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-Project Gutenberg's Thoughts on a Pebble, by Gideon Algernon Mantell
-
-This eBook is for the use of anyone anywhere in the United States and
-most other parts of the world at no cost and with almost no restrictions
-whatsoever. You may copy it, give it away or re-use it under the terms
-of the Project Gutenberg License included with this eBook or online at
-www.gutenberg.org. If you are not located in the United States, you'll
-have to check the laws of the country where you are located before using
-this ebook.
-
-
-
-Title: Thoughts on a Pebble
- or, A First Lesson in Geology
-
-Author: Gideon Algernon Mantell
-
-Release Date: August 7, 2020 [EBook #62871]
-
-Language: English
-
-Character set encoding: ISO-8859-1
-
-*** START OF THIS PROJECT GUTENBERG EBOOK THOUGHTS ON A PEBBLE ***
-
-
-
-
-Produced by Tom Cosmas from materials made freely available
-on The Internet Archive. All derived products are placed
-in the Public Domain.
-
-
-
-
-
-
-
-
-
-Transcriber Note
-
-Text emphasis is denoted as _Italics_ and =Bold=. Whole and fractional
-parts of numbers as 123-4/5.
-
-
-
-
-THOUGHTS ON A PEBBLE.
-
-[Illustration]
-
-REEVE, BENHAM, AND REEVE, PRINTERS AND PUBLISHERS OF SCIENTIFIC WORKS,
-KING WILLIAM STREET, STRAND.
-
-[Illustration: GIDEON ALGERNON MANTELL, L.L.D. F.R.S
-
-_Vice-President of the Geological Society &c. &c._]
-
-
-
-
- THOUGHTS
-
- ON A
-
- PEBBLE,
-
- OR,
-
- A FIRST LESSON IN GEOLOGY.
-
-
- BY THE AUTHOR OF "THE WONDERS OF GEOLOGY."
-
-
-[Illustration: _The Nautilus and the Ammonite._ _Vide_, p. 57.]
-
-
-"There is no picking up a pebble by the brook-side, without finding all
-nature in connexion with it."
-
- _Contemplations of Nature._
-
-EIGHTH EDITION; WITH THIRTY-TWO ILLUSTRATIONS.
-
-
-LONDON:
-
-REEVE, BENHAM, AND REEVE, KING WILLIAM STREET, STRAND.
-
-1849.
-
-
- TO
-
- MY SON,
-
- =Reginald Nebille Mantell, C.E.,=
-
- THESE
-
- "THOUGHTS ON A PEBBLE"
-
- ARE MOST AFFECTIONATELY
-
- INSCRIBED.
-
-
- LONDON,
-
- 19, CHESTER SQUARE, PIMLICO.
-
- 1849.
-
-"Every grain of sand is an immensity--every leaf a world--every insect
-an assemblage of incomprehensible effects in which reflection is lost."
-
- Lavater.
-
-
-"To the natural philosopher there is no natural object that is
-unimportant or trifling. From the least of Nature's works he may learn
-the greatest lessons. The fall of an apple to the ground may raise his
-thoughts to the laws which govern the revolutions of the planets in
-their orbits; or the situation of a _pebble_ may afford him evidence of
-the state of the globe he inhabits, myriads of ages before his species
-became its denizens."
-
- Sir J. F. W. Herschel.
-
-
-
-
-TO THE READER.
-
-
-Deeply impressed with the conviction that it is of the highest
-importance the young and inquiring mind should have a correct idea
-of natural phenomena--that it should not be left to its own unaided
-efforts to unravel the mysteries of the beautiful world in which this
-first state of being is destined to be passed--or have its curiosity
-stifled or misled by unsatisfactory or erroneous conjectures--I have
-endeavoured in this little work to explain in a simple and attractive
-guise, some of the grand truths relating to the ancient physical
-history of our planet, which modern geology has established.
-
-The favourable reception of these desultory "_Thoughts_" which
-were originally penned for the amusement and instruction of an
-intelligent boy, is a gratifying proof that the attempt has not been
-unsuccessful; and I would fain indulge the hope, that this "_First
-Lesson in Geology_" may still be productive of good, by exciting in
-some youthful minds a desire for the acquisition of natural knowledge;
-and inculcating the important truth, that He who formed the Universe
-has created nothing in vain; that His works all harmonize to blessings
-unbounded by the mightiest or most minute of His creatures; and that
-the more our knowledge is increased, and our powers of observation are
-enlarged, the more exalted will be our conception of His wondrous works.
-
- Chester Square,
- Pimlico.
-
-
-
-
-CONTENTS.
-
-
- Page.
-
- Thoughts on a Pebble: Part I. 5
-
- More Thoughts on a Pebble: Part II. 33
-
- "The Nautilus and the Ammonite" 57
-
- Supplementary Notes 61
-
- Note I. _Shells in Chalk_ 61
-
- ---- II. _Wood in Flint_ 66
-
- ---- III. _Whitby Ammonites_ 69
-
- ---- IV. _Fossil Nautili_ 72
-
- ---- V. _Brighton Cliffs_ 75
-
- ---- VI. _Rotaliĉ in Chalk and Flint_ 79
-
- ---- VII. _Isle of Wight Pebbles_ 82
-
- ---- VIII. _Zoophytes of the Chalk_ 87
-
- ---- IX. _Minute Corals from the Chalk_ 92
-
- ---- X. _Infusorial Earths_ 97
-
-
-
-
-LIGNOGRAPHS.
-
-
- Page.
-
- 1. Vignette of Title-page.
-
- 2. Fossil Turban-echinus (_Cidaris_), with spines. 9
-
- 3. Bivalve with spines (_Plagiostoma spinosum_) in
- chalk; from Lewes. 11
-
- 4. Teeth of several species of the Shark tribe, in
- chalk; from Lewes. 12
-
- 5. Chalk-dust highly magnified, consisting of minute
- shells. 13
-
- 6. Shells (_Rotaliĉ_) from the chalk, highly magnified. 14
-
- 7. Ammonite (_A. communis_) from the Lias, at Whitby. 20
-
- 8. Nautilus (_N. elegans_) from the chalk-marl, Lewes. 22
-
- 9. View of the Cliffs east of Brighton. 27
-
- 10. Fossil animalcules (_Xanthidia_) in flint. 35
-
- 11. _Xanthidium palmatum_, in flint. 37
-
- 12. Rotalia in flint. 39
-
- 13. Minute scales of fishes in flint. 40
-
- 14. Choanites from the chalk; near Lewes. 44
-
- 15. A branch of fossil coral attached to the pebble 46
-
- 16. Coral-polype in flint. 47
-
- 17. Minute Corals from chalk. 50
-
- 18. Fossil cases or shields of animalcules from
- Richmond, Virginia; highly magnified. 53
-
- 19. Several species of Lamp-shells (_Terebratulĉ_) from
- the chalk, near Brighton. 63
-
- 20. Silicified Oyster from the chalk. 65
-
- 21. Coniferous wood in flint, from Lewes Priory. 68
-
- 22. Several species of Ammonite. 69
-
- 23. The body of a recent microscopic animalcule
- (_Nonionina_), the shell having been removed by
- immersion in acid. 81
-
- 24. A branch of Sponge in flint; a minute Coral from
- chalk; and a section of a pebble enclosing a
- zoophyte (_Siphonia Morrisiana_). 85
-
- 25. Flints deriving their shapes from Zoophytes
- (_Ventriculites_). 89
-
- 26. Ventriculites in chalk; from Lewes. 90
-
- 27. Portions of three kinds of recent corals. 94
-
-
-
-
-LITHOGRAPHS.
-
- Page.
-
- Plate I. A rolled flint pebble, having a Choanite as a
- nucleus, and the remains of an echinus and spine,
- shell, and coral, apparent on the surface. 5
-
- Plate II. A longitudinal section of the pebble, showing
- the structure of the enclosed _Choanite_. 42
-
- Plate III. A polished section of an Ammonite, having
- the septa or chambers filled with variously coloured
- spar, &c. 70
-
- Plate IV. Polished sections of two pebbles from the
- Isle of Wight; in the upper specimen, the transition
- from opaque flint to cloudy chalcedony and
- transparent quartz crystals, is beautifully shown;
- the lower specimen is richly tinted; the dark
- appearance is derived from manganese. 86
-
-[Illustration: _Plate I._
-
-"THE PEBBLE"
-
-
-_Page 5_]
-
-
-
-
- THOUGHTS
-
- ON A
-
- PEBBLE.
-
- "Honoured, therefore, be thou, thou small pebble, lying in the lane;
- and whenever any one looks at thee, may he think of the beautiful and
- noble world he lives in, and all of which it is capable."
-
- Leigh Hunt's _London Journal_, p. 10.
-
-
-
-
-PART I.
-
-
-Well might our immortal Shakspeare talk of "_Sermons in stones_;" and
-Lavater exclaim, that "_Every grain of sand is an immensity_" and the
-author of 'Contemplations of Nature' remark, that "_there is no picking
-up a pebble by the brook-side without finding all nature in connexion
-with it._"
-
-I shall confine my remarks to a _flint_ pebble, as being the kind of
-stone familiar to every one. The pebble I hold in my hand was picked
-up in the bed of the torrent which is dashing down the side of yonder
-hill, and winding its way through that beautiful valley, and over those
-
- Huge rocks and mounds confus'dly hurl'd.
- The fragments of an earlier world,
-
-which partially filling up the chasm, and obstructing the course of
-the rushing waters, give rise to those gentle murmurings that are so
-inexpressibly soothing and delightful to the soul.
-
-[Sidenote: ORIGIN OF THE PEBBLE.]
-
-Upon examining this stone I discover that it is but the fragment of a
-much larger mass, and has evidently been transported from a distance,
-for its surface is smooth and rounded, the angles having been worn
-away by friction against other pebbles, produced by the agency of
-running water. I trace the stream to its source, half way up the hill,
-and find that it gushes out from a bed of gravel lying on a stratum of
-clay, which forms the eminence where I am standing, and is nearly 300
-feet above the level of the British Channel. From this accumulation of
-water-worn materials the pebble must have been removed by the torrent,
-and carried down to the spot where it first attracted our notice; but
-we are still very far from having ascertained its origin. The bed of
-stones on the summit of this hill is clearly but a heap of transported
-gravel--an ancient sea-beach or shingle--formed of chalk-flints, that
-at some remote period were detached from their parent rock, and
-broken, rolled, and thrown together, by the action of the waves. We are
-certain of this because we know that flints cannot grow;[A] that they
-were originally formed in the hollows or fissures of other stones; and
-upon inspecting the pebble more attentively, we perceive, not only that
-such was the case, but also that it has been moulded in _Chalk_, for it
-contains the remains of certain species of extinct shells and corals,
-which are found exclusively in that rock. Here then a remarkable
-phenomenon presents itself for our consideration; this flint, now so
-hard and unyielding, must once have been in a soft or fluid state,
-for the delicate markings of the case and spine of an _Echinus_, or
-Sea-Urchin, are deeply impressed on its surface;[B] and a fragile shell
-with its spines, is partially imbedded in its substance.[C] Nay more,
-upon breaking off one end of the pebble,[D] we find that a sponge, or
-some analogous marine zoophyte, is entirely enveloped by the flint;
-and also that there are here and there portions of minute corals, and
-scales of fishes. What a "_Medal of Creation_" is here--what a page of
-nature's volume to interpret--what interesting reflections crowd upon
-the mind!
