CATASTROPHISM IN GEOLOGY.

Mr. Clarence King was probably not a little surprised to learn from

the Tribune that in his most suggestive address on "Catastrophism and

the Evolution of Environment," he had turned the guns of Geology upon

Biology; and that in calling attention to the influence of periods of

accelerated change in environment upon exposed types of life he had

swept away the "fundamental doctrines upon which has been built the

scheme of development by natural selection and the survival of the

fittest." Certainly nothing in the address betrays any consciousness

of possible effects of that sort. And it is quite probable also that

Mr. King will have to suffer some annoyance from seeing his name set

up at gaze, like Joshua's moon in Ajalon, by the unscientific press

generally, as that of the newest champion of orthodoxy against the

leaders of modern scientific thought: a penalty which scientific men

always have to pay for emphasizing neglected truths.

Mr. King certainly deals some telling blows against the position of

the stricter school of Uniformitarians in geology, and brings into

prominence a much neglected element in the struggle for existence; but

there is no scientific revolution threatened, nor are any crumbs of

comfort spread for those endeavoring to arrest the natural drift of

scientific progress.

The issue between Mr. King and the sticklers for uniformity in rates

of geological change is simply this: In the reaction against the

sweeping cataclysms, the sudden wipings out of whole creations and

the sudden introductions of new worlds of life believed in by earlier

geologists, the modern English school has come to look upon time and

the slower modifications of the earth's surface, now observable, with

the struggle for existence under easy conditions, as the chief factors

in geological change and its accompanying variations in the forms of

life. Mr. King, on the other hand, insists that in so doing they have

taken too little account of catastrophic changes, that is, widespread

and sudden movements of sea and land. In other words, he raises rapid

change of environment from the subordinate place it has hitherto

occupied in the scheme of historical development, and gives special

emphasis to the grand geologic movements which have to do with such

changes.

In this Mr. King has unquestionably rendered good service to the

science he has done so much to extend and honor in the field; while

the illustrations from American geology which he brings to bear on the

subject are as likely as his sturdy opinions to attract attention.

Yet we are inclined to think that in some things he has allowed his

enthusiasm to run away with him. The stolid self-confidence of

extreme Uniformitarians has tempted him to exaggerate the periodic

accelerations of geologic and biologic movement, and to overstate

their effects quite as much as others have underestimated them;

and when he charges the followers of Lyell with intellectual

near-sightedness and a lack of "the very mechanism of imagination,"

they may possibly be able to retort not unjustifiably that he has

mistaken the natural foreshortening of the geological vista due to

distance for actual brevity; and that his belief in the abruptness and

suddenness of the great changes which the earth's strata record, may

be due to his own lack of sustained imaginative power for grasping and

interpreting all the evidences of the enormous time really involved.

But this is a question not of imaginative capacity but of logical

deduction from observed facts; and however abrupt the beginning of

some of the great geologic movements may have been, their subsequent

progress cannot in all cases have been so rapid as to allow of their

being called catastrophic in any ordinary acceptation of the term.

Take, for example, the alleged catastrophe which marked the close of

the mesozoic age in the West. Of this movement Mr. King remarks: "In

a quasi-uniformitarian way, 20,000 or 30,000 feet of sediment had

accumulated in the Pacific and 14,000 in the [American] mediterranean

sea; when these regions, which, during the reception of sediment,

had been areas of subsidence, suddenly upheaved, the doming up of the

middle of the continent quite obliterating the mediterranean sea and

uniting the two land masses into one. The catastrophe which removed

this sea resulted in the folding up of mountain ranges 20,000 and

40,000 feet in height, thereby essentially changing the whole climate

of the continent."

That this great change occurred, and was attended with an obliteration

of the wonderful reptilian and avian fauna of the mesozoic age, is

most true: that it occurred suddenly does not appear. On the contrary,

there is evidence to show that the prodigious folding up of mountain

ranges involved could not have proceeded with sufficient rapidity to

turn the course of a stream of water. It happened that one of those

folds--one which, had no denudation been going on meanwhile,

would have lifted its crest higher than the highest peak of the

Himalayas--lay directly across the course of the Colorado river. The

river held its course uninterruptedly, sawing its way through the

uplift until six vertical miles of rocky strata had risen past it. At

no time, therefore, could the rapidity of motion in the bulging strata

have exceeded the capacity of the river to wear away the obstruction,

and the bulge was fifty miles across! We do not know how rapidly a

river may sink its channel through such a rising barrier; but we do

know that a process of that nature cannot legitimately be described

as swift or sudden. And surely it requires not less intellectual

far-sightedness and imaginative faculty to carry the mind across the

enormous stretch of time involved in such a change slowly wrought--a

period during which at least three vertical miles of the rising

mountain fold was worn down by rain and atmospheric abrasion--as to

mass the continental doming, the mountain folding, and the attendant

life changes together as a convulsive "catastrophe."

Mr. King, however, is not a Catastrophist of a very violent sort. He

shelves among the errors of the past the belief in such cataclysms as

Cuvier believed in, involving world-wide destruction of all life--"the

mere survival of a prehistoric terror, backed up by breaks in the

palaeontological record and protected within those safe cities of

refuge, the Cosmogonies;" though he rejects as equally unsatisfactory

the mild affirmations of the Uniformitarians, that existing rates

of change and indefinite time are enough to account for all the

geological record. With our present light, he holds, geological

history seems to be a dovetailing together of the two ideas. "The ages

have had their periods of geological serenity, when change progressed

in the still, unnoticeable way, and life through vast lapses of

time followed the stately flow of years; drifting on by insensible

gradations through higher and higher forms, and then all at once

a part of the earth suffered short, sharp, destructive revolution

unheralded as an earthquake or volcanic eruptions." Thus stated, his

position does not seem to be radically different from that of

the broader Uniformitarians, except that he marks the periods of

accelerated physical change, and not those of comparative quiescence,

as the dominant ones in their influence on life-change. He takes

high and strong ground, too, in insisting that it is the business

of geology not simply to decipher and map out the changes which have

taken place in the configuration of the globe and in its climatic

conditions, but also to investigate and fix the rates of change. And

when the evolution of environment takes form as a distinct branch of

geology, he expects to witness a marked modification in the dominant

views of biologists. Its few broad laws will include "neither the

absolute uniformitarianism of Lyell and Hutton, Darwin and Haeckel,

nor the universal catastrophism of Cuvier and the majority of

teleogists." "Huxley alone among prominent evolutionists opens the

door for a union of the residue of truth in the two schools, fusing

them in his proposed evolutional geology."

So, on looking back over a trail of thirty thousand miles of

geological travel, Mr. King is impelled to say that Mr. Huxley's

far-sighted view perfectly satisfies his interpretation of the broad

facts of the American continent.

Of Mr. King's observations in regard to plasticity of physical

structure in connection with rapidly changing environment and the

struggle for existence, we propose to speak at another time.

* * * * *

The great stone monuments of England, like Stonehenge, are supposed,

by Mr. James Fergusson, to be military trophies, erected in the time

of King Arthur on the battle fields by the victorious armies.

* * * * *

Scientific American, Vol. XXXVII.—No. 2. [New Series.], July 14, 1877 A Weekly Journal of Practical Information, Art, Science, Mechanics, Chemistry, and Manufactures · 第 28 / 213 题