A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
Both these authorities supposed the creatures whose remains they studied
to have perished suddenly in the mighty flood whose awful current, as
they supposed, gouged out the modern valleys and hurled great blocks of
granite broadcast over the land. And they invoked similar floods for the
extermination of previous populations.
It is true these scientific citations had met with only qualified
approval at the time of their utterance, because then the conservative
majority of mankind did not concede that there had been a plurality of
populations or revolutions; but now that the belief in past geologic
ages had ceased to be a heresy, the recurring catastrophes of the great
paleontologists were accepted with acclaim. For the moment science and
tradition were at one, and there was a truce to controversy, except
indeed in those outlying skirmish-lines of thought whither news from
headquarters does not permeate till it has become ancient history at its
source.
The truce, however, was not for long. Hardly had contemporary
thought begun to adjust itself to the conception of past ages of
incomprehensible extent, each terminated by a catastrophe of the
Noachian type, when a man appeared who made the utterly bewildering
assertion that the geological record, instead of proving numerous
catastrophic revolutions in the earth's past history, gives no warrant
to the pretensions of any universal catastrophe whatever, near or
remote.
This iconoclast was Charles Lyell, the Scotchman, who was soon to be
famous as the greatest geologist of his time. As a young man he had
become imbued with the force of the Huttonian proposition, that present
causes are one with those that produced the past changes of the
globe, and he carried that idea to what he conceived to be its logical
conclusion. To his mind this excluded the thought of catastrophic
changes in either inorganic or organic worlds.
But to deny catastrophism was to suggest a revolution in current
thought. Needless to say, such revolution could not be effected without
a long contest. For a score of years the matter was argued pro and con.,
often with most unscientific ardor. A mere outline of the controversy
would fill a volume; yet the essential facts with which Lyell at last
established his proposition, in its bearings on the organic world, may
be epitomized in a few words. The evidence which seems to tell of past
revolutions is the apparently sudden change of fossils from one stratum
to another of the rocks. But Lyell showed that this change is not always
complete. Some species live on from one alleged epoch into the next. By
no means all the contemporaries of the mammoth are extinct, and numerous
marine forms vastly more ancient still have living representatives.
Public-domain text, read in full here on John Shaqi.
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