-
-[A] "_Flints cannot grow._"--Here I would digress for a moment to
-notice an opinion so generally prevalent, that perhaps some of my
-young readers will not be prepared at once to answer the question--_Do
-stones grow?_ The farmer who annually ploughs the same land, and
-observes a fresh crop of stones every season, will probably reply in
-the affirmative; and the general observer who has for successive years
-noticed his gardens and plantations strewn with stones, notwithstanding
-their frequent removal, may possibly entertain the same opinion; but
-a little reflection will show that stones cannot be said to grow or
-increase, in the proper acceptation of the term. Animals and plants
-grow, because they are provided with vessels and organs by winch they
-are capable of taking up particles of matter and converting them
-into their own substance; but an inorganic body can only increase in
-bulk by the addition of some extraneous material; hence stones may
-become incrusted, or they may be cemented together and form a solid
-conglomerate, but they possess no inherent power by which they can
-increase either in size or number--_they cannot grow_.
-
-[B] Plate I, _a_.
-
-[C] Plate I, _b_.
-
-[D] Plate I, _c_.
-
-[Sidenote: FOSSIL ECHINUS WITH SPINES.]
-
-[Illustration: Lign. 2:--Fossil Turban Echinus, with its
-spines; in limestone.
-
-(See '_Medals of Creation_', p. 340.)]
-
-[Sidenote: FOSSIL SHELLS IN CHALK.]
-
-[Illustration: Lign. 3:--Shell with spines, imbedded in Chalk;
-from Lewes. (See '_Medals of Creation_,' 1 p. 390.)]
-
-To avoid confusion, we will reverse the order of our inquiry, and first
-contemplate the formation of the flint in its native rock. The Chalk,
-that beautiful white stone, which (as an American friend, who saw it
-for the first time, observed), is so like an artificial production,
-abounds in marine shells and corals, and in the remains of fishes,
-crabs, lobsters, and reptiles, all of which differ essentially from
-living species; although a few of the corals and shells resemble, in
-some particulars, certain kinds that inhabit the seas of hot climates.
-These remains are found in so perfect a state--the shells with all
-their spines and delicate processes (_Lign. 3_), and the fishes with
-their teeth (_Lign, 4_), scales, and fins, entire--that no doubt can be
-entertained of the animals having been surrounded by the chalk while
-living in their native sea, and that many of them were entombed in
-their stony sepulchres suddenly, when the rock was in the state of mud,
-or like liquid plaster of Paris.[E]
-
-[E] See Note I. _Shells in the Chalk._
-
-[Illustration: Lign. 4:--Fossil teeth of Fishes of the Shark
-family, in Chalk; from Lewes. (See '_Medals of Creation_.' p. 625.)]
-
-[Sidenote: SHELLS AND FISHES IN CHALK.]
-
-But besides the fossils which are obvious to the unassisted eye, the
-Chalk teems with myriads of minute forms that may readily be detected
-with a lens of moderate power; and even when these have been extracted,
-the residue, which appears to be merely white calcareous earth, is
-found, when examined under the microscope, to consist almost wholly of
-bodies yet more infinitesimal--of perfect shells and corals, so minute,
-that a cubic inch of chalk may contain upwards of a million of these
-organic remains (see _Lign. 5_)!
-
-[Illustration: Lign. 5:--A few grains of Chalk-dust highly
-magnified, and shown to consist of shells, &c.
-
- _a, a_, Shells called Rotalia.
-
- _b_, ------------- Textularia.
-
- (See '_Medals of Creation_,' p. 232.)
-
-]
-
-
-The Chalk is stratified--that is, divided into _strata_ or layers--as
-if a certain quantity of mud had sunk to the bottom of the sea, and
-enveloped the shells, corals, &c., which fell in its way, and had
-become somewhat solid before another layer was deposited upon it.
-
-[Sidenote: FLINT NODULES AND VEINS.]
-
-The mineral substance termed _silex_ or _flint_, is variously
-distributed in the chalk. It most commonly occurs in the state of
-nodules of an irregular or spheroidal, globular figure, which are
-arranged in rows parallel and alternating with, the cretaceous strata;
-it is likewise disposed in continuous thin layers, which are spread
-over considerable areas; and it often forms horizontal, vertical, and
-oblique veins, that fill up the fissures and interstices of the chalk.
-The siliceous nodules frequently enclose corals, shells, sponges,
-and other organic remains, as in the pebble before us; and in many
-instances these fossils are found partly imbedded in the chalk and
-partly invested with flint. But though flints contain in abundance
-relics of the same species of marine animals as the chalk, they are not
-like that rock composed of an aggregation of fossil remains; on the
-contrary, the siliceous earth, which is their constituent substance,
-was evidently once in a state of complete solution in water, and
-precipitated into the chalk before the latter was consolidated, the
-organic bodies serving as nuclei or centres around which the silex
-concreted; for the deposition of the flint, like that of the chalk,
-appears to have taken place periodically.[F]
-
-[F] Note II. _Wood in flint._
-
-[Illustration: Lign. 6:--Minute fossil shells from Flint and
-Chalk, very highly magnified, and seen by transmitted light.
-
- 1, 2, 3, 6, Rotaliĉ;
-
- 4, Portion of a Nautilus;
-
- 5, Rotalia composed of flint.
-
- (See '_Medals of Creation_,' p. 232.)
-
-]
-
-[Sidenote: ANIMALCULES IN CHALK.]
-
-The composition of the Chalk, and the prevalence throughout that rock
-of the relics of animals that can only live in salt-water, prove
-incontestably that the chalk and flint were deposited in the sea;
-and that our beautiful South Downs, now so smooth and verdant, and
-supporting thousands of flocks and herds, and the rich plains and
-fertile valleys spread around their flanks, were once the bed of an
-ocean. It is also evident not only that such must have been the case,
-but also that the Chalk was deposited in the basin of a very _deep_
-sea--in the profound abyss of an ocean as vast as the Atlantic.
-
-[Sidenote: AMMONITES AND NAUTILI.]
-
-From the absence of gravel, shingle, and sea-beach, it is certain that
-the white chalk-strata were formed at a great distance from sea-shores
-and cliffs; and this inference is confirmed by the swarms of shells
-termed _Ammonites_ and _Nautili_, which we know from their peculiar
-structure were, like the recent pearly Nautilus, inhabitants of deep
-waters only. For these are chambered shells; that is, are divided
-internally by thin transverse shelly septa or plates, into numerous
-cells; the body of the animal occupied only the outer compartment,
-but was connected with the entire series of chambers by a tube or
-siphuncle, which passed through each partition. This mechanism
-constituted an apparatus which contributed to the buoyancy of these
-animals when afloat on the waves; for the Ammonites and Nautili were
-able to swim on the surface, or sink to the depths of the ocean at
-pleasure.
-
- The fragile Nautilus that steers his prow,
- The sea-born sailor of his shell canoe,
- The Ocean Mab, the fairy of the sea,
- O'er the blue waves at will to roam is free.
- He, when the lightning-winged tornadoes sweep
- The surf, is safe, his home is in the deep;
- And triumphs o'er the Armadas of mankind,
- Which shake the world, yet crumble in the wind.
-
- Byron, _The Island_.
-
-[Sidenote: WHITBY SNAKE-STONES.]
-
-[Illustration: Lign. 7:--Ammonite from Whitby.]
-
-The Ammonites, so called from the supposed resemblance of their shells
-to the fabled horn of Jupiter Ammon, are only known in a fossil state;
-but they must have swarmed in the ancient seas, for several hundred
-species have been discovered in the Chalk and antecedent strata, though
-none have been found in any deposits of more recent formation; at the
-termination of the chalk epoch the whole race, therefore, appears to
-have perished. The Ammonites are commonly termed _snake-stones_, from
-the origin ascribed to them by local legends; those of Whitby are well
-known (see _Lign. 7_).[G]
-
-[G] Note III. _Whitby Ammonites._
-
- Thus Whitby's nuns exulting told--
- How that of thousand snakes, each one
- Was changed into a coil of stone,
- When holy Hilda prayed:
- Themselves, within their sacred bound,
- Their stony folds had often found.
-
- Scott's _Marmion_.
-
-[Illustration: Lign. 8:--Nautilus from the Chalk, near Lewes,
-(one-eighth the natural size.)]
-
-The Nautili were the contemporaries of the Ammonites, and many kinds
-are found associated with those shells, in strata far more ancient than
-the Chalk; and several species of both genera, as we have previously
-shown, were inhabitants of the cretaceous ocean. When the Ammonites
-became extinct, the Nautili continued to flourish, and numerous
-examples occur in the strata that were deposited during the vast period
-which intervened between the close of the Chalk formation, and the
-dawn of the existing condition of the earth's surface. At the present
-time two or three kinds only are known in a living state, and these are
-restricted to the seas of tropical climes, and so seldom approach the
-shores, that but few specimens of the animals that inhabit the shells
-have been obtained.
-
-The Nautilus, therefore, is one of those types of animal organization
-that have survived all the physical revolutions to which the surface of
-the earth was subjected during the innumerable ages that preceded the
-creation of the human race.[H] This remarkable fact is portrayed with
-much force and beauty by Mrs. Howitt, in the following stanzas:
-
-[H] Note IV. _Fossil Nautili._
-
-TO THE NAUTILUS.
-
- Thou didst laugh at sun and breeze
- In the new created seas;
- Thou wast with the reptile broods
- In the old sea solitudes,
- Sailing in the new-made light,
- With the curled-up Ammonite.
- Thou surviv'dst the awful shock,
- Which turn'd the ocean-bed to rock;
- And chang'd its myriad living swarms
- To the marble's veined forms.
