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
Had I, in reasoning _a priori_, asserted, That all mineral bodies might
have been melted without change, when under sufficient compression,
there might have arisen, in the minds of reasoning men, some doubt with
regard to the certainty of that proposition, however probable it were to
be esteemed: But when, in reasoning _a posteriori_, it is found that all
mineral bodies have been actually melted, then, all that is required to
establish the proposition on which I have founded my theory, is to
see that there must have been immense degrees of compression upon the
subjects in question; for we neither know the degree of heat which had
been employed, nor that of compression by which the effect of the heat
must have been modified.
Now, in order to see that there had been immense compression, we have
but to consider that the formation of the strata, which are to be
consolidated, was at the bottom of the ocean, and that this place is to
us unfathomable. If it be farther necessary to show that it had been at
such unfathomable depth strata were consolidated, it will be sufficient
to observe, it is not upon the surface of the earth, or above the level
of the sea, that this mineral operation can take place; for, it is there
that those consolidated bodies are redissolved, or necessarily going
into decay, which is the opposite to that operation which we are now
inquiring after; therefore, if they were consolidated in any other place
than at the bottom of the sea, it must have been between that place of
their formation and the surface of the sea; but that is a supposition
which we have not any reason to make; therefore, we must conclude that
it was at the bottom of the ocean those stratified bodies had been
consolidated.]
To conclude this long chemico-mineral disquisition, I have specimens in
which the mixture of calcareous, siliceous, and metallic substances,
in almost every species of concretion which is to be found in mineral
bodies, may be observed, and in which there is exhibited, in miniature,
almost every species of mineral transaction, which, in nature, is found
upon a scale of grandeur and magnificence. They are nodules contained in
the whin-stone, porphyry, or basaltes of the Calton-hill, by Edinburgh;
a body which is to be afterwards examined, when it will be found to have
flowed, and to have been in fusion, by the operation of subterraneous
heat.
Public-domain text, read in full here on John Shaqi.
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