CHAPTER I.

Produced by Tom Cosmas compiled from images made available

by The Internet Archive.

Transcriber Note

Text emphasis is denoted by _Italics_ and =Bold=. Whole and fractional

parts are displayed as 123-4/5.

[Illustration: Cape Trinity on the Saguenay. A salient point of

Laurentian Gneiss, on an old fiord of Pliocene erosion (p. 99). (_From a

Photograph by Henderson._)]

SOME SALIENT POINTS

IN THE

SCIENCE OF THE EARTH

BY

SIR J. WILLIAM DAWSON C.M.G., LL.D., F.R.S., F.G.S., &c.

_WITH FORTY-SIX ILLUSTRATIONS_

[Illustration]

NEW YORK

HARPER & BROTHERS PUBLISHERS

1894

PREFACE.

The present work contains much that is new, and much in correction

and amplification of that which is old; and is intended as a closing

deliverance on some of the more important questions of geology, on the

part of a veteran worker, conversant in his younger days with those

giants of the last generation, who, in the heroic age of geological

science, piled up the mountains on which it is now the privilege of

their successors to stand.

J. W. D.

_Montreal_ 1893.

CONTENTS.

CHAPTER I. Page

The Starting-point 3

CHAPTER II.

World-making 9

CHAPTER III.

The Imperfection of the Geological Record 39

CHAPTER IV.

The History of the North Atlantic 57

CHAPTER V.

The Dawn of Life 95

CHAPTER VI.

What May Be Learned from Eozoon 135

CHAPTER VII.

The Apparition and Succession of Animal Forms 169

CHAPTER VIII.

The Genesis and Migrations of Plants 201

CHAPTER IX.

The Growth of Coal 233

CHAPTER X. PAGE

The Oldest Air-breathers 257

CHAPTER XI.

Markings, Footprints, and Fucoids 311

CHAPTER XII.

Pre-determination in Nature 329

CHAPTER XIII.

The Great Ice Age 345

CHAPTER XIV.

Causes of Climatal Change 363

CHAPTER XV.

The Distribution of Animals and Plants As Related

to Geographical and Geological Changes 401

CHAPTER XVI.

Alpine and Arctic Plants in Connection With

Geological History 425

CHAPTER XVII.

Early Man 459

CHAPTER XVIII.

Man in Nature 481

LIST OF ILLUSTRATIONS.

Page

Cape Trinity on the Saguenay _Frontispiece_

Folding of the Earth's Crust _To face_ 9

Cambro-Silurian Sponges " 39

Map of the North Atlantic " 57

Nature-print of Eozoon " 95

Laurentian Hills, Lower St. Lawrence 100

Section from Petite Nation Seigniory to St. Jerome 101

The Laurentian Nucleus of the American Continent 103

Attitude of Limestone at St. Pierre 109

Weathered Eozoon and Canals _To face_ 112

" " " 113

Group of Canals in Eozoon 115

Amœba and Actinophrys 119

Minute Foraminiferal Forms 123

Section of a Nummulite 127

Portion of Shell of Calcarina 128

Weathered Eozoon with Oscular tubes _To face_ 135

Diagram showing different States of Fossilization

of a Cell of a Tabulate Coral 139

Slice of Crystalline Lower Silurian Limestone 141

Walls of Eozoon penetrated with Canals 141

Joint of a Crinoid 145

Shell from a Silurian Limestone, Wales 146

Casts of Canals of Eozoon in Serpentine 147

Canals of Eozoon 147

Primordial Trilobites _To face_ 169

Primitive Fishes " 184

Devonian Forest " 201

Coal Section in Nova Scotia 233

Skeleton of _Hylonomus Lyelli_ _To face_ 257

Footprints of _Hylopus Logani_ " 260

Humerus and Jaws of _Dendrerpeton_ " 272

Reptiliferous Tree " 276

Microsaurian, restored " 278

_Dolichosoma longissimum_, restored " 286

_Pupa_ and _Conulus_ " 288

Millipedes and Insect " 296

Footprints of _Limulus_ " 311

_Rusichnites Grenvillensis_ " 322

Restoration of _Protospongia tetranema_ " 329

Giant Net-sponge " 336

Boulder Beach, Little Metis " 345

Palæogeography of North America " 383

Distribution of Animals in Time " 401

Tuckerman's Ravine and Mount Washington " 425

Pre-historic Skulls " 459

Primitive Sculpture " 481

TABLE OF GEOLOGICAL HISTORY.