- Thou wert there, thy little boat,
- Airy voyager! kept afloat,
- O'er the waters wild and dismal,
- O'er the yawning gulfs abysmal;
- Amid wreck and overturning,
- Rock-imbedding, heaving, burning,
- Mid the tumult and the stir,
- Thou, most ancient mariner!
- In that pearly boat of thine,
- Sail'dst upon the troubled brine.
-
-[Sidenote: THE SEA-SHORE.]
-
-We have thus acquired satisfactory proof that the flint of which our
-pebble is composed, was once fluid in an ocean teeming with beings, of
-genera and species unknown in a living state, and that it consolidated
-and became imbedded in the chalk, which was then being deposited at
-the bottom of the sea; hence the shells, corals, and other organic
-remains, which we now find attached to its surface, and enclosed in
-its substance. Thus much for the origin of the pebble; let us next
-inquire by what means it was dislodged from its rocky sepulchre, cast
-up from the depths of the ocean, and transported to the summit of the
-hill whence it was dislodged by yonder torrent. If we stroll along the
-sea-shore, and observe the changes which are there going on, we shall
-obtain an answer to these questions; for
-
- There is a _language_ by the lonely shore--
- There is society where none intrudes,
- By the deep Sea, and music in its roar!
-
- Byron.
-
-The incessant dashing of the waves against the base of the
-chalk-cliffs, undermines the strata, and huge masses of rock are
-constantly giving way and falling into the waters. The chalk then
-becomes softened and disintegrated, and is quickly reduced to the state
-of mud, and transported to the tranquil depths of the ocean, where it
-subsides and forms new deposits; but the flints thus detached, are
-broken and rolled by attrition into the state of boulders, pebbles, and
-gravel, and ultimately of sand.
-
-[Illustration: Lign. 9:--View of Brighton Cliffs; looking
-eastward from Kemp Town.[I]
-
- _a. Cliff's composed of chalk rubble._
-
- _b. Ancient elevated sea-beach._
-
- _c. Chalk forming the base of the Cliffs._
-
-]
-
-[I] Note V. _Brighton Cliffs._
-
-[Sidenote: BRIGHTON CLIFFS.]
-
-Now we must bear in mind, that had the chalk remained at the bottom of
-the deep sea in which it was originally deposited, it would not have
-been exposed to these destructive operations. It is therefore manifest,
-that at some very distant period of the earth's physical history, the
-bed of the Chalk-ocean was broken up, extensive areas were protruded
-above the waters, lines of sea-cliffs were formed, and boulders, sand,
-and shingle accumulated at their base. Subsequent elevations of the
-land took place, and finally, the sea-beach was raised to its present
-situation, which is several hundred feet above the level of the sea!
-
-Every part of the earth's surface presents unequivocal proofs that the
-elevation of the bed of the ocean in some places, and the subsidence
-of the dry land in others, have been, and are still, going on; and
-that, in truth, the continual changes in the relative position of the
-land and water, are the effects of laws which the Divine Author of
-the Universe has impressed on matter, and thus rendered it capable of
-perpetual renovation:--
-
- Art, Empire, Earth itself, to change are doomed;
- Earthquakes have raised to heaven the humble vale,
- And gulfs the mountain's mighty mass entombed,
- And where the Atlantic rolls wide continents have bloomed.
-
- Beattie.
-
-[Sidenote: IMMUTABILITY OF THE SEA.]
-
-Our noble poet, Lord Byron, in his sublime apostrophe to the Sea,
-has most eloquently enunciated the startling fact revealed by modern
-geological researches,--namely, that if the character of immutability
-be attributable to anything on the surface of our planet, it is to the
-ocean and not to the land!--
-
- Roll on, thou deep and dark blue ocean--roll!
- Ten thousand fleets sweep over thee in vain;
- Man marks the earth with ruin--his controul
- Stops with the shore:--upon the watery plain
- The wrecks are all thy deed, nor doth remain
- A shadow of man's ravage, save his own.
- When, for a moment, like a drop of rain.
- He sinks into thy depths with bubbling groan,
- Without a grave, unknell'd, uncoffin'd, and unknown!
-
- Thy shores are empires, changed in all save thee,--
- Assyria, Greece, Rome, Carthage, what are they?
- Thy waters wasted them while they were free,
- And many a tyrant since; their shores obey
- The stranger, slave, or savage,--their decay
- Has dried up realms to deserts:--not so thou,
- Unchangeable, save to thy wild waves' play--
- _Time writes no wrinkle on thine azure brow:_
- _Such as Creation's dawn beheld, thou rollest now!_
-
- Thou glorious mirror, where the Almighty's form
- Glasses itself in tempests; in all time,
- Calm or convulsed--in breeze, or gale, or storm,
- Icing the Pole, or in the torrid clime
- Dark-heaving, boundless, endless, and sublime--
- The image of Eternity--the throne
- Of the Invisible; even from out thy slime
- The monsters of the deep are made; each zone
- Obeys thee: thou goest forth, dread, fathomless, alone!
-
- Childe Harold. _Canto IV._
-
-[Sidenote: APOSTROPHE TO THE OCEAN.]
-
-I will conclude this "first lesson" with the following beautiful
-remark of an eminent living philosopher:[J]--"To discover order and
-intelligence, in scenes of apparent wildness and confusion, is the
-pleasing task of the geological inquirer; who recognises, in the
-changes which are continually taking place on the surface of the globe,
-a series of necessary operations, by which the harmony, beauty, and
-integrity of the Universe are maintained and perpetuated; and which
-must be regarded, not as symptoms of frailty or decay, but as wise
-provisions of the Supreme Cause, to ensure that circle of changes, so
-essential to animal and vegetable existence."
-
-[J] Dr. Paris.
-
-[Illustration]
-
-
-
-
- MORE THOUGHTS
-
- ON A
-
- PEBBLE.
-
- "Not a mote in the beam, not an herb on the mountain, not a pebble
- on the shore, not a seed far-blown into the wilderness, but contributes
- to the lore that seeks in all the true principle of life--the
- beautiful--the joyous--the immortal."
-
- Sir E. Bulwer Lytton's _Zanoni_.
-
-
-
-
-PART II.
-
-
-More thoughts on a pebble!--is not the subject exhausted? have not
-all the hieroglyphics impressed on the flint been interpreted?--can
-Science, like the fabled wand of the magician, call forth from the
-stone and from the rock their hidden lore, and reveal the secrets they
-have so long enshrined?--Gentle Reader! but one page of the eventful
-history of the pebble has been deciphered; I proceed to transcribe this
-natural record of the past, explain its mysterious characters, and
-present to thy notice the marvels they disclose.
-
-Our previous examination of the specimen showed that the flint had
-once been in a fluid state, and had consolidated in a sea inhabited by
-shells, echini, fishes, corals, sponges, and other zoophytes; and the
-appearance of the fractured end (_Plate I, c_), indicated that some
-organic body had formed the nucleus of the pebble, and that traces of
-the structure of the original still remained. To ascertain if this
-inference is correct, it will be necessary to divide the stone in a
-longitudinal direction--but I will first strike off a small fragment,
-and examine it by the aid of a microscope.
-
-[Sidenote: FOSSIL ANIMALCULES.]
-
-[Illustration: Lign. 10:--Fossil animalcules (_Xanthidia_) in
-Flint.]
-
-By a sharp blow of a hammer, a very thin and minute portion of the
-flint has been detached (see _Lign. 10, fig. 1_); it is translucent,
-and when held between the eye and a strong light, appears like a slice
-of horn; and a few extremely minute specks may with difficulty be
-detected. Under the microscope, five of these almost invisible points
-are well defined, and present a radiated appearance (see _fig. 3_); but
-I will substitute a higher power, and lo! they are seen to be distinct
-globular or spherical bodies beset with spines (_fig. 3_); and with a
-still more powerful lens, one which magnifies many hundred times, their
-nature is completely displayed. The whole five possess this general
-character--a central globular case or shell, from which radiate tubes
-or hollow spines, that terminate in fringed or divided extremities
-(_figs. 4, 5, 6_); but these bodies differ from each other in the
-relative proportions of the shell and spines, and in the number,
-shape, and length of the tubular appendages. The group, in short, is
-separable into three distinct species, of the same kind of fossil
-remains; and several other varieties occur in the chalk and flint. .
-
-[Sidenote: XANTHIDIA IN FLINT.]
-
-[Illustration: Lign. 11:--_Xanthidium palmatum_ in flint:
-highly magnified.]
-
-But what are these bodies?--They are the durable cases of animalcules,
-many species of which swarm in our seas, and are so minute, that
-thousands may be contained in a drop of water! In a living state,
-the case is flexible and filled with a granular jelly, which is the
-soft body of the animalcule, and the tubes and the outer surface are
-invested with a similar substance. After death the soft parts dissolve;
-but the case and its spines often remain unchanged.
-
-In another magnified portion of the pebble, a specimen of the
-microscopic discoidal shells which we have already seen compose the
-greater part of the white chalk (_Lign. 5_, p. 14), is beautifully
-displayed when viewed by transmitted light, under a highly magnifying
-power (_Lign. 12_).[K] Our investigation has thus shown, that a great
-part of the pebble is actually composed of the aggregated fossil
-remains of animalcules, so minute as to elude our unassisted vision,
-but which the magic power of the microscope reveals to us, preserved,
-like flies in amber, in all their original sharpness of outline and
-delicacy of structure.
-
-[K] Note VI. _Rotaliĉ in chalk and flint._
-
-[Sidenote: ROTALIA IN FLINT.]
-
-[Illustration: Lign. 12:--Rotalia in flint: highly magnified.]
-
-On another fragment of this stone two glittering specks, not larger
-than a pin's head, are discernible (_Lign. 9_): these with a magnifier
-of moderate power, are seen at a glance to be scales of fishes. But
-they differ from each other; both have the surface smooth, and without
-enamel: in the one the margin or edge is simple (_fig. 3_); in the
-other, it is divided like the teeth of a comb (_fig. 2_);--trifling as
-this difference may appear, it is sufficient to enable the naturalist
-to determine that the fishes which furnished these scales belonged to
-two distinct orders, of which the Salmon and the Mullet are living
-examples.
-
-[Illustration: Lign. 13:--Scales of Fishes in flint.
-
- Fig. 1.--A fragment of the pebble with the scales of the natural size.
-
- 2.--One of the Scales (of a species of _Beryx_) highly magnified.
-
- 3.--The other Scale (of a species of _Salmo_).
-
-]
-
-[Illustration: _Plate II._
-
-_Longitudinal section of the Pebble._
-
-_Page 41._]
-
-
-
-
-[Sidenote: SECTION OF THE PEBBLE.]
-
-SECTION OF THE PEBBLE.
