[Illustration: From a Painting by James Hall, Esq. Engraved by S. Williams.
STRATA OF RED SANDSTONE, SLIGHTLY INCLINED, RESTING ON VERTICAL SCHIST, AT THE SICCAR POINT, BERWICKSHIRE.
TO ILLUSTRATE UNCONFORMABLE STRATIFICATION. See page 60.
_"The mind seemed to grow giddy by looking so far into the abyss of time; and while we listened with earnestness and admiration to the philosopher who was now unfolding to us the order and series of these wonderful events, we became sensible how much farther reason may sometimes go than imagination can venture to follow."_--PLAYFAIR, Biography of Hutton.]
A MANUAL OF ELEMENTARY GEOLOGY: OR, THE ANCIENT CHANGES OF THE EARTH AND ITS INHABITANTS
AS ILLUSTRATED BY GEOLOGICAL MONUMENTS.
BY SIR CHARLES LYELL, M.A. F.R.S.
AUTHOR OF "PRINCIPLES OF GEOLOGY," "TRAVELS IN NORTH AMERICA," "A SECOND VISIT TO THE UNITED STATES," ETC. ETC.
"It is a philosophy which never rests--its law is progress: a point which yesterday was invisible is its goal to-day, and will be its starting post to-morrow." EDINBURGH REVIEW, No. 132. p. 83. July, 1837.
_FOURTH AND ENTIRELY REVISED EDITION._ ILLUSTRATED WITH 500 WOODCUTS.
LONDON: JOHN MURRAY, ALBEMARLE STREET. 1852.
LONDON: SPOTTISWOODES and SHAW, New-street-Square.
PREFACE TO THE FOURTH EDITION.
In consequence of the rapid sale of the third edition of the "Manual," of which 2000 copies were printed in January last, a new edition has been called for in less than a twelvemonth. Even in this short interval some new facts of unusual importance in palaeontology have come to light, or have been verified for the first time. Instead of introducing these new discoveries into the body of the work, which would render them inaccessible to the purchasers of the former edition, I have given them in a postscript to this Preface (printed and sold separately), and have pointed out at the same time their bearing on certain questions of the highest theoretical interest.[v-A]
As on former occasions, I shall take this opportunity of stating that the "Manual" is not an epitome of the "Principles of Geology," nor intended as introductory to that work. So much confusion has arisen on this subject, that it is desirable to explain fully the different ground occupied by the two publications. The first five editions of the "Principles" comprised a 4th book, in which some account was given of systematic geology, and in which the principal rocks composing the earth's crust and their organic remains were described. In subsequent editions this book was omitted, it having been expanded, in 1838, into a separate treatise called the "Elements of Geology," first re-edited in 1842, and again recast and enlarged in 1851, and entitled "A Manual of Elementary Geology."
Although the subjects of both treatises relate to geology, as their titles imply, their scope is very different; the "Principles" containing a view of the _modern_ changes of the earth and its inhabitants, while the "Manual" relates to the monuments of _ancient_ changes. In separating the one from the other, I have endeavoured to render each complete in itself, and independent; but if asked by a student which he should read first, I would recommend him to begin with the "Principles," as he may then proceed from the known to the unknown, and be provided beforehand with a key for interpreting the ancient phenomena, whether of the organic or inorganic world, by reference to changes now in progress.
