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
Now, it is not at all obvious, to what physical cause this phenomenon
is to be ascribed. The earth, as it exists at present, has none of the
conditions that render the assumption of the figure of equilibrium in
any way necessary to it. Constituted as it is, its parts cohere with
forces incomparably too great to obey the laws of statical pressure,
or to assume any one figure rather than another, on account of the
centrifugal tendency which results from its revolution on its axis.
There is no necessity that its superficies should be every where level,
or perpendicular to the direction of gravity, nor that every two
columns, standing on the same base, any where within it, and reaching
from thence to any two points of the surface, should be of such weights
as precisely to balance one another. Neither of these, indeed, is at
all conformable to fact. They are, however, the very suppositions on
which the determination of the spheroid of equilibrium is founded; and
as they certainly do in no degree belong to the earth, it seems strange
that the result deduced from them should be in any way applicable to
it. This coincidence remains, therefore, to be explained; and it must
greatly enhance the merit of any geological system, if it can connect
this great and enigmatical phenomenon with the other facts in the
natural history of the earth.
430. To establish such a connection, has, accordingly, been a favourite
object with geologists, whether they have embraced the Neptunian or
Volcanic theory: both have thought that they were entitled to suppose
the primeval fluidity of the globe, the one by water, and the other
by fire; and in whatsoever way that fluidity was produced, the result
of it could be no other than the spheroidal figure of the whole mass,
agreeably to the laws of hydrostatics. If in this fluid state the earth
was homogeneous, the spheroid would be accurately elliptical, and the
compression at the poles would be 1/230 of the radius of the equator;
if the fluid was denser toward the centre, the flattening would be
less: and in either case, the body, as it acquired solidity, may be
supposed to have retained its spheroidal figure with little variation.
But though the fluidity of the earth will account for the phenomenon
of its oblate figure, it may reasonably be questioned, whether this
fluidity can be admitted, in consistency with other appearances.
According to what is established above, none of the appearances in the
mineral kingdom indicate more than a partial fluidity in any former
condition of the earth. The present strata, made up as they are of the
ruins of former strata, though softened by heat, have not been rendered
fluid by it, and have even possessed their softness in parts, and in
succession, not altogether, nor at the same time.
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