Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
When men of science reason upon subjects where the ideas are distinct
and definite, with terms appropriated to the ideas, they come to
conclusions in which there is no difference of opinion. It is otherwise
in physical subjects, where things are to be assimilated, in being
properly compared; there, things are not always compared in similar and
equal circumstances or conditions; and there, philosophers often draw
conclusions beyond the analogy of the things compared, and thus judge
without data. When, for example, they would form the physical induction,
with regard to the effect of fire or water upon certain substances in
the mineral regions, from the analogy of such events as may be observed
upon the surface of the earth, they are apt to judge of things acting
under different circumstances or conditions, consequently not producing
similar effects; in which case, they are judging without reason, that
is, instead of inductive reasoning from actual data or physical truth,
they are forming data to themselves purely by supposition, consequently,
so far as these, imagined data may be wrong, the physical conclusion, of
these philosophers may be erroneous.
It is thus that philosophers have judged, with regard to the effects of
fire and water upon mineral substances below the bottom of the sea,
from what their chemistry had taught them to believe concerning bodies
exposed to those agents in the atmosphere or on the surface of the
earth. If in those two cases the circumstances were the same, or
similar, consequently the conditions of the action not changed, then,
the inductive reasoning, which they employ in that comparison, would be
just; but, so far as it is evidently otherwise, to have employed that
inductive conclusion for the explanation of mineral appearances, without
having reason to believe that those changed circumstances of the case
should not make any difference in the action or effect, is plainly to
have transgressed the rules of scientific reasoning; consequently,
instead of being a proper physical conclusion, it is only that imperfect
reasoning of the vulgar which, by comparing things not properly analysed
or distinguished, is so subject to be erroneous. This vague reasoning,
therefore, cannot be admitted as a part of any geological or mineral
theory. Now I here maintain, that philosophers have judged in no other
manner than by this false analogy, when they conclude that water is the
agent by which mineral concretions have been formed. But it will be
proper to state more particularly the case of that misunderstanding
among mineral philosophers.
Public-domain text, read in full here on John Shaqi.
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