Discourses: Biological & Geological: EssaysHuxley, Thomas Henry
Science
Discourses: Biological & Geological: Essays
Huxley, Thomas Henry
Biology; Geology
I find three, more or less contradictory, systems of geological thought,
each of which might fairly enough claim these appellations, standing side
by side in Britain. I shall call one of them CATASTROPHISM, another
UNIFORMITARIANISM, the third EVOLUTIONISM; and I shall try briefly to
sketch the characters of each, that you may say whether the
classification is, or is not, exhaustive.
By CATASTROPHISM, I mean any form of geological speculation which, in
order to account for the phenomena of geology, supposes the operation of
forces different in their nature, or immeasurably different in power,
from those which we at present see in action in the universe.
The Mosaic cosmogony is, in this sense, catastrophic, because it assumes
the operation of extra-natural power. The doctrine of violent upheavals,
_débâcles_, and cataclysms in general, is catastrophic, so far as it
assumes that these were brought about by causes which have now no
parallel. There was a time when catastrophism might, pre-eminently, have
claimed the title of "British popular geology"; and assuredly it has yet
many adherents, and reckons among its supporters some of the most
honoured members of this Society.
By UNIFORMITARIANISM, I mean especially, the teaching of Hutton and of
Lyell.
That great though incomplete work, "The Theory of the Earth," seems to me
to be one of the most remarkable contributions to geology which is
recorded in the annals of the science. So far as the not-living world is
concerned, uniformitarianism lies there, not only in germ, but in blossom
and fruit.
If one asks how it is that Hutton was led to entertain views so far in
advance of those prevalent in his time, in some respects; while, in
others, they seem almost curiously limited, the answer appears to me to
be plain.
Hutton was in advance of the geological speculation of his time, because,
in the first place, he had amassed a vast store of knowledge of the facts
of geology, gathered by personal observation in travels of considerable
extent; and because, in the second place, he was thoroughly trained in
the physical and chemical science of his day, and thus possessed, as much
as any one in his time could possess it, the knowledge which is requisite
for the just interpretation of geological phenomena, and the habit of
thought which fits a man for scientific inquiry.
It is to this thorough scientific training that I ascribe Hutton's steady
and persistent refusal to look to other causes than those now in
operation, for the explanation of geological phenomena.
Thus he writes:--"I do not pretend, as he [M. de Luc] does in his theory,
to describe the beginning of things. I take things such as I find them at
present; and from these I reason with regard to that which must have
been."[2]
[Footnote 2: _The Theory of the Earth_, vol. i. p. 173, note.]
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