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Hutton, James, 1726-1797

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

Let us now reason from those
facts, without either constraining nature, which we know, or forming
visionary systems, with regard to things which are unknown. It would
appear, that at one period of time, or in one place, the matter of the
globe may be deposited, in strata, without containing any organised
bodies; at another time, or in another place, much animal matter may be
deposited in strata, without any vegetable substance there appearing;
but at another period, or at another time, strata may be formed with
much vegetable matter, while there is hardly to be observed any animal
body. What then are we to conclude upon the whole? That nature, forming
strata, is subject to vicissitudes; and that it is not always the same
regular operation with respect to the materials, although always forming
strata upon the same principles. Consequently, upon the same spot in
the sea, different materials may be accumulated at different periods of
time, and, conversely, the same or similar materials may be collected in
different places at the same time. Nothing more follows strictly from
the facts on which we now are reasoning; and this is a conclusion which
will be verified by every appearance, so far as I know.


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