-
-_Plate II._
-
-
-We will now avail ourselves of the assistance of the lapidary, and
-divide the pebble in a longitudinal direction;--what a beautiful and
-interesting section is thus obtained! The markings observable on the
-fractured portion of the stone (see Plate I, c), are thus
-shown to have originated, as we surmised, from some organic body,
-which the flint, when fluid, had penetrated and enveloped. The enclosed
-fossil was obviously one of those soft marine zoophytes, allied to the
-_Actiniĉ_ or _Sea-Anemones_, which are of a globular, spherical, or
-inversely conical shape, and consist of a tough, jelly-like substance,
-permeated with tubes, disposed in a radiated manner around a central
-cavity, or digestive sac; a structure admitting of that constant supply
-and circulation of sea-water, which the economy of these curious forms
-of animal existence requires.
-
-[Sidenote: ISLE OF WIGHT PEBBLES.]
-
-The surface exposed by the division of the pebble, is an oblique
-vertical section of the petrified zoophyte. It shows a central canal
-filled with bluish-grey flint (_Plate II, c_), in a mass traversed by
-tubes or channels, which possess considerable beauty and variety of
-colour from an impregnation of iron.[L] A transverse section (see
-_Lign. 14._ fig. 1) would, of course, have a central spot, with rays
-proceeding thence to the circumference, as in the oblique fracture
-(_Plate I, c_).[M]
-
-[L] Specimens of this kind form beautiful objects when polished, and
-are mounted as brooches by the lapidaries of Brighton, Bognor, and
-the Isle of Wight, who term them petrified sea-animal flowers. Mr. G.
-Fowlstone (4, Victoria Arcade) of Ryde, has many splendid examples, and
-also agates and jaspers, the genuine productions of the Island.
-
-[M] Note VII. _Isle of Wight Pebbles._
-
-[Sidenote: CHOANITES KONIGI.]
-
-The form of the original zoophyte when living, must have been that of
-an inverted cone or funnel, (hence the scientific name _Choanite_ or
-funnel-like,) with a long cylindrical digestive cavity in the centre,
-from which tubes ramified through every part of the mass. It was
-attached to a rock, stone, or shell, by root-like fibres which spread
-out from its base; and its soft body was strengthened, as is the case
-in many sponges and animals of a similar nature, by numerous siliceous
-spines or spicula, which are often found in the flint and chalk (see
-_Lign. 10._ fig. 5).[N]
-
-[N] Note VIII. _Zoophytes of the Chalk._
-
-[Illustration: Lign. 14:--Choanites _Konigi_: from
-the Chalk.
-
- Fig. 1.--A transverse section.
-
- 2.--Upper portion of the body.
-
- 3.--Vertical section, like the pebble, Pl. II. p. 41.
-
- 4.--A flint, enclosing a Choanite, which is exposed on the
- upper surface.
-
- 5.--Various forms of siliceous spines of Choanites and other
- analogous bodies; magnified slightly.
-
- (See '_Medals of Creation_,' p. 264.)
-
-]
-
-The _Choanites_ must have swarmed in the Chalk ocean, for in some of
-the strata almost every flint exhibits traces of these zoophytes.[O]
-
-[O] The shingle at Brighton and Bognor in Sussex, and in various
-localities in the Isle of Wight, abounds in specimens more or less
-perfect. I would inform my fair readers who may visit these places, and
-be inclined to purchase a brooch, in illustration of these "_Thoughts
-on a Pebble_," that by far the greater number of the so-called
-Brighton and Isle of Wight moss-agates, jaspers, &c., sold by the
-lapidaries and jewellers, are of German or Scotch origin; and that the
-_false-emeralds_, and _aquamarines_, are water-worn fragments of common
-green glass bottles!
-
-[Sidenote: CORALS IN CHALK.]
-
-[Illustration: Lign. 15:--Branch of Coral on the
-Pebble.
-
- Fig. 1.--A portion magnified.
-
- 2.--A fragment represented as when alive.
- _a, a_, Two polypes collapsed.
- _b, b_, Two polypes with their tentacula extended.
-
-]
-
-One more character inscribed on the pebble remains to be interpreted;
-it is the minute branch of coral partially imbedded in the flint.[P]
-The surface of this coral, when seen with a powerful lens, is found to
-be studded with small pores or cells. In a recent state, each cell was
-inhabited by a living polype or animalcule, which, though permanently
-united at its base to the general mass, had an independent existence,
-and possessed sensation and voluntary motion; expanding its thread-like
-feelers or tentacula to catch its prey, and withdrawing, at will, into
-its little cell.[Q]
-
-[P] Plate I. immediately below the shell and spine of Echinus.
-
-[Q] For a popular account of recent and fossil corals, see 'Wonders of
-Geology,' 6th Edit., vol. ii. Lecture VI. p. 589.
-
-[Illustration: Lign. 16:--A Coral-polype preserved in flint:
-magnified 500 diameters.]
-
-From these investigations, we learn that the Pebble, which has formed
-the subject of our contemplation, had its origin in a living zoophyte
-that was growing on a rock, in a sea whose boundaries have long since
-been swept away; that corals, shells, and echini inhabited the bottom
-of the deep; and that fishes related to existing families, sported in
-the waters of that ancient ocean. In fine, we have presented to us the
-scene so exquisitely described by the American poet:--
-
-[Sidenote: THE CORAL GROVE.]
-
-THE CORAL GROVE.
-
- Deep in the waves is a coral grove.
- Where the purple mullet and gold fish rove,
- Where the sea-flower spreads its leaves of blue,
- That never are wet with the falling dew.
- But in bright and changeful beauty shine,
- Far down in the green and glassy brine.
- The floor is of sand, like the mountain drift.
- And the pearl-shells spangle the flinty snow;
- From coral rocks the sea-plants lift
- Their boughs, where the tides and billows flow;
- The water is calm and still below.
- For the winds and the waves are absent there,
- And the sands are bright as the stars that glow
- In the motionless fields of upper air:
- There with its waving blade of green,
- The sea-flag waves through the silent water,
- And the crimson leaf of the dulse is seen.
- To blush like a banner bathed in slaughter.
- There with a light and easy motion
- The fan-coral sweeps through the clear deep sea;
- And the yellow and scarlet tufts of ocean,
- Are bending like corn on the upland lea;
- And life in rare and beautiful forms,
- Is sporting amidst those bowers of stone.
-
- Percival.
-
-[Illustration: Lign. 17:--Minute Corals from the Chalk;[R]
-_highly magnified_.]
-
-[R] Note IX. _Minute corals from the Chalk._
-
-[Sidenote: MICROSCOPIC CORALS.]
-
-Our previous examination of the pebble had prepared us for these
-results; but the microscope, that mighty talisman of wisdom, has shown
-us, that even those infinitesimal creatures to whom a drop of water
-is an unbounded ocean--those living atoms of that world of being which
-is for ever concealed from the uninstructed mind--the inhabitants of
-that universe beneath us, which the eye of science can alone penetrate,
-existed in ages incalculably remote, and were, like their gigantic
-contemporaries, the living instruments by which a large proportion
-of the solid materials of the surface of our planet was elaborated;
-their imperishable siliceous and calcareous skeletons, constituting no
-inconsiderable amount of the crust of the earth.[S]
-
-[S] See _"Thoughts on Animalcules, or a Glimpse of the Invisible World
-revealed by the Microscope_," by the Author. Published by Mr. Murray,
-London, 1846.
-
-Fossil animalcules and corals similar to those we have discovered in
-the pebble and in the chalk, and hundreds of other genera and species
-equally minute, occur in such prodigious numbers, as to warrant the
-conclusion, that this class of animal existence has contributed more
-largely than any other, to the formation of the sedimentary strata.
-
-Not only the Chalk hills, but whole mountain-ranges formed of other
-deposits of great thickness and extent, are found to consist almost
-entirely of similar remains. In the state of rock, of sand, of clay,
-of marl--in the coarsest limestone, and in the purest crystal, the
-petrified skeletons of animalcules alike abound. The town of Richmond,
-in Virginia, is built on a bed of stone twenty feet thick, which is
-wholly composed of the fossil skeletons of different kinds of marine
-animalcules. The polishing slate of Bilin, in Germany, is wholly made
-up of the siliceous shields of similar beings, disposed in layers
-without any connecting medium; and these belong to species so minute,
-and are so closely compressed together, that in a cubic inch of the
-stone, weighing but two hundred and twenty grains, there are the
-remains of _forty-one thousand millions_ of animalcules![T]
-
-[T] See '_Medals of Creation_,' p. 221.
-
-[Illustration: Lign. 18:--Animalcules from the Richmond earth:
-very highly magnified[U]]
-
-[U] Note X. _Richmond Infusorial earth._
-
- * * * * *
-
-
-[Sidenote: REFLECTIONS.]
-
-Here we must bring our "_Thoughts on a Pebble_" to a close; but not
-without adverting to the pure and elevating gratification which
-investigations of this nature afford, and the beneficial influence
-they exert upon the mind and character. In circumstances where the
-uninstructed and incurious eye can perceive neither novelty nor beauty,
-he who is imbued with a taste for natural science will everywhere
-discover an inexhaustible mine of pleasure and instruction, and new
-and stupendous proofs of the power and goodness of the Eternal! For
-every rock in the desert, every boulder on the plain, every pebble by
-the brook-side, every grain of sand on the sea-shore, is fraught with
-lessons of wisdom to the mind which is fitted to receive and comprehend
-their sublime import.
-
- "From millions take thy choice,
- In all that lives a guide to God is given;
- Ever thou hear'st some guardian angel's voice,
- When nature speaks of heaven!"
-
-Amidst the turmoil of the world and the dreary intercourse of common
-life, we possess in these pursuits a never-failing source of delight,
-of which nothing can deprive us--an oasis in the desert, to which
-we may escape, and find a home "wherever the intellect can pierce,
-and the spirit can breathe the air."[V] For like the plant which the
-Prophet threw into the waters of Marah,[W] that changed the bitterness
-of the wave into sweetness, a branch from the tree of knowledge thrown
-into the turbid stream of life, purifies its waters, and imparts to
-them a healing virtue, which sheds a hallowing and refreshing influence
-over the soul!
-
-[V] Sir E. Bulwer Lytton.
-
-[W] Exod. XV. 23.
-
-
-
-
-THE
-
-NAUTILUS and the AMMONITE.
-
-(_See Page 22._)
-
-
-
-FROM SKETCHES IN PROSE AND VERSE,
-
-By the late G. F. Richardson, Esq.
