Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
It must not be alleged, that the heights of the Oural mountains, or the
hardness of their rocks, make an essential distinction between them
and the argillaceous or arenaceous strata of the plains; solidity and
hardness, as well as changes in their height and natural position, has
been superinduced in operations posterior to the collection of those
masses,--operations which may be formed in various degrees, even in the
different parts of the same mass. If this is the case, there can be no
difficulty in conceiving a stratum, which appears to be argillaceous
or marly in the plains, to be found jasper in the Oural mountains. But
there is nothing in the Oural mountains, that may not be found some
where or other in the plains, although the soft and easily decomposing
argillaceous strata be not found upon the Oural mountains, or the Alps,
for this reason, that had those mountains been formed of such materials,
there had not been a mountain there at this day.
But surely the greatest possible error, with regard to the philosophy of
this earth, would be to confound the sediment of a river with the strata
of the globe; bodies deposited upon the surface of the earth, with those
sunk at the bottom of the sea; and things which only form the travelled
or transported soil, with those which constitute the substratum or the
solid earth. How far M. Pallas has committed this oversight, I leave
others to determine. After mentioning those strata in which wood is
found petrified, and metallic minerals formed, he thus proceeds, (page
69).
"Dans ces mêmes dépôts sableux et souvent limoneux, gisent les restes
des grands animaux de l'Inde: ces ossemens d'éléphans, de rhinocéros, de
buffles monstrueux, dont on déterre tous les jours un si grand nombre,
et qui font l'admiration des curieux. En Sibérie, où l'on à découvert le
long de presque toutes les rivières ces restes d'animaux étrangers,
et l'ivoire même bien conservé en si grande abondance, qu'il forme un
article de commerce, en Sibérie, dis je, c'est aussi la couche la plus
moderne de limon sablonneux qui leur sert de sépulture, et nulle part
ces monumens étrangers sont si frequens, qu'aux endroits où la grande
chaine, qui domine surtout la frontière méridionale de la Sibérie, offre
quelque dépression, quelