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
Our author is in a mistake in supposing that Dr Black had written any
thing upon the subject; he had only suggested the argument of this
example of mineral alkali to me, as I have mentioned; and, the use I
made of that argument was to corroborate the example I had given of sal
gem. If, therefore, our author does not deny the inference from the
state of that mineral alkali, his observation upon it must refer to
something which this other example of his is to prove on the opposite
side, or to support the aqueous instead of the igneous theory; and, this
is a subject which I am always willing to examine in the most impartial
manner, having a desire to know the true effect of aqueous solution in
the consolidation of mineral bodies, and having no objection to allow it
any thing which it can possibly produce, although denying that it can do
every thing, as many mineralists seem to think.
The question, with regard to this example of our author's of a mineral
alkali with its water of crystallization, must be this, Whether those
saline bodies had been concreted by the evaporation of the aqueous
solvent with which they had been introduced, or by the congelation of
that saline substance from a fluid state of fusion; for, surely, we are
not to suppose those bodies to have been created in the place and state
in which we find them. With regard to the evaporation or separation
of the aqueous solvent, this may be easily conceived according to the
igneous theory; but, the aqueous theory has not any means for the
producing of that effect in the mineral regions, which is the only place
we are here concerned with. Therefore, this example of a concreted body
of salt, whatever it may prove in other respects, can neither diminish
the evidence of my Theory with regard to the igneous origin of stony
substances, nor can it contribute to support the opposite supposition of
an aqueous origin to them.
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