Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4) — John Shaqi
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
It must not be here objected, That there are frequently found siliceous
crystals and amethysts containing water; and that it is impossible
to confine water even in melted glass. It is true, that here, at the
surface of the earth, melted glass cannot, in ordinary circumstances, be
made to receive and inclose condensed water; but let us only suppose a
sufficient degree of compression in the body of melted glass, and we
can easily imagine it to receive and confine water as well as any
other substance. But if, even in our operations, water, by means of
compression, may be made to endure the heat of red hot iron without
being converted into vapour, what may not the power of nature be able to
perform? The place of mineral operations is not on the surface of the
earth; and we are not to limit nature with our imbecility, or estimate
the powers of nature by the measure of our own.[10]
[Note 10: This is so material a principle in the theory of consolidating
the strata of the earth by the fusion of mineral substances, that I beg
the particular attention of the reader to that subject. The effect of
compression upon compound substances, submitted to increased degrees of
heat, is not a matter of supposition, it is an established principle
in natural philosophy. This, like every other physical principle, is
founded upon matter of fact or experience; we find, that many compound
substances may with heat be easily changed, by having their more
volatile parts separated when under a small compression; but these
substances are preserved without change when sufficiently compressed.
Our experiments of this kind are necessarily extremely limited; they
are not, however, for that reason, the less conclusive. The effects of
increasing degrees of heat are certainly prevented by increasing degrees
of compression; but the rate at which the different effects of those
powers proceed, or the measure of those different degrees of increase
that may be made without changing the constitution of the compound
substance, are not known; nor is there any limit to be set to that
operation, so far as we know. Consequently, it is a physical principle,
That the evaporation of volatile substances by heat, or the reparation
of them from a compound substance, consequently the effect of fire in
changing that compound substance, may be absolutely prevented by means
of compression.
It now remains to be considered, how far there is reason to conclude
that there had been sufficient degrees of compression in the mineral
regions, for the purpose of melting the various substances with which we
find strata consolidated, without changing the chemical constitution of
those compound substances.
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