, that it proves speedily fatal to any
+animal that is immersed in it, as is shown to all strangers by the
+experiment with the dog.
+
+"The sensation I experienced, on stooping my head for a moment to
+the bottom, resembled that of which we are sometimes sensible on
+drinking a large glass of soda water in a state of brisk
+effervescence. The cause in both instances is plainly the same.
+
+"The quantity of carbonic acid present in the cavern at various
+heights, was shown by immersing in it various combustibles in a
+state of inflammation. I found that phosphorus would continue
+lighted at about two feet from the bottom, whilst a sulphur match
+went out a few inches above, and a wax taper at a still higher
+level.
+
+"It was impossible to fire a pistol at the bottom of the cavern,
+for although gunpowder may be exploded even in carbonic acid by the
+application of a heat sufficient to decompose the nitre, and
+consequently to envelop the mass in an atmosphere of oxygen gas,
+yet the mere influence of a spark from steel produces too slight an
+augmentation of temperature for this purpose."
+
+Similar phenomena, but on a grander scale, are presented by the
+extinct crater in the Island of Java called "Guevo Upas," the
+Poison-Valley. It is a level about half a mile in circumference,
+surrounded by precipitous rocks. From various parts of its soil
+carbonic acid gas is discharged in such quantities as to prove
+fatal to any animal venturing nigh. The ground is consequently
+strown with numerous skeletons. This valley gave rise to the famous
+figment about the upas-tree, which once obtained such general
+belief in Europe.
+
+There is another extinct crater in Java, whence are exhaled vapours
+equally deadly, but which exert a most peculiar effect on the dead
+carcasses subjected to their influence. Instead of their being, as
+in the Gruevo Upas, reduced to skeletons, the carcasses have all
+their bones dissolved by the vapours; while the flesh, skin, hair,
+and nails are by their action preserved from decay. This remarkable
+crater is situated near the volcano of Talaga Bodas.
+
+Of all the extinct volcanoes in the world, however, none is so
+remarkable as the Dead Sea. That singular collection of salt and
+bitter water has the level of its surface depressed 1312 feet below
+that of the Mediterranean--thus indicating an enormous subsidence.
+The Dead Sea occupies the site of what was formerly the plain of
+Jordan, described as having been "well-watered everywhere, as the
+garden of the Lord, like the land of Egypt." One part of it, called
+the Vale of Siddim, was full of slime-pits--the only indications of
+volcanic action. When the cities of Sodom and Gomorrah, which stood
+in the plain, were destroyed, the Lord, it is said, rained upon
+them fire and brimstone from heaven; but while these fell upon the
+cities from the atmosphere, it appears that they must have
+primarily been discharged from the earth; for "the smoke of the
+country went up as the smoke of a furnace." The phenomena,
+therefore, most likely resembled, in the first instance, those of
+Jorullo; but the catastrophe seems to have ended like the last
+great eruption of the volcano in Timor--the whole of the plain
+having been ingulfed and replaced by the salt lake, whose depressed
+level so clearly indicates the nature of its origin.
+
+
+
+End of the Project Gutenberg EBook of Wonders of Creation, by Anonymous
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