Table of contents (by pages)
- 1: A Manual of Elementary Geology by Lyell
- 2: Abstract of the Principles of Geology
- 3: And full of a species of Lingula
- 4: Chelonian foot prints in Old Red Sandstone
- 5: Mantell has proposed for it the generic name of Telerpeton
- 6: Rather than to a Batrachian or Chelonian
- 7: Triassic Mammifer Microlestes antiquus Plieninger
- 8: Previous to this discovery of Professor Plieninger
- 9: Dicotyledonous leaves in lower cretaceous strata
- 10: And other Quadrumana had been met with
- 11: As much was known of the Mammalia of the Stonesfield Oolite
- 12: Of the Eocene period has depended
- 13: Even in the Eocene strata of Europe
- 14: Xxii B In my Anniversary Address
- 15: Why the position of marine strata
- 16: Classification of tertiary formations
- 17: Chronological classification of Pleistocene formations
- 18: The Wealden divisible into Weald Clay
- 19: Permian or magnesian limestone group
- 20: And explanation of names and synonyms
- 21: On the different ages of the volcanic rocks
- 22: 2d edition in octavo 1832
- 23: A manual of elementary geology
- 24: The geologist soon comes to a different conclusion
- 25: Metalliferous and non metalliferous formations
- 26: Are found almost everywhere imbedded in stratified rocks
- 27: And they commonly traverse deposits of volcanic tuff
- 28: Which constitute the plutonic family
- 29: Whether crystalline or fossiliferous
- 30: The term hypogene for this purpose
- 31: Although it does not belong to pure alumine
- 32: Or of calcareous sand cemented together
- 33: Magnesian limestone or dolomite
- 34: Or in that of micaceous sandstones
- 35: Diagonal or Cross Stratification
- 36: Or those nearest to Monte Calvo
- 37: Slab of ripple marked new red sandstone from Cheshire
- 38: When he reflects on the origin of stratification
- 39: A living species of Spatangus
- 40: Recent Spatangus with the spines removed from one side
- 41: In the family Bacillaria see fig
- 42: The species of Diatomaceae or Infusoria
- 43: We may distinguish a freshwater formation
- 44: Of the Ancylus is usually thinner
- 45: Such as that seen at b in Ancillaria fig
- 46: The seed vessels and stems of Chara
- 47: 33 A But changes like these in the Lym Fiord
- 48: But becoming stony near Kelloway
- 49: At the depth of about 230 fathoms
- 50: The concretionary action may spread upwards into a part of A
- 51: And exhibits when broken the same texture as native graphite
- 52: Yet when the whole is lapidified
- 53: Naturally imbedded in sediment
- 54: Is intimately combined with alumine
- 55: The cellular and the woody fibre
- 56: Why the position of marine strata
- 57: The beds of one of the oldest of the fossiliferous deposits
- 58: On the southern skirts of the Grampians
- 59: And advancing upon older strata
- 60: Representing a section at Wallsend
- 61: Even where the argillaceous substrata are hard at first
- 62: Apparent horizontality of inclined strata
- 63: Section illustrating the structure of the Swiss Jura
- 64: An anticlinal axis forms a ridge
- 65: Although this chert could not have been brittle as now
- 66: Strata are said to be unconformable
- 67: Junction of unconformable strata near Mons
- 68: Upon reaching the strata of sandstone c
- 69: 64 A The walls of the fissure are scored by grooves
- 70: That we are able to explain the phenomena of denudation
- 71: The base of gneiss varies in height
- 72: Where a series of palaeozoic strata
- 73: Faults and denuded coal strata
- 74: No evidence may remain of the denuding operation
- 75: Section of inland cliff at Abesse
- 76: All bound together by a crystalline calcareous cement
- 77: It was necessary first to remove a mass of breccia
- 78: And the same is resumed to the south beyond the town of Noto
- 79: And more exposed to denudation in an open sea
- 80: As the adjoining calcareous rocks
- 81: Lavas of Auvergne resting on alluviums of different ages
- 82: And as if included in the subjacent formation
- 83: Derived from overlying beds of gravel
- 84: In like manner we may sometimes compare the gravel