Non-Geological readers will find in the following table a condensed

explanation of the more important technical terms used in the following

pages. The order is from older to newer.

GREATER SYSTEMS OF CHARACTERISTIC FOSSILS.

PERIODS. FORMATIONS.

Archæan or Eozoic

Pre-Laurentian

Laurentian Protozoa Protophyta

Palæozoic

Huronian { Crustaceans Algæ

Cambrian { Molluscs Cryptogamous

Cambro-Silurian[A] { Worms and

Silurian[B] { Corals, etc, Gymnospermous

Devonian Fishes Plants.

Carboniferous Amphibians

Permian

Mesozoic

Triassic { Reptiles Pines and

Jurassic { Birds Cycads

Cretaceous { Earliest Mammals. Trees of modern

types.

Kainozoic or Tertiary

Eocene Higher Mammals

Miocene of extinct forms

Pliocene Recent Mammals Modern Plants,

Pleistocene and

Modern Man.

[A] Ordovician of Lapworth.

[B] Salopian of Lapworth.

_THE STARTING-POINT._

DEDICATED TO THE MEMORY OF

PROF. ROBERT JAMESON,

Of the University of Edinburgh, my first Teacher in Geology,

whose Lectures I attended, and whose kind Advice and

Guidance I enjoyed, in the Winter of 1840-1841.

Headlands and Spurs--Popular Papers on Leading Topics--Revisiting Old

Localities--Dedications--General Scope of the Work

CHAPTER I.

_THE STARTING-POINT._

An explorer trudging along some line of coast, or traversing some

mountain region, may now and then reach a projecting headland, or bold

mountain spur, which may enable him to command a wide view of shore

and sea, or of hill and valley, before and behind. On such a salient

point he may sit down, note-book and glass in hand, and endeavour to

correlate the observations made on the ground he has traversed, and

may strain his eyes forward in order to anticipate the features of

the track in advance. Such are the salient points in a scientific

pilgrimage of more than half a century, to which I desire to invite

the attention of the readers of these papers. In doing so, I do not

propose to refer, except incidentally, to subjects which I have already

discussed in books accessible to general readers, but rather to those

which are imbedded in little accessible transactions, or scientific

periodicals, or which have fallen out of print. I cannot therefore

pretend to place the reader on all the salient points of geological

science, or even on all of those I have myself reached, but merely to

lead him to some of the viewing-places which I have found particularly

instructive to myself.

For similar reasons it is inevitable that a certain personal element

shall enter into these reminiscences, though this autobiographical

feature will be kept as much in the background as possible. It is

also to be anticipated that the same subject may appear more than

once, but from different points of view, since it is often useful to

contemplate certain features of the landscape from more than one place

of observation.

To drop the figure, the reader will find in these papers, in a plain

and popular form, yet it is hoped not in a superficial manner, some

of the more important conclusions of a geological worker of the old

school, who, while necessarily giving attention to certain specialties,

has endeavoured to take a broad and comprehensive view of the making of

the world in all its aspects.

The papers are of various dates; but in revising them for publication

I have endeavoured, without materially changing their original form,

to bring them up to the present time, and to state any corrections or

changes of view that have commended themselves to me in the meantime.

