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Hutton, James, 1726-1797

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


This, therefore, is the object which we are to have in view during this
physical investigation; this is the end to which are to be directed all
the steps in our cosmological pursuit.
The solid parts of the globe are, in general, composed of sand, of
gravel, of argillaceous and calcareous strata, or of the various
compositions of these with some other substances, which it is not
necessary now to mention. Sand is separated and sized by streams and
currents; gravel is formed by the mutual attrition of stones agitated
in water; and marly, or argillaceous strata, have been collected, by
subsiding in water with which those earthy substances had been floated.
Thus, so far as the earth is formed of these materials, that solid body
would appear to have been the production of water, winds, and tides.
But that which renders the original of our land clear and evident,
is the immense quantities of calcareous bodies which had belonged
to animals, and the intimate connection of these masses of animal
production with the other strata of the land. For it is to be proved,
that all these calcareous bodies, from the collection of which the
strata were formed, have belonged to the sea, and were produced in it.


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