- 85: And might be strewed over with littoral sand and pebbles
- 86: Roads or shelves in the outer alluvial covering of the hill
- 87: In Glen Roy and only one in Glen Spean
- 88: The several groups of plutonic
- 89: And the horizontality of the floetz
- 90: That granite as well as trap was of igneous origin
- 91: This covering of crystalline stone
- 92: In a subsequent chapter on the plutonic rocks
- 93: And tertiary hypogene formations
- 94: On the three principal tests of relative age superposition
- 95: As if the supply of sediment had failed in that direction
- 96: The extent of some single zoological provinces
- 97: Including the remains of Mediterranean species
- 98: We behold six groups superimposed one upon the other
- 99: Cambrian and older fossiliferous strata
- 100: Classification of tertiary formations
- 101: Contemporaneous with those of Bordeaux
- 102: But in separating families and genera
- 103: Have each their peculiar fauna
- 104: A revolution thus effected is rarely
- 105: The utility of the testacea is
- 106: The term Pliocene from pleion
- 107: Whereas even the Newer Pliocene
- 108: Is composed of greenish indurated tuff
- 109: They decidedly represent a more arctic fauna
- 110: Have there shown that fluviatile strata
- 111: Loess of the Valley of the Rhine
- 112: The loess is met with near Basle
- 113: Credner and I obtained in a quarry at Tonna
- 114: And partly to the newer pliocene
- 115: Resulting from the liquefaction of icebergs
- 116: Consisting of gneiss for the most part unrounded
- 117: Are found huge angular fragments of mica schist
- 118: Except a minute Paludina now inhabiting France
- 119: Section of concentric beds west of Cromer
- 120: Chalk with regular layers of chalk flints
- 121: With its characteristic marine fossils
- 122: Even the southern extension of the drift
- 123: Or would be regularly stratified by marine currents
- 124: Sand and loam with Mya truncata
- 125: An unstratified and unfossiliferous mass
- 126: If the cold of the glacial epoch came on slowly
- 127: Another specimen of the same quadruped
- 128: Some derived from the antarctic continent
- 129: And are called the lateral moraines
- 130: Which flow along the surface of glaciers
- 131: And almost everywhere on the Jura
- 132: All parts of Chiloe and the intervening strait
- 133: Chronological classification of Pleistocene formations
- 134: Remnants of ancient fluviatile deposits occur
- 135: Fossil remains of the extinct mammiferous genera Megatherium
- 136: Such as Nucula Cobboldiae fig
- 137: Newer Pliocene strata of Sicily
- 138: While the marine serpulae adhered to them
- 139: Like those of Girgenti Agrigentum
- 140: Caverns filled with marine breccias
- 141: Ossiferous breccias are not confined to Europe
- 142: I ascertained that the Megatherium
- 143: Is by no means confined to the mammalia
- 144: Older pliocene and miocene formations
- 145: And the lower the Coralline Crag
- 146: Have never been found in the white or coralline division
- 147: Like the living Voluta Magellanica
- 148: In which no Balaenidae have yet been met with
- 149: One freshwater and the other marine Limnea palustris
- 150: The scattered patches of faluns are of slight thickness
- 151: The total number of mollusca from the faluns
- 152: Which attains a great thickness in the valley of the Bormida
- 153: And partly in the faluns of Touraine
- 154: Although they may all be termed Eocene
- 155: Lower freshwater limestone and marl
- 156: Like those of Kleyn Spauwen and Etampes
- 157: Tritonium flandricum De Koninck
- 158: Which separates the Allier from the Sioule
- 159: At the bottom are foliated marls
- 160: Containing the Cypris in abundance
- 161: Of caddis worms the larvae of Phryganea
- 162: More than 50 feet of thinly laminated gypseous marls
- 163: The Amphitragulus elegans of Pomel
- 164: In the neighbourhood of Aurillac
- 165: FOOTNOTES 175 A Bulletin des Sci
- 166: 191 B There are no pebbles or coarse sand in the gypsum
- 167: Paleotherium magnum was of the size of a horse
- 168: And called by the French geologists Miliolite limestone