-
- The Nautilus and the Ammonite
- Were launch'd in storm and strife;
- Each sent to float, in its tiny boat,
- On the wide, wild sea of life.
-
- And each could swim on the ocean's brim,
- And anon, its sails could furl;
- And sink to sleep in the great sea deep,
- In a palace all of pearl.
-
- And their's was a bliss, more fair than this,
- That we feel in our colder time;
- For they were rife in a tropic life,
- In a brighter, happier clime.
-
- They swam 'mid isles, whose summer smiles
- No wintry winds annoy;
- Whose groves were palm, whose air was balm.
- Where life was only joy.
-
- They roam'd all day, through creek and bay,
- And travers'd the ocean deep;
- And at night they sank on a coral bank,
- In its fairy bowers to sleep.
-
- And the monsters vast, of ages past.
- They beheld in their ocean caves;
- And saw them ride, in their power and pride,
- And sink in their billowy graves.
-
- Thus hand in hand, from strand to strand,
- They sail'd in mirth and glee;
- Those fairy shells, with their crystal cells,
- Twin creatures of the sea.
-
- But they came at last, to a sea long past,
- And as they reach'd its shore,
- The Almighty's breath spake out in death,
- And the Ammonite liv'd no more.
-
- And the Nautilus now, in its shelly prow,
- As o'er the deep it strays,
- Still seems to seek, in bay and creek,
- Its companion of other days.
-
- And thus do we, in life's stormy sea,
- As we roam from shore to shore;
- While tempest-tost, seek the lov'd--the lost--
- But find them on earth no more!
-
-Geology, in the magnitude and sublimity of the objects of which it
-treats, ranks next to Astronomy in the scale of the sciences.
-
- Sir J. F. W. Herschel.
-
-[Illustration]
-
-
-
-
-SUPPLEMENTARY NOTES.
-
-
-
-
-Note I. Page 13. _Shells in Chalk._
-
-
-The shells of mollusca, in consequence of their durability, are the
-most abundant fossils in the sedimentary strata;[X] entire layers
-of marble and other limestone, of great thickness and extent, are
-wholly composed of an aggregation of a few species or genera: in some
-instances of fresh-water snails--as, for example, the Sussex and
-Purbeck marbles;[Y] in others, of marine bivalves and univalves, as the
-oyster-conglomerate of Bromley, and the shelly limestones of Portland,
-Dorsetshire, &c.
-
-[X] For an account of the geological value of fossil shells, see
-'_Medals of Creation_,' vol. i. p. 363.
-
-[Y] See '_Wonders of Geology_,' 6th Edition, p. 402.
-
-The cretaceous strata contain many hundred species of bivalves and
-univalves, by far the greater part of which belong to extinct genera;
-and the species, with but four or five exceptions, are unknown in more
-recent deposits. In loose sandy strata, fossil shells are oftentimes
-beautifully preserved, and may be obtained in as perfect a condition
-as if gathered from the sands on the sea-shores: such is the state of
-the specimens which abound in the sandy clays near Barton in Hampshire,
-and in the "_Crag_" of Essex and Suffolk. In certain beds of clay,
-shells are also found entire; sometimes retaining the epidermis, and
-the cartilaginous ligament of the hinge. The bivalves in the white
-chalk are generally perfect; but the univalves, probably from the more
-delicate structure of the originals, seldom retain any vestiges of the
-shell, excepting portions of the internal nacreous coat adhering to the
-chalk casts, which have been moulded in the interior of the shells.
-
-[Illustration: Lign. 19:--Bivalve shells (_Terebratulĉ_) from
-Chalk (_natural size_).
-
- 1, 2. Plicated species. 1. _T. octoplicata._ 2. _T. subplicata._
- 3, 4. Smooth species. 3. _T. semiglobosa._ 4. _T. subrotunda._
-
-]
-
-[Sidenote: TEREBRATULĈ FROM CHALK.]
-
-In some of the cretaceous strata several extinct species of _Oyster_,
-_Scallop_, _Arca_, _Tellina_, and other well-known marine bivalves
-abound; and with them are associated many genera of which no living
-species have been observed. Among the bivalves that prevail in the
-English chalk, are three or four kinds of _Terebratulĉ_: which are
-small, elegant, subglobular shells, belonging to a family of which
-nearly 500 species, referable to several genera, have been obtained
-from the British strata.[Z] Certain genera are restricted to the most
-ancient sedimentary rocks, in which they occur in almost incredible
-numbers; others have a wider range and are met with in the later
-secondary deposits; while a few are found in the newest beds, and
-have living representative species in the seas of warm climates. From
-the immense antiquity of their lineage, these _Terebratulĉ_ have been
-humourously termed the "_fossil aristocracy_." Some of the most common
-chalk species are figured of the natural size in _Lign. 19_. When
-living the animal was attached to a rock or other body by means of a
-_byssus_ or peduncle, exserted through the aperture in the beak or
-curved extremity of the largest valve.[AA] The shells of the smooth
-_Terebratulĉ_ are full of minute holes or perforations, which may
-readily be distinguished with a lens of moderate power.
-
-[Z] See '_Wonders of Geology_,' 6th Edit. p. 329.
-
-[AA] In the Conchological Gallery of the British Museum there is a
-group of thirty or forty recent _Terebratulĉ_ attached to a stone by
-their peduncles; from Australia.
-
-[Sidenote: PETRIFIED OYSTER.]
-
-[Illustration: Lign. 20:--Oyster from the Chalk, near Brighton
-(natural size).]
-
-Occasionally the soft body of the mollusk completely silicified--that
-is, transmuted into flint--is found in its natural position in the
-shell. A beautiful example of this kind is represented in _Lign. 20_.
-It is an extinct species of oyster: both valves were entire when I
-removed the chalk and cleared the specimen; part of one valve has
-been broken away to expose the petrified body of the animal. I have
-seen a _Trigonia_[AB] from the oolite of Tisbury in Wiltshire, in
-which the entire body of the mollusk was transformed into flint, and
-the _branchiĉ_ or lamellated gills were beautifully defined, though
-converted into semi-transparent chalcedony.
-
-[AB] _Trigonia:_ a genus of bivalves, of which there are many extinct
-species in the chalk and oolite; some bands of Portland stone are an
-aggregation of _Trigoniĉ:_ a few very small species, inhabitants of the
-seas of Australia and New Zealand, are the only known living forms of
-this once prevailing type of mollusca. See '_Medals of Creation_,' p.
-407.
-
-
-
-
-Note II. Page 17. _Wood in Flint._
-
-
-[Sidenote: WOOD IN FLINT.]
-
-I would remind the reader that the white chalk, together with the
-various strata of sand, clay, and limestone, comprising the cretaceous
-formation of England, must be regarded as an ancient ocean-bed; in
-other words, an accumulation of earthy sediments, formed in the
-profound depths of the sea, in periods of long duration and of
-incalculable antiquity, and more or less consolidated by subsequent
-chemical and mechanical agency. These deposits are made up of organic
-and inorganic materials: the former consist of the debris of the cliffs
-and shores which encompassed the ancient ocean, of the spoils of the
-land brought into the waters by floods and rivers, and of mineral
-matter thrown down from chemical solutions. The organic substances
-are the durable remains of the animals and plants which lived and
-died in the sea, and of terrestrial and fluviatile species that were
-transported from islands or continents by rivers and their tributaries.
-The whole constitutes such an assemblage of strata as would probably be
-presented to observation, if a mass of the bed of the Atlantic 2,000
-feet in thickness, were elevated above the waters, and became dry land;
-the only essential difference would be in the generic and specific
-characters of the imbedded animal and vegetable remains.
-
-The vestiges of terrestrial and fluviatile animals and plants found in
-the chalk are comparatively but few: I have collected from Kent and
-Sussex, bones of gigantic land lizards, (the _Iguanodon_), of flying
-reptiles, (_Pterodactyles_), and of fresh-water Turtles, and water-worn
-fragments of stems of coniferous trees allied to the _Araucaria_ or
-Norfolk Island Pine; fruits or aments of coniferse; and stems and
-foliage of plants related to the _Cycas_ and _Zamia_.
-
-[Illustration: Lign. 21:--Fragment of coniferous wood in flint.]
-
-A fragment of silicified wood imbedded in a flint, is represented in
-_Lign. 21_. It was obtained from a wall in Lewes Priory in Sussex; and
-though it has been exposed to the atmosphere seven or eight centuries,
-still exhibits the characteristic internal structure.
-
-
-
-
-Note III. Page 20. _Whitby Ammonites._
-
-
-[Sidenote: AMMONITES.]
-
-[Illustration: _Lign. 22_:--Ammonites from the cretaceous formation.
-
- 1. _Ammonites varians_, from Hamsey.
-
- 2. _A. Dufresnoyi_: 2_a_, part of the same.
-
- 3. _A. lautus_: 3_a_, keel and septum of the same.
-
-]
-
-The Ammonites differ from the Nautili in having the margins of the
-septa or internal shelly partitions (which in the latter are smooth),
-foliated or wrinkled; and the siphunculus or tube placed along the
-back of the shell, whereas in the Nautilus it is central. The sides of
-the shell in the Ammonites are very generally more or less ornamented
-with arched elevations and depressions, and studded with spines and
-tubercles, as in the specimens above figured.
-
-There are several kinds of Ammonites found in the Lias at Whitby and
-other places in Yorkshire; the most common species is figured in
-_Lign. 7_. p. 20; the dark colour of this fossil is produced by the
-argillaceous stone with which it is now filled. The internal structure
-of these Ammonites is generally well preserved, the chambers being
-lined with spar or other mineral matter; transverse polished sections
-are often very beautiful from the several cells being occupied by
-variously coloured marble, susceptible of a high polish. (Pl. III.) In
-some examples the entire shell is transmuted into brilliant pyrites
-(sulphuret of iron), and the chambers are filled with white spar; a
-specimen of this kind in my possession, collected by Lady Murchison, is
-the most elegant fossil imaginable.
-
-[Illustration: _Plate III._
-
-_Polished section of an Ammonite._
-
-_Page 70._]
-
-[Sidenote: AMMONITE-MARBLE.]
-
-It is not unusual for the visitors at Whitby to inquire of the
-collectors how it is that the head of the animal is never found?
-and the crafty dealers, willing to accommodate the taste of their
-customers, carve the extremity of an Ammonite into the semblance of
-a serpent's head, and affix two red eyes; thus producing a veritable
-proof of the truth of the legend of St. Hilda! My young readers will
-not be duped by this trick-of-trade, if they reflect but a moment on
-the real nature of a fossil Ammonite: they will remember that it is a
-shell which, when empty, became filled with what was then soft mud, but
-is now stone; in like manner as if liquid plaster of Paris were poured
-into an empty snail-shell and consolidated.
