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
This system need not be considered in detail; the foundation of it is
laid in such defiance of the principles of geometry and mechanics, that
the architect, notwithstanding all the fertility of his invention, and
all the resources of his genius, was never able to give any solidity to
the structure.
But it will be said, that we may take a part of the system, without
venturing on the whole, and may suppose that the earth, or at least
the external crust of it, has been fluid by fire, though we do not
inquire into the cause of this fire, or into the manner in which it was
produced.
It is indeed true, that, when this is done, we have not the same sort
of absurdity to encounter that we met with in the Neptunian system, and
that the Volcanic theory does not, like it, come into direct collision
with an axiom of geometry. There are, nevertheless, great objections
to it; for though all the phenomena of the mineral kingdom attest a
fluidity of igneous origin, yet it is a fluidity that was never more
than partial; and though it has been over all the earth, has been over
it in succession only. Besides, we are not entitled to assume the
existence, and again the disappearance of such a great quantity of
heat, without assigning some cause for the change.
435. Since, then, neither the hypothesis of the Neptunists or the
Vulcanists, affords any good explanation of the figure of the earth, or
such a one as can connect it with the other appearances in its natural
history, it remains to inquire, whether the system that supposes a
partial and successive fluidity, like Dr Hutton's, has any resource for
explaining this great phenomenon.
Of this subject Dr Hutton has not treated; and when I was first made
acquainted with his system, it appeared to me a very serious objection
to it, that it did not profess to give an explanation of so important
a fact as the oblate figure of the earth. On considering the matter
more closely, however, I found that there were principles contained
in it from which a very satisfactory solution (and, I think, the only
satisfactory solution) of that difficulty might be deduced. This
solution I shall endeavour to explain, in as far, at least, as is
necessary for the purpose of general illustration.
It is laid down in Dr Hutton's theory, that the surface of the earth is
perpetually changed by the _detritus_ of the land; and that from the
materials thus afforded, new horizontal strata are perpetually formed
at the bottom of the sea. If this be true, and if the alternations of
decay and renovation have been often repeated, it is certain, that the
figure of the earth, whatever it may have originally been, must be
brought at length to coincide with the spheroid of equilibrium.
436. Here it is necessary to remark, that the expressions, _figure of
the earth_, and _surface of the earth_ are each of them occasionally
taken in two different senses.
Public-domain text, read in full here on John Shaqi.
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