- 169: Called calcaire grossier and calcaire siliceux
- 170: Bagshot and Bracklesham Bagshot Heath
- 171: Both in the cliffs of Headon Hill and Hordwell
- 172: Nummulites Nummularia laevigatus
- 173: The fossil species of the island of Sheppey
- 174: And shells of the genera Terebellum
- 175: And Cyrena cuneiformis are very common
- 176: Nummulitic formation of the Alps and Pyrenees
- 177: D'Orbigny to the genus Orbitoides
- 178: Due to the decomposition of the orbitoides
- 179: Maestricht beds and Faxoe limestone
- 180: Among the cephalopoda of Faxoe
- 181: Portion of Baculites Faujasii
- 182: 4 Illustrations Hippurites Mortoni
- 183: Geographical extent and origin of the While Chalk
- 184: Coprolites of fish called Iulo eido copri
- 185: The Fucus giganteus of Solander
- 186: Sometimes intermixed with greensand
- 187: Among these may be mentioned many Hippurites
- 188: Are wholly unlike the hippurite itself
- 189: But covered with marls abounding in Inocerami
- 190: 222 A D'Orbigny's Paleontologie Francaise
- 191: The Wealden divisible into Weald Clay
- 192: Very characteristic of the Wealden
- 193: The calcareous sandstone and grit of Tilgate Forest
- 194: Sphenopteris gracilis Fitton
- 195: Containing shells of the genera Paludina
- 196: Were overspread with fluviatile mud
- 197: Freshwater Upper Purbeck
- 198: And annihilated in the Wealden
- 199: In regard to the geographical extent of the Wealden
- 200: Denudation of the chalk and wealden
- 201: Section across Valley of Seine
- 202: Like the detached rocks before mentioned at Senneville
- 203: And this again by the Greensand No
- 204: The Ouse corresponds to the Darent
- 205: Of the gorge of the river Adur
- 206: Under the provincial name of firestone
- 207: The upper greensand is represented fig
- 208: Which are portions of smaller concentric ellipses
- 209: Cleared away before any part of the lower greensand No
- 210: Lowest chalk or chalk marl upper greensand wanting
- 211: And clayey beds of fluvio marine and shallow water origin
- 212: At the commencement of the Eocene epoch
- 213: Ammonites and Belemnites Lower Oolite
- 214: Great Oolite and Stonesfield slate
- 215: May be mentioned the Ostrea deltoidea fig
- 216: In the annexed figure of an Astrea
- 217: Among which the Eunomia radiata fig
- 218: After the parasitic serpulae were full grown
- 219: Especially near Minchinhampton
- 220: Is convex in the Stonesfield specimens
- 221: Broderip Didelphys Bucklandi see fig
- 222: Portion of a fossil fruit of Podocarya magnified
- 223: And Pholadomya fidicula fig
- 224: Although usually conformable to the oolite
- 225: Commonly called Ichthyodorulite
- 226: One specimen of Ichthyosaurus platyodon
- 227: So there may have been formerly some saurians proper to salt
- 228: Not unfrequently there are layers of these coprolites
- 229: The nervures of the wings of neuropterous insects fig
- 230: Arenaceous matter replaces the clay
- 231: Oolite and Lias of the United States
- 232: Trias or new red sandstone group
- 233: Wanting in England Muschelkalk Muschelkalk
- 234: Such as Equisetites columnaris
- 235: Both in the neighbourhood of Axmouth
- 236: Provisionally named Chirotherium by Professor Kaup
- 237: Transverse section of tooth of Labyrinthodon Jaegeri
- 238: In the eastern Grampians of Scotland
- 239: The boundaries of the Runn have been enlarged by subsidence
- 240: Through the narrow Straits of Babelmandeb
- 241: According to Professor Hitchcock
- 242: Among the supposed bipedal tracks
- 243: In the rocks of the Connecticut
- 244: Permian or magnesian limestone group
- 245: Brecciated and pseudo brecciated 2
- 246: Agassiz has called Heterocercal
- 247: Dolomitic conglomerate of Bristol
- 248: Brongniart to be allied to Cycas
- 249: And the same may be said of the Permian fauna
- 250: Coal measures Strata of shale
- 251: Ferns and trunks of trees abound without any Stigmariae
- 252: Adolphe Brongniart Lepidostrobus
- 253: Brongniart includes several genera
- 254: Stigmaria attached to a trunk of Sigillaria
- 255: Being now indurated to stone and shale
- 256: In what is called an open work at Parkfield Colliery