-
-In some parts of Somersetshire, a beautiful marble composed of an
-aggregation of two or three small species of Ammonites, is used for
-sideboards and other ornamental purposes: the polished slabs are
-diversified by the numerous sections of the shells.
-
-Some of the clays of the Lias abound in a species of Ammonite of
-extraordinary beauty from the iridescent lustre of the pearly coat of
-the shell: a slab of stone from Watchett, on which a hundred or more
-Ammonites of this kind are displayed, may be seen in the British Museum.
-
-
-
-
-Note IV. Page 23. _Fossil Nautili._
-
-
-The beauty, elegant form, and remarkable internal structure of the
-shell of the Nautilus, have rendered it in all ages an object of
-curiosity and admiration: yet an accurate knowledge of the organization
-of the animal to which it belongs, has but recently been obtained. The
-Nautili may be regarded as Cuttle-fish or _Sepiĉ_, inhabiting shells
-furnished with an apparatus to impart buoyancy, and enable the animals
-to swim on the surface, or sink to the profound depths of the ocean.
-A few explanatory remarks on the nature of the recent Sepia may be
-necessary to render the subject intelligible to the unscientific reader.
-
-[Sidenote: RECENT NAUTILUS.]
-
-The _Sepia_ or Cuttle-fish of our seas is of an oblong form, and
-composed of a soft substance covered with a tough integument or skin:
-it varies from a few inches to a foot or more in length. The mouth
-is placed in the centre of one extremity of the body, and has a
-pair of powerful, curved, horny mandibles, much resembling the beaks
-of a parrot: it is surrounded by eight long arms like the rays of a
-star-fish, and these are beset with rows of little cups which act as
-suckers, and enable the animal to secure its prey, and attach itself
-with great firmness to any object.[AC] It has a distinct head, with
-two eyes as perfect as in the vertebrated animals, and complicated
-organs of hearing: and below the head there is a tube or funnel which
-acts as a locomotive instrument, and propels the animal backwards by
-the forcible ejection of the water which has served the purpose of
-respiration, and can be thrown out with considerable force by the
-contraction of the body. The soft parts are supported by a large
-internal bone or osselet of a very curious structure, which, when dried
-and reduced to powder, forms the substance used by scriveners, termed
-_pounce_. These naked mollusca also possess a membranous bag or sac,
-containing a dark-coloured fluid resembling ink in appearance, which
-they eject into the surrounding water upon the approach of danger, and
-by the obscurity thus induced foil the pursuit of their enemies. This
-fluid, when inspissated, forms the base of the colour termed _sepia_ by
-artists.
-
-[AC] From this arrangement of the organs of prehension around the head,
-this order of mollusca is termed the _Cephalopoda_; _i. e._, the feet
-around the head.
-
-The body of the Nautilus resembles in its essential characters that of
-the Cuttle-fish, and occupies the large outer receptacle of the shell;
-maintaining a connection with the inner compartments by means of the
-membranous siphunculus or tube, which is only partially invested with
-shell. The internal chambers are air-cells, and the animal can fill
-the siphunculus with fluid, or exhaust it at will; the difference thus
-effected in its specific gravity enables it to rise to the surface or
-sink to the bottom with facility. Now if' we imagine a Cuttle-fish
-placed in the outer chamber of a Nautilus-shell, and provided with a
-siphuncule, but having neither ink-bag nor osselet--these organs being
-unnecessary to an animal possessing a chambered shell--we shall have a
-general idea of the nature of the recent species.
-
-The Nautilus is essentially an inhabitant of deep water: it creeps
-along the ground at the bottom of the sea, with its shell upwards like
-the snail; and by means of its arms can proceed with considerable
-speed.[AD]
-
-[AD] See '_Conchologia Systematica_,' vol. ii. p. 302, and '_Elements
-of Conchology_,' p. 22, by Mr. Lovell Reeve, F.L.S., for an admirable
-description of the recent Nautilus, with illustrations.
-
-A large and splendid species of fossil Nautilus is not uncommon in the
-London Clay of the Isle of Sheppey, Sussex, and Hampshire. The chambers
-are often lined with spar or other brilliant mineral matter; and
-polished sections, like those of the Ammonites, admirably display the
-internal structure.[AE]
-
-[AE] See Dr. Buckland's '_Bridgewater Treatise_' for numerous figures
-of Ammonites and Nautili; _plates_ 31 to 34. Consult also '_Medals of
-Creation_,' vol. ii. p. 457.
-
-
-
-
-Note V. Page 27. _Brighton Cliffs._
-
-
-[Sidenote: BRIGHTON CLIFFS.]
-
-The stranger who approaches Brighton by the railroads through deep
-tunnels and cuttings in the chalk, and perceives the town spread
-over the plain and on the sides of a valley of the South Downs, will
-naturally expect to find the sea-shore bounded by chalk-cliffs. But
-a wall of admirable construction, extends from the Steyne to beyond
-Kemptown, and effectually conceals from view the materials that
-compose the site of that part of Brighton; a ramble along the shore to
-Rottingdean is therefore necessary to reveal to the inquiring observer,
-the nature of the strata that flank the southern border of the Downs.
-
-The sketch given in page 27, represents the appearance of part of the
-coast to the east of Kemptown. The base of the cliff to the height of a
-few feet, is seen to consist of the white chalk with its usual layers
-of flint nodules, forming a low wall or terrace, which slopes seaward,
-and extends far into the British channel--probably to the opposite
-coast of France: at low-water a considerable expanse of modern shingle
-and sand is spread over, and in a great measure conceals, the chalk,
-at a few yards distance from the cliff. Upon the terrace of chalk, at
-the height of from ten to fifteen feet above the modern beach, there
-is a bed of pebbles and sand, containing also a considerable number
-of boulders of granite, porphyry, and other crystalline rocks foreign
-to the south-east of England: in fact, a sea-beach, which must have
-been formed at some remote period, in the same manner as the modern
-shingle. Upon this ancient beach are strata of loam, and chalk-rubble,
-with flints partially water-worn, and boulders of sandstone, breccia,
-granite, &c., constituting the upper sixty or eighty feet of the cliff.
-In these beds, and also in the ancient shingle, many teeth and bones of
-mammoths (extinct species of elephant), horse, deer, oxen, and other
-ruminants, and bones of whales, have been discovered.[AF]
-
-[AF] See '_Medals of Creation_,' p. 914.
-
-[Sidenote: THE SUSSEX COAST.]
-
-A few hundred yards beyond Kemptown the inroads of the sea have
-destroyed all vestiges of the strata above described, and the cliffs
-consist of a perpendicular wall of chalk; if we extend our walk to
-Rottingdean, we shall perceive here and there isolated patches of the
-ancient shingle, and of the calcareous strata containing elephants'
-bones.
-
-The appearances described demonstrate the following changes in this
-part of the Sussex coast. _Firstly_, the chalk terrace (_Lign. 9, c_;
-p. 27) on which the ancient shingle (_b_) rests, was on a level with
-the sea for a long period; for this beach must have been accumulated,
-like the modern, by the action of the waves on the then existing chalk
-cliffs. But there must also have been some cause not now in operation,
-by which pebbles, and boulders of granite and other rocks foreign to
-this coast, with bones of extinct mammalia, &c., were thrown up on
-the strand, and imbedded in the beach then in progress of formation.
-These materials were probably brought from some distant part of the
-then continental shores by floating ice: an agency by which delicate
-bones and shells may be transported and deposited without injury amidst
-pebbles and boulders.
-
-_Secondly._ The whole line of coast with the ancient shingle must
-have subsided to such a depth as to admit of the deposition of the
-calcareous materials forming the "Elephant bed;" and from the absence
-of beach and shingle in these strata, it may be inferred that this
-deposition took place in tranquil water: possibly at that period this
-part of the Sussex coast formed a sheltered bay.
-
-_Lastly._ The land was elevated to its present level, and the formation
-of the modern sea-beach and cliffs commenced.[AG]
-
-[AG] See '_Medals of Creation_,' "On the Geological structure of
-Brighton Cliffs," p. 913.
-
-
-
-
-Note VI. Page 38. _Rotaliĉ in Chalk and Flint._
-
-
-[Sidenote: FOSSIL FORAMINIFERA.]
-
-The shells called _Rotaliĉ_ (see _Lign._ 5 and 6, p. 14 and 16) belong
-to a group of marine animals of very simple organization, and which
-present great variety in the form and markings of their testaceous
-coverings; but they all agree in having the sides of the shell pierced
-by numerous holes or foramina; whence the scientific term of the
-Order, _Foraminifera_, is derived: these openings are for the egress
-of delicate filaments, which appear to be organs of progression and
-respiration.
-
-The _Foraminifera_ are, with but few exceptions, exceedingly minute;
-in an ounce of sea-sand, between three and four millions have been
-detected. The body of these animalcules consists of uniform granules
-enclosed in a skin or integument, having one or more digestive sacs
-or cavities; these creatures appear, in fact, to be mere polypes,
-protected by testaceous coverings. Some have but a single cell; others
-have many, disposed in a conical or cylindrical form; many kinds, of
-which the _Rotaliĉ_ are examples, are discoidal involutes, and divided
-internally by septa into distinct chambers:[AH] they resemble in this
-respect the shell of the Nautilus, but are readily distinguished by the
-perforations.
-
-[AH] See '_Wonders of Geology_,' 6th Edit. p. 322.
-
-All the various kinds of _Foraminifera_ swarm in the present seas,
-and were not less numerous in the ancient ocean. We have seen that
-the white chalk almost wholly consists of a few genera of these
-animalcules; and in many strata of sand they are so abundant, that
-a cubic inch of the mass contains upwards of sixty thousand. In the
-_Rotalia_, the body is entirely enclosed within the shell, and occupies
-all the cells; and long, soft, tentacula are sent off through the
-foramina. The shell, therefore, though resembling in form that of
-the Nautilus, is essentially different; for in the latter, the outer
-chamber only is occupied by the body of the animal, the internal ones
-being successively quitted empty dwellings; whereas, in the _Rotaliĉ_
-and analogous _Polythalamia_,[AI] all the cells are contemporaneously
-filled by the soft parts of the animalcule.
-
-[AI] _Polythalamia, many-chambered_, is a general term applied to these
-shells.
-
-[Sidenote: RECENT FORAMINIFERA.]
-
-When the shell is removed, which is readily effected by immersion in
-diluted hydrochloric acid, the body is exposed, and found to consist
-of a series of lobes or sacs, united by a tube corresponding somewhat
-in its position with the siphuncle of the Nautilus, but which is the
-digestive canal. The body of a recent animalcule of this kind, deprived
-of the shell, is figured in _Lign. 23_.
