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Hutton, James, 1726-1797

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

It is a truth unquestionable,
that what had been originally at the bottom of the sea, is at present
the highest of our land. In explaining this appearance, therefore, no
other alternative is left, but either to suppose strata elevated by the
power of heat above the level of the present sea, or the surface of the
ocean reduced many miles below the height at which it had subsisted
during the collection and induration of the land which we inhabit.
Now, if, on the one hand, we are to suppose no general power of
subterraneous fire or heat, we leave to our theory no means for the
retreat of the sea, or the lowering of its surface; if, on the other
hand, we are to allow the general power of subterraneous heat, we cannot
have much difficulty in supposing, either the surface of the sea to have
subsided, or the bottom of the ocean, in certain parts, to have been
raised by a subterranean power above the level of its surface, according
as appearances shall be found to require the one or other of those
conclusions. Here, therefore, we are again remitted to the history of
nature, in order to find matter of fact by which this question may be
properly decided.


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