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Hutton, James, 1726-1797

"Theory of the Earth, Volume 1 (of 4)"


Thus, it will appear, that, to consolidate strata formed at the bottom
of the sea, in the manner now considered, operations are required
unnatural to this place; consequently, not to be supposed, in order to
support a hypothesis.
But now, instead of inquiring how far water may be supposed instrumental
in the consolidation of strata which were originally of a loose
texture, we are to consider how far there may be appearances in those
consolidated bodies, by which it might be concluded, whether or not the
present state of their consolidation has been actually brought about by
means of that agent.
If water had been the menstruum by which the consolidating matter was
introduced into the interstices of strata, masses of those bodies could
only be found consolidated with such substances as water is capable of
dissolving; and these substances would be found only in such a state as
the simple separation of the solvent water might produce.
In this case, the consolidation of strata would be extremely limited;
for we cannot allow more power to water than we find it has in nature;
nor are we to imagine to ourselves unlimited powers in bodies, on
purpose to explain those appearances by which we should be made to know
the powers of nature.


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