Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
If he means by this to say, that a precipitation without solution
would take place the sooner the more inadequate the menstruum was to
dissolve the whole, the proposition may be true; but will be of no
use to explain the crystallization of minerals, (the very object he
has in view,) because to crystallization, it is not a bare subsidence
of particles suspended in a fluid, but it is a passage from chemical
solution to non-solution, or insolubility, that is required.
If, on the other hand, he means to say, that the solution actually took
place more quickly, and was more immediately followed by precipitation,
because the quantity of the menstruum was insufficient, this is to
assert, that the weaker the cause, the more instantaneous will be its
effect.
Of two propositions the one of which is nugatory, and the other absurd,
it is not material to inquire which the author had in view.
NOTE VII. § 16.
_Compression in the mineral regions._
163. It is worthy of remark, that the effects ascribed to compression
in the Huttonian Theory, very much resemble those which Sir ISAAC
NEWTON supposes to be produced in the sun and the fixed stars by
that same cause. "Are not," says he, "the sun and fixed stars great
earths, vehemently hot, whose heat is conserved by the greatness of
the bodies, and the mutual action and reaction between them, and the
light which they emit; and _whose parts are kept from fuming away,
not only by their fixity, but also by the vast weight and density of
the atmospheres incumbent upon them, and very strongly compressing
them_."[73]
[Footnote 73: Newton's Optics, Query 11.]
164. The fact of water boiling at a lower temperature under a less
compression, is sufficient to justify the supposition, that bodies may
be made by pressure to endure extreme heat, without the dissipation
of their parts, that is, without evaporation or combustion. A further
_postulatum_ is introduced in Dr Hutton's theory, namely, that compound
bodies, such as carbonate of lime, when the compression prevents their
separation, may admit of fusion, notwithstanding that the fixed part
may be infusible when separated from the volatile. This assumption is
supported by the analogical fact of the fusion of the carbonate of
barytes, as mentioned in the text.
165. In a region where the action of heat was accompanied with such
compression as is here supposed, there could be no fire, properly so
called, and no combustion; this is admitted by Dr Hutton, and it is
therefore a fallacious argument which is brought against his theory,
from the impossibility of fire being maintained in the bowels of the
earth. This impossibility is precisely what he supposes; and yet Mr
Kirwan's arguments are directed, not against the existence of heat in
the interior of the earth, but against the existence of burning and
inflammation.
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