- 257: A slanting trunk was exposed in Craigleith quarry
- 258: And above them is an underclay
- 259: Allied to Serpula or Spirorbis
- 260: In the lower coal measures of Coalbrook Dale
- 261: CARBONIFEROUS GROUP continued
- 262: Consists of granitic rocks hypogene
- 263: Subsequently laid open by denudation
- 264: There are thirteen seams of anthracitic coal
- 265: And this again by micaceous sandstone c
- 266: Chiefly by the discharge of carburetted hydrogen
- 267: Horner in the Cannel coal of Fifeshire
- 268: Goldfuss under the generic name of Archegosaurus
- 269: In the European Cheirotherium
- 270: A siphuncled and chambered shell
- 271: Rest unconformably on a base of gneiss
- 272: Scale of Holoptychius nobilissimus
- 273: The genera Dipterus and Diplopterus are so named
- 274: The Cyathophyllum caespitosum fig
- 275: Devonian Strata in the United States
- 276: Formerly referred to the Devonian era
- 277: And the intervening Aymestry limestone
- 278: And the lowest or mudstone beds
- 279: Also in the Aymestry and Wenlock limestones
- 280: From the Aymestry limestone to the bottom of the series
- 281: Perhaps the young of Pentamerus oblongus
- 282: Occurs in the Llandeilo beds in Wales
- 283: The abundance of orthidiform brachiopoda
- 284: Tabular view of fossiliferous strata
- 285: Near Berlin
- 286: With bright green Greensand
- 287: Calcareous slates Chiefly freshwater
- 288: And white marls Rhyncosaurus
- 289: And many parts Cyrtoceras
- 290: The aqueous or fossiliferous rocks having now been described
- 291: Except in the nodules of amygdaloids
- 292: Called glassy felspar and compact felspar
- 293: Werner first distinguished augite from hornblende
- 294: At other times solely of augite
- 295: Augite is the predominant mineral
- 296: The upper part is usually scoriaceous
- 297: CLAYSTONE and CLAYSTONE PORPHYRY
- 298: It passes into compact felspar and hornstone
- 299: Pyroxene being Hauey's name for augite
- 300: A soft and earthy variety of trap
- 301: Or in horizontal sheets intercalated between strata
- 302: Ground plan of greenstone dike traversing sandstone
- 303: Syenitic greenstone dike of Naesodden
- 304: Having a porcellanous aspect and a bluish grey colour
- 305: One of the greenstone dikes of Antrim
- 306: Columnar and globular structure
- 307: As in the Cheese grotto at Bertrich Baden
- 308: The trappean rocks first studied in the north of Germany
- 309: And the associated trappean rocks
- 310: What is said of the plutonic formations
- 311: Called Barranco de las Angustias
- 312: We have to account for the Caldera and the great Barranco
- 313: That where the great gorge or Barranco occurs
- 314: Long sealed up at the bottom of the caldera
- 315: If a volcanic rock rests upon an aqueous deposit
- 316: A basaltic dike at Quarrington Hill
- 317: It has been remarked that in Auvergne
- 318: The more felspathic lavas have been first emitted
- 319: The loftiest of the Cyclopian islets
- 320: It is found to consist largely of tufaceous strata
- 321: Dikes or veins at the Punta del Nasone on Somma
- 322: Newer Pliocene Period Val di Noto
- 323: A district of extinct volcanos near Olot
- 324: Which flows near the town of Olot
- 325: As is seen between Olot and Cellent
- 326: Flowing from a ridge of hills on the east of Olot
- 327: When Olot was destroyed by an earthquake
- 328: Layers of trachytic tuff are interstratified
- 329: On arriving at the village of Gemund
- 330: Which is called the Gemunder Maar
- 331: The tufaceous alluvium called trass
- 332: Are supposed to have become silicified
- 333: Or the contiguous lacustrine strata
- 334: Bone bed of the Tour de Boulade
- 335: At the bottom of the valley of the Couze
- 336: The bones found in this alluvium
- 337: There are beds of gravel in Velay
- 338: On the northern side of the Plomb du Cantal
- 339: Consisting exclusively of tuff
- 340: Trappean rocks are associated with New Red Sandstone
- 341: And intersecting veins of greenstone
- 342: The stone resembles a sandy claystone of the trap family
- 343: So that volcanic and plutonic rocks