-
-[Illustration: Lign. 23:--The body of a recent animalcule
-allied to the _Rotalia_, deprived of its shell; _highly magnified_.]
-
-Not only the characters of fossil shells of such infinite minuteness
-can be revealed by the microscope, but even the soft parts of the
-animalcules which inhabited them; for these are occasionally preserved,
-and may be demonstrated with as much distinctness as the recent
-examples.[AJ] In flint the soft parts of _Rotaliĉ_, _Textulariĉ_,
-&c., are abundant, and may be seen, with but little preparation, like
-insects in amber: the specimen figured in _Lign. 12_, p. 39, shews
-the body of a _Rotalia_ well defined; the only preparation this atom
-of flint has undergone, is immersion in Canada balsam. To detect such
-delicate structures in chalk requires, however, some experience in
-microscopic manipulation, as the calcareous matter must be dissolved
-in hydrochloric acid, and the animal substance separated from the
-residuum.[AK]
-
-[AJ] See '_Wonders of Geology_,' 6th Edit., p. 322.
-
-[AK] See my '_Memoir on the fossil remains of the soft parts of
-Foraminifera in Chalk, &c._' Philosophical Transactions, 1846, p. 465.
-
-
-
-
-Note VII. Page 43. _Isle of Wight Pebbles._
-
-
-[Sidenote: ISLE OF WIGHT PEBBLES.]
-
-The nodules and veins of flint that are so abundant in the upper
-chalk, have probably been produced by the agency of heated waters
-and vapours; the perfect fluidity of the siliceous matter before its
-consolidation is proved, not only by the sharp moulds and impressions
-of shells and other organisms retained by the flints, but also by the
-presence of numerous remains in the substance of the nodules, and the
-silicified condition of the sponges and other zoophytes which abound in
-the cretaceous strata.
-
-Now although silex, or the earth of flint, is but sparingly soluble in
-water of the ordinary temperature, its solution readily takes places
-in vapour heated a little above that of fused cast iron, as has been
-proved by direct experiment;[AL] and similar effects are being produced
-at the present moment by natural causes. The siliceous deposits thrown
-down by the intermittent boiling fountains, called the Geysers, in
-Iceland, are well known;[AM] and in New Zealand this phenomenon is
-exhibited on a still grander scale. From the crater of the volcanic
-mountain of Tongariro,[AN] which is several thousand feet above the
-level of the sea, jets of vapour and streams of boiling water highly
-charged with silex, are continually issuing forth, and dashing down
-the flanks of the volcano in cascades and torrents, empty themselves
-into the lakes at its base. As the water cools, siliceous sinter is
-deposited in vast sheets, and incrustations of flint form around the
-extraneous substances lying in the course of the thermal streams. Silex
-is also precipitated by the boiling waters in stalagmitic concretions,
-and in nodules resembling in colour and solidity the flints of the
-English chalk. The complete impregnation and silicification of
-organized bodies is attributable to an agency of this kind; and
-although the origin of the siliceous waters that deposited the nodules
-and veins of flint in the chalk is still involved in obscurity, the
-mode in which the latter were formed is satisfactorily elucidated.
-
-[AL] See '_Wonders of Geology_,' p. 100.
-
-[AM] Ibid., p. 95.
-
-[AN] Ibid., p. 98.
-
-[Illustration: Lign. 24:--Zoophytes in Chalk and Flint.
-
- 1. A minute coral from chalk and flint; the lower figure is of the
- natural size.
-
- 2. Branch of a sponge in flint. 3. Pebble enclosing a zoophyte.
-
-]
-
-Of the perfect transmutation into flint of the most delicate organic
-structures, the pebbles strewn along the sea-shore of the south coast
-of England, afford a beautiful illustration; those from the Isle of
-Wight are especially celebrated for their rich and varied colours.
-The most common and interesting are those which exhibit sections of
-Choanites, as in the specimen which suggested the reflections embodied
-in these pages. Other allied forms are scarcely less beautiful; the
-petrified zoophytes called _Siphonia_, which, when living, consisted
-of a soft mass traversed by tubes, for the free ingress and egress of
-the water, often display the internal structure of the original: as
-in the polished transverse section figured above, _Lign. 24, fig. 3_.
-Other bodies of this class occur in the flint, and present interesting
-examples of the zoophytes of the chalk ocean.
-
-But many of the Isle of Wight pebbles exhibit no traces of animal
-structure, yet are valuable and instructive as mineralogical specimens:
-such are the clear and transparent pebbles with bands and veins of
-quartz and chalcedony. Some specimens are as pellucid as rock-crystal;
-others are of a bright yellow, amber, dark-brown, and bluish-black
-colour, and are often mottled with dendritical or arborescent
-manganese. (_Plate IV._) The moss agates, as they are called by the
-lapidaries, are silicified sponges. Small pebbles of pure transparent
-rock-crystal are often found among the shingle in Compton and Sandown
-bays, and have probably been washed out of the wealden strata; for
-similar stones occur in the Tilgate grit, and at Tunbridge Wells: in
-the latter place, they are cut and polished for rings, brooches, &c.
-
-[Illustration: _Plate IV._
-
-_Polished sections of Pebbles._
-
-_Page 86._]
-
-[Sidenote: ZOOPHYTES OF THE CHALK.]
-
-On the shores of the Isle of Wight, pebbles of jasper, resembling those
-from Egypt, and of banded quartz, with arborescent markings, or with
-zones of rich brown, are also met with; these do not appear to have
-originated from the chalk strata.
-
-Pebbles of silicified wood have been collected in Sandown bay by Mr.
-Fowlstone; and water-worn boulders and pebbles of petrified wood,
-bones, &c., are common in Brook bay; rolled masses of the fresh-water
-shelly limestones (Sussex and Purbeck marbles) are also abundant in the
-same localities.[AO]
-
-[AO] All these varieties may be obtained of Mr. Fowlstone, 4, Victoria
-Arcade, Ryde.
-
-
-
-
-Note VIII. Page 45. _Zoophytes of the Chalk._
-
-
-Zoophytes, especially sponges, occur in such prodigious numbers in some
-of the chalk strata, that the nucleus of almost every flint nodule is
-an organic body. In many instances the silex has completely permeated
-the animal substance, as in the pebbles before described; but sometimes
-the sponge is a white calcareous mass, occupying a hollow in the flint:
-a branched specimen of this kind, exposed on breaking a small nodule,
-is represented at _Lign. 24, fig. 2_.
-
-In describing sponge as an animal substance, it may be necessary to
-explain that the sponge in ordinary use is the flexible skeleton of
-a living zoophyte, and was originally invested with a gelatinous or
-slimy matter, which lined all the pores and channels. When alive in
-the water, currents constantly enter the outer pores, traverse all
-the internal inosculating canals, and issue from the larger orifices
-which often project above the surface in perforated papillĉ. By
-the circulation of the sea-water through the porous structure, the
-nutrition of the animated mass is effected; and the modifications
-observable in the number, size, form, and arrangement of the pores,
-canals, and apertures, in the different kinds of this type of
-organization, are subservient to this especial function.
-
-But associated with the true _Poriferĉ_ or sponges, are numerous
-zoophytes which resemble them in form, but are of an entirely distinct
-nature; for they are the fossilized remains of _Polyparia_, that is, of
-the frame-work of an aggregation of polypes, each individual of which
-had an independent existence, although the whole were united by one
-common living integument, like the _Alcyonium_, or dead-men's fingers,
-of our coasts.[AP]
-
-[AP] See '_Medals of Creation_,' p. 251.
-
-[Illustration: Lign. 25:--Flints deriving their forms from the
-zoophytes they enclose.]
-
-[Sidenote: FUNGIFORM FLINTS.]
-
-Among the flints whose forms depend on the organic bodies they enclose,
-are some which bear so close a resemblance in shape to _Fungi_, that
-they are provincially called in Sussex "_petrified mushrooms_;" several
-of them are figured above (_Lign. 25_). In these fossils there are
-openings at the base, and a groove on the margin of the upper part, in
-which the structure of the enclosed body is generally more or less
-distinctly seen; and upon breaking one of these bodies, a section of
-a funnel-shaped zoophyte is obtained. The origin of these flints will
-be understood by reference to the four interesting specimens here
-delineated, one-sixth of the natural size in linear dimensions.
-
-[Illustration: Lign. 26:--Ventriculites from the Chalk, Lewes.
-
- 1. A perfect specimen in Chalk, shewing the external net-like surface.
-
- 2. An expanded specimen, displaying the inner surface studded with cells.
-
- 3. A Ventriculite with the lower part enveloped in Flint.
-
- 4. Part of a Ventriculite; the base invested with Flint: the root-like
- fibres are seen at a.
-
-]
-
-[Sidenote: VENTRICULITES.]
-
-This zoophyte, to which the name of _Ventriculite_ has been given to
-denote its usual shape, was a hollow inverted cone, terminating at
-the base in a point, whence radicles or root-like processes were sent
-off, by which the animal was firmly attached to the rock. The outer
-integument was disposed in meshes like a net (see _Lign. 26, fig.
-1_), and the inner surface was beset with regular circular openings,
-the orifices of tubular cells (_fig. 2_); each of which was probably
-occupied by a polype. The substance of the _Polyparium_, or general
-support of this family of animalcules, which alone occurs in a fossil
-state, appears to have been analogous to that of the soft _Alcyonia_,
-and to have possessed a common irritability; the entire mass
-contracting and expanding, as is the case in many recent zoophytes.[AQ]
-
-[AQ] See '_Wonders of Geology_,' 6th Ed., p. 610; '_Medals of
-Creation_,' p. 273-276; and '_Geological Excursions round the Isle of
-Wight_,' pp. 179-184, for an account of the silicification of these and
-other Zoophytes.
-
-The flints, _figs. 3, 7, 8, 9, Lign. 25_, were evidently formed
-in the manner exemplified in _fig. 3, Lign. 26_; _figs._ 2, 4, 6,
-are illustrated by _fig. 4, Lign. 26_; for the chalk specimens,
-_Lign. 26_, shew that all these flints have been moulded around
-_Ventriculites_, and that their diversity of figure has arisen from
-the quantity of silex that happened to permeate the substance of the
-zoophyte; if but a small portion, flint like _figs._ 2 and 4, were
-the result; if the quantity were considerable, the larger fungiform
-examples were produced.
