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Hutton, James, 1726-1797

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


If granite be truly stratified, and those strata connected with the
other strata of the earth, it can have no claim to originality; and
the idea of primitive mountains, of late so much employed by natural
philosophers, must vanish, in a more extensive view of the operations of
the globe; but it is certain that granite, or a species of the same kind
of stone, is thus found stratified. It is the _granit feuilletee_ of
M. de Saussure, and, if I mistake not, what is called _gneis_ by the
Germans. We have it also in our north alpine country of Scotland; of
this I have specimens, but have not seen it in its place.
Granite being thus found stratified, the masses of this stone cannot be
allowed to have any right of priority over the schistus, its companion
in the alpine countries, although M. de Saussure, whose authority I
would revere, has given it for the following reason; that it is found
the most centrical in the chains of high mountains, or in alpine
countries. Now, supposing this fact to be general, as he has found it in
the Alps, no argument for the priority of those masses can be founded
either upon the height or the situation of those granite mountains; for
the height of the mountain depends upon the solidity and strength of the
stone.


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