- 344: Granite having a cuboidal and rude columnar structure
- 345: Among these black schorl or tourmaline
- 346: A granite composed of hornblende
- 347: Like that of hornstone or chert
- 348: Veins of granite in talcose gneiss
- 349: In the gneiss of Tronstad Strand
- 350: So as to overlie fossiliferous shale and limestone
- 351: On the different ages of the plutonic rocks
- 352: Recent and Pliocene plutonic rocks
- 353: And converted into crystalline schists of the hypogene class
- 354: The strata in both resting on plutonic rocks
- 355: Or become melted down into plutonic and volcanic rocks
- 356: And has a saccharoid structure
- 357: Granite sending veins into Silurian strata and Gneiss
- 358: If we admit that solid hypogene rocks
- 359: Metamorphic or Hypogene schists
- 360: And the beds of conglomerate No
- 361: Or schistose hypogene formations
- 362: And more especially hornblende schist
- 363: Composed chiefly of actinolite
- 364: And hypogene limestone that of Carrara for example
- 365: Mica schist alternates with chlorite schist
- 366: D D are lines of slaty cleavage
- 367: Parallel planes of cleavage intersecting curved strata
- 368: And even the foliation of mica schist and gneiss
- 369: Speaking of the planes of slaty cleavage
- 370: Have confounded it with the ancient hornblende schist
- 371: Sends forth veins into a coarse argillaceous schist
- 372: By sulphuretted hydrogen and muriatic acid gases
- 373: The forms of stratification in metamorphic rocks
- 374: Is sometimes converted into hornblende schist
- 375: In the islands of Ponza and Palmarola
- 376: Or any other member of the hypogene class
- 377: Or Liassic Cretaceous strata of the Hypogene class
- 378: Argillaceous and siliceous sandstones
- 379: Studer in the highest of the Bernese Alps
- 380: Uniformity of mineral character in Hypogene rocks
- 381: In the hypogene formations generally
- 382: Fossil shells or corals may often lose their carbonic acid
- 383: Both hypogene and fossiliferous
- 384: Vertical sections of the mine of Huel Peever
- 385: Some lodes occur where the vertical plates
- 386: Alternate with ores and veinstones
- 387: When lodes are many fathoms wide
- 388: Many of these bodies occur as veinstones
- 389: Before the Devonian strata were deposited
- 390: The tin lodes are newer than the elvans
- 391: On the chronology of the volcanic and hypogene formations
- 392: 501 B FOOTNOTES 489 A Principles
- 393: In plutonic rocks by relative position
- 394: Auvergne freshwater formations
- 395: On tertiary strata near Berlin
- 396: On mountains of Caernarvonshire
- 397: Chemical and mechanical deposits
- 398: Creeps in coal mines described
- 399: On volcanos of Sandwich Islands
- 400: Elvans of Ireland and Cornwall
- 401: On changes of Wealden testacea
- 402: Freshwater formations of Auvergne
- 403: Rocks in connection with mineral veins
- 404: Of Siebengebirge and Westerwald
- 405: On footprints of Cheirotherium
- 406: On conversion of coal into lignite
- 407: Mammifer in trias near Stuttgart
- 408: On mineral composition of Somma
- 409: On subdivisions of cretaceous series
- 410: Plutonic and sedimentary rocks
- 411: Composed of fossil zoophytes and shells
- 412: On fossil of Caradoc sandstone
- 413: Steno on classification of rocks
- 414: Superposition of aqueous deposits
- 415: Tuffs on Wrekin and Caer Caradoc
- 416: On horizontal strata in Russia
- 417: Memoir of the life of the late bishop stanley
- 418: By henry lord bishop of exeter
- 419: The scholar the gipsy and the priest
- 420: Fergusson writes very dispassionately
- 421: As the Earl of Ellesmere declares
- 422: By lord chief justice campbell
- 423: Period between the persian and the peloponnesian wars
- 424: And illustrated with 520 Woodcuts
- 425: The right honourable george grenville
- 426: JENKINSON first EARL OF LIVERPOOL
- 427: Naval and Military Technological Dictionary
- 428: Assisted by colonel rawlinson
- 429: Handbook to the antiquities and sculpture there
- 430: Handbook for England and Wales
- 431: Handbook for the Environs of London
- 432: Is into Saurichthys Mougeotii