-
-
-
-
-Note IX. Page 50. _Minute Corals from Chalk._
-
-
-Some layers of chalk are composed of an aggregation of many kinds of
-delicate corals, the interstices being filled up with _Rotaliĉ_ and
-other foraminiferous shells. In the cliffs near Dover there are several
-beds of this nature, well known to collectors for the profusion of
-exquisite specimens they yield to the experienced investigator. _Lign.
-17_, p. 50, represents several varieties from different localities;
-the small figures shew the natural size, and the enlarged ones their
-appearance when magnified. Attached to the surface of shells, and
-sometimes standing erect in crannies of flint nodules, beautiful corals
-may often be detected by the aid of a lens of moderate power. By
-brushing chalk in water, and examining the deposit, delicate fossils of
-this kind may also be obtained.[AR]
-
-[AR] Refer to '_Medals of Creation_,' p. 284, and to '_Wonders of
-Geology_,' _Lecture VI._ p. 588, for a comprehensive view of Recent and
-Fossil Corals.
-
-[Sidenote: NATURE OF CORALS.]
-
-From the close analogy of the fossil corals to existing forms, it would
-not be difficult to give restored figures of the originals. Every
-little branch might be represented fraught with living polypes: in some
-cells the agile inmates might be shown with the mouth expanded, and
-the tentacula in rapid motion; in others withdrawn into their stony
-recesses, and devouring the infinitesimal atoms that constitute their
-food: even their varied hues might be introduced, and thus a vivid
-picture be presented of the microscopic beings which peopled the waters
-of the ancient chalk ocean.
-
-That the Corals, which from their elegance and beauty are preserved in
-almost every cabinet, have been fabricated--or, in other words, built
-up--by polypes, in the same manner as the honey-comb of the bee and
-wasp, is so prevalent yet erroneous an opinion, that I am induced to
-point out its fallacy, by giving a brief account of the formation of
-these substances. The three recent specimens represented in _Lign. 27_
-will serve to illustrate my remarks.
-
-[Illustration: Lign. 27:--Recent Corals.
-
- 1. _Oculina ramea._
-
- 2. _Madrepora muricata._
-
- 3. _Isis hippuris._
-
-]
-
-The coral, _fig. 1_, was an internal axis or skeleton, deposited by the
-soft fleshy integument with which, when living, it was wholly invested;
-in the same manner as are the bones of animals, by the special membrane
-(_periosteum_) that secretes them. This integument lined every cell,
-and the polypes were permanently united to it. When the live coral is
-taken out of the water, the animalcules shrink up and quickly perish;
-their soft parts and the external investing substance putrefy, and the
-stony axis beset with the radiated cells alone remains.
-
-[Sidenote: RECENT CORALS.]
-
-In the example of _Oculina ramea_, or May-blossom Coral, _fig. 1_, from
-the Mediterranean, the cells are large and distinct; in the _Madrepore_
-from the West Indies, _fig. 2_, they are small and very closely
-aggregated.
-
-The specimen of _Isis_ (_fig. 3_) belongs to a group of coral-zoophytes
-in which the polype-cells consist of a substance that is durable, but
-not so hard as coral, and invests an axis composed of a tough flexible
-material, which is exposed at the base of _fig 3_, by the removal of
-the external or cortical part in which the polypes were situated. The
-_Gorgonia_, or Venus's fan, has a similar structure and composition.[AS]
-
-[AS] See '_Wonders of Geology_,' vol. ii. p. 616.
-
-In the _Red Coral_, so largely employed in the manufacture of beads,
-brooches, and other ornaments, not only the animalcules, but also
-their receptacles, are composed of a soft perishable substance. When
-alive, the polypes, as well as the investing fleshy integument, are of
-a delicate bluish tint; the internal calcareous axis alone possesses
-the peculiar red colour. Upon being taken out of the sea, vitality
-quickly ceases, the soft parts decompose, and the beautiful crimson
-stone commonly known as the _true coral_, is obtained free from all
-traces of the soft mass by which it was secreted. Although an actual
-investigation of the facts described can only be instituted near the
-seas of warm climates, yet our coasts abound in certain coral-zoophytes
-in which similar phenomena may readily be observed. Most persons in
-their rambles by the sea-side must have noticed on the fuci, algĉ,
-shells, pebbles, &c., patches of a white earthy substance, which
-when closely examined resemble delicate lace-work. These apparently
-calcareous incrustations are clusters of the zoophytes termed
-the _Flustra_, or sea-mat.[AT] When removed from the water, this
-aggregation of polypes seems coated over with a glossy film or varnish;
-and with a lens of moderate power the surface is seen to be full of
-pores, disposed with much regularity. If viewed under the microscope
-while immersed in sea-water, a very different appearance is presented.
-Every pore is found to be the opening of a cell whence issues a tube
-fringed with several long feelers or arms; these expand, then suddenly
-contract and withdraw into the cell, and again issue forth; the whole
-surface of the Flustra being covered with these hydra-like animalcules.
-The Flustra, therefore, like the corals, constitutes an assemblage of
-polypes, each individual being permanently fixed in a durable cell,
-and the whole attached to a common integument by which the calcareous
-frame-work was secreted and maintained.[AU]
-
-[AT] See '_Wonders of Geology_,' Plate 5.
-
-[AU] See Dr. Johnson's beautiful work on '_British Zoophytes_,' in
-which are numerous figures of various species of Flustra.
-
-
-
-
-
-
-Note X. Page 53. _Infusorial earth from Richmond in Virginia._
-
-
-[Sidenote: INFUSORIAL EARTHS.]
-
-The greatest natural operations are produced by the most simple
-and apparently inadequate agents: for as the illustrious Galileo
-emphatically remarked, "_La nature fait beaucoup avec peu, et ses
-opérations sont toutes également merveilleuses._" The profound thinker
-Hobbes, in the same spirit observes, "The majesty of God appeareth no
-less in small things than in great, and as it exceedeth human sense in
-the immensity of the universe, so also doth it in the smallness of the
-parts thereof." This sublime truth is strongly impressed on the mind
-of the geological inquirer, who perceives that whole countries and
-mountain ranges of great elevation and extent, are wholly composed of
-the aggregated remains of beings of such infinite minuteness that but
-for the powerful optical instruments of modern times, their presence
-would never have been suspected.
-
-A few years only have elapsed since the sagacious Ehrenberg first
-drew attention to this subject, and pointed out the proper method of
-investigation;[AV] and so rapid has been the progress of discovery in
-this department of science, that _infusorial deposits_, as these beds
-of fossil animalcules are designated, have been detected in every
-quarter of the globe. A fact equally unexpected and remarkable has also
-been established, namely, that at the present moment similar minute
-living agents are largely contributing to the increase of the solid
-materials of the crust of our planet.
-
-[AV] See '_Medals of Creation_,' p. 244, for instructions for the
-microscopical examination of earths, chalk, &c.
-
-[Sidenote: RICHMOND EARTH.]
-
-The infusorial earth of Virginia, alluded to in the text, is a
-yellowish siliceous clay, forming a deposit from twelve to fifteen
-feet in thickness, upon which the towns of Richmond and Petersburgh
-are built. The surface of the country over which it extends is
-characterized by a scanty vegetation, owing to the siliceous nature of
-the soil dependent on the minute organisms of which it almost entirely
-consists. When a few grains of this earth are properly prepared for
-microscopic examination, immense numbers of the shields or cases of
-animalcules are visible under a magnifying power of 300 diameters; in
-fact, the merest stain left by the evaporation of water in which some
-of the marl has been mixed, teems with these fossil remains.[AW]
-
-[AW] Specimens of Infusorial earths, prepared for the microscope, may
-be obtained of Mr. Topping, 4, New Winchester Street, Pentonville Hill,
-New Road, London.
-
-These organisms are of exquisite structure, and comprise many
-species and genera. The most beautiful and abundant are the circular
-shields, termed _Coscinodisci_ (sieve-like disks), which are elegant
-saucer-shaped cases, elaborately ornamented with hexagonal apertures
-disposed in curves, somewhat resembling the engine-turned sculpturing
-of a watch; these shells are from 1/1000 to 1/100 of an inch in
-diameter. A segment of one of these disks, highly magnified, is
-represented in _Lign. 18, fig. 2_. The body of the living animalcule
-was protected and enclosed by a pair of these concave shells, the
-perforations admitting of the exsertion of filaments or tentacula.
-This species of _Coscinodiscus_ abounds in the present seas, and
-constitutes no inconsiderable proportion of the food of Pectens and
-other testaceous mollusca.[AX]
-
-[AX] See '_Thoughts on Animalcules_,' p. 103.
-
-All the animalcules found in the Richmond earth are marine, and most
-of them belong to genera, and many to existing species; although the
-position of the American strata proves that they are referable to a
-period of immense antiquity.
-
-In Germany, beds of a white infusorial earth, resembling magnesia
-in appearance, and termed _Bergh-mehl_, or fossil farina, occur at
-Bilin, and several other places: at San Fiora in Tuscany, near Egra
-in Bohemia, in the Bermudas, Barbadoes, &c., similar deposits have
-been discovered; all being composed of the shields of various kinds of
-animalcules. But I must not extend these remarks, and will only add a
-few observations on the infusorial earth of Barbadoes, which has but
-recently been brought under the notice of geologists by Sir Robert
-Schomburgk, and is especially interesting for the exquisite beauty and
-variety of its organisms, and the circumstances under which the deposit
-occurs.
-
-[Sidenote: FOSSIL INFUSORIA OF BARBADOES.]
-
-Barbadoes, an island of the West Indies, is about twelve miles in
-length from north to south, and consists of coral reefs, capped in one
-district by tertiary sandstones and limestones, which attain a height
-of 1200 feet above the sea. Over the rest of the island, coral reefs
-form the entire surface, which is divided by vertical walls of coral,
-some of them nearly 200 feet high, into six terraces, indicating as
-many periods of upheaval. In the lowest reef, Indian hatchets have
-been found twenty feet above high water mark; shewing that the last
-movement, at least, took place within the human period. The tertiary
-strata are more or less inclined, and in many places vertical, and
-contorted. Strata of marl, several hundred feet thick, predominate; and
-there are beds of bituminous coal, sandstone, clays, and ferruginous
-sands. Arenaceous limestone containing teeth of sharks, spines of
-echini, and shells, forms the summit of a hill nearly 1,000 feet high.
-The white marls abound in 300 species of the most beautiful siliceous
-infusoria; many are peculiar, others the same as occur in the Richmond
-earth, and some belong to recent species.[AY]
-
-[AY] Sir R. H. Schomburgk: Brit. Assoc. 1847.
-
-
-
-
- THE END.
-
-
- * * * * *
-
-
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