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
132. The circumstance, however, which gives to this theory its
peculiar character, and exalts it infinitely above all others, is
the introduction of the principle of pressure, to modify the effects
of heat when applied at the bottom of the sea. This is in fact the
key to the grand enigma of the mineral kingdom, where, while one
set of phenomena indicates the action of fire, another set, equally
remarkable, seems to exclude the possibility of that action, by
presenting us with mineral substances, in such a state as they could
never have been brought into by the operation of the fires we see at
the surface of the earth. These two classes of phenomena are reconciled
together, by admitting the power of compression to confine the volatile
parts of bodies when heat is applied to them, and to force them,
in many instances, to undergo fusion, instead of being calcined or
dissipated by burning or inflammation. In this hypothesis, which some
affect to consider as a principle gratuitously assumed, there appears
to me nothing but a very fair and legitimate generalization of the
properties of heat. Combustion and inflammation are chemical processes,
to which other conditions are required, besides the presence of a high
temperature. The state of the mineral regions makes it reasonable
to presume, that these conditions are wanting in the bowels of the
earth, where, of consequence, we have a right to look for nothing but
expansion and fusion, the only operations which seem essential to
heat, and inseparable from the application of it, in certain degrees,
to certain substances. Though this principle, therefore, had no
countenance from analogy, the admirable simplicity, and the unity,
which it introduces into the phenomena of geology, would sufficiently
justify the application of it to the theory of the earth.
As another excellence of this theory, I may, perhaps, be allowed to
remark, that it extends its consequences beyond those to which the
author of it has himself adverted, and that it affords, which no
geological theory has yet done, a satisfactory explanation of the
spheroidal figure of the earth.[40]
[Footnote 40: NOTE XXV.]
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