Such changes or modifications of view must of necessity occur to every

geological worker. Sometimes, after long digging and hammering in some

bed rich in fossils, and carrying home a bag laden with treasures, one

has returned to the spot, and turned over the _débris_ of previous

excavation, with the result of finding something rare and valuable,

before overlooked. Or, in carefully trimming and chiselling out the

matrix of a new fossil, so as to uncover all its parts, unexpected

and novel features may develop themselves. Thus, if we were right or

partially right before, our new experience may still enable us to

enlarge our views or to correct some misapprehensions. In that spirit

I have endeavoured to revise these papers, and while I have been able

to add confirmations of views long ago expressed, have been willing to

accept corrections and modifications based on later discoveries.

In the somewhat extended span of work which has been allotted to me,

I have made it my object to discover new facts, and to this end have

spared no expenditure of time and labour; but I have felt that the

results of discoveries in the works of God should not be confined to a

coterie, but should be made public for the benefit of all. Hence I have

gladly embraced any opportunities to popularise my results, whether in

lectures, articles, popular books, or in the instruction of students,

and this in a manner to give accurate knowledge, and perhaps to attract

the attention of fellow-workers to points which they might overlook if

presented merely in dry and technical papers. These objects I have in

view in connection with the present collection of papers, and also the

fact that my own pilgrimage is approaching its close, and that I desire

to aid others who may chance to traverse the ground I have passed over,

or who may be preparing to pass beyond the point I have reached.

To a naturalist of seventy years the greater part of life lies in the

past, and in revising these papers I have necessarily had my thoughts

directed to the memory of friends, teachers, guides, and companions in

labour, who have passed away. I have therefore, as a slight token of

loving and grateful remembrance dedicated these papers to the memory

of men I have known and loved, and who, I feel, would sympathise with

me in spirit, in the attempt, however feeble, to direct attention to

the variety and majesty of those great works of the Creator which they

themselves delighted to study.

Since the design of these papers excludes special details as to

Canadian geology, or that of those old eastern countries to which I

have given some attention, I must refer for them to other works, and

shall append such reference of this kind as may be necessary. At the

same time it will be observed that as my geological work has been

concerned most largely with the oldest and newest rocks of the earth,

and with the history of life rather than with rocks and minerals, there

must necessarily be some preponderance in these directions, which might

however, independently of personal considerations, be justified by

the actual value of these lines of investigation, and by the special

interest attaching to them in the present state of scientific discovery.

Having thus defined my starting-point, I would now with all respect and

deference ask the reader to accompany me from point to point, and to

examine for himself the objects which may appear either near, or in the

dim uncertain distance, in illustration of what the world is, and how

it became what it is. Perhaps, in doing so, he may be able to perceive

much more than I have been able to discover; and if so, I shall

rejoice, even if such further insight should correct or counteract

some of my own impressions. It is not given to any one age or set of

men to comprehend all the mysteries of nature, or to arrive at a point

where it can be said, there is no need of farther exploration. Even in

the longest journey of the most adventurous traveller there is an end

of discovery, and, in the study of nature, cape rises beyond cape and

mountain behind mountain interminably. The finite cannot comprehend

the infinite, the temporal the eternal. We need not, however, on that

account be agnostics, for it is still true that, within the scope of

our narrow powers and opportunities, the Supreme Intelligence reveals

to us in nature His power and divinity; and it is this, and this alone,

that gives attraction and dignity to natural science.

_WORLD-MAKING._

DEDICATED TO THE MEMORY OF

ADAM SEDGWICK AND SIR RODERICK IMPEY MURCHISON,

Whose joint Labours carried

our Knowledge of the History of the Earth

two Stages farther back,

and whose Differences of Opinion served to

render more glorious their Victories.

[Illustration: Fig. 1. Diagram illustrating Folding of the Crust

of the Earth.--(_a_) Undisturbed crust. (_b_) Primary depression

and deposition. (_c_) Mountain-making folds with their relations

to an upper and lower magma. Fig. 2. Result of folding, faulting,

and denudation, as seen at Cascade Mountain, Western Canada (after

McConnell, p. 33).]

Some Salient Points in the Science of the Earth · 第 1 / 18 章