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
not very considerably,) by which means it returns whenever the force
is removed, and vibrates backward and forward, till it is reduced to
rest. Were it required to remove the stone from its place, it might be
most easily done, by cutting off a part from one side, or blowing it
away by gunpowder; the stone would then lose its balance, would tumble
from its pedestal, and might roll to a considerable distance. Now, what
art is here supposed to perform, nature herself in time will probably
effect. If the waste on one side of this great mass shall exceed that
on the opposite in more than a certain proportion, and it is not likely
that that proportion will be always maintained, the equilibrium of the
Logan stone will be subverted, never to return. Thus we perceive how
motion may be produced by the combined action of the decomposition and
gravitation of large masses of rock.
[Footnote 178: I do not presume so far as to say, that all
rocking-stones are produced by natural means: I have not sufficient
information to justify that assertion; but the great size of that
at the Land's End, its elevated position, and the approaches toward
something of the same kind which are to be seen in other parts of that
shore, prove that it is no work of art. They who ascribe it to the
Druids, do not consider the rapidity with which the Cornish granite
wastes, nor think how improbable it is, that the conditions necessary
to a rocking-stone, whether produced by nature or art, should have
remained the same for sixteen or seventeen hundred years.]
356. Besides the gradual waste to which stones exposed to the
atmosphere are necessarily subject, those of a great size appear to be
liable to splitting, and dividing into large portions, no doubt from
their weight. This may be observed in almost all stones that happen to
be in such circumstances as we are now considering; and from this cause
the subversion of their balance may be more sudden, and of greater
amount, than could be expected from their gradual decay.
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