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
Here are two things to be considered; the interesting facts described
by our author, and the inference that he would have us draw from those
facts. It would appear from the facts, that the body of schistus below,
and that of lime-stone above, had not undergone the same disordering
operations, or by no means in the same degree. But our author has formed
another conclusion; he says, that these lime-stone strata must have been
formed precisely in the place and order in which they lie at present;
and the reason for this is, because these strata appeared to him to
follow perfectly the contour of the summit of this mountain. Now, had
there been in the top of this mountain a deep hollow encompassed about
with the schistus rock; and had this cavity been now found filled with
horizontal strata, there might have been some shadow of reason for
supposing those strata to have been deposited upon the top of the
mountain. But to suppose, _first_, that shells and corals should be
deposited upon the convex summit of a mountain which was then covered by
the sea; _secondly_, that these moveable materials should remain upon
the summit, while the sea had changed its place; and, _lastly_, that
those shells and corals left by the sea upon the top of a mountain
should become strata of solid limestone, and have also metallic veins
in it, certainly holds of no principle of natural philosophy that I am
acquainted with. If, therefore, such an appearance as this were to be
employed either in illustration or confirmation of a theory, it
would itself require to be explained; but this is a task that this
cosmologists does not seem willing to undertake.
He has formed a hypothesis for explaining the general appearance of that
which was once the bottom of the sea being now found forming the summits
of our mountains; but surely this philosopher will acknowledge, that
those natural appearances, in any particular place, will be the same,
whether we suppose the bottom of the sea to have been raised, as in the
present theory, or the surface of the sea to have sunk according to his
hypothesis. For, it is equally easy to suppose a portion of the earth
to have been raised all this height, as to suppose all the rest of the
surface of the globe to have sunk an equal space, while a small portion
of the bottom of the sea, remaining here and there fixed in its place,
became the highest portion of the globe. Consequently, whatever evidence
this philosopher shall find in support of his theory of the present
earth, (a subject which it is not our purpose to examine) it cannot be
allowed that he has here brought any argument capable of disproving the
elevation of the bottom of the sea; a supposition which other theories
may require.
Public-domain text, read in full here on John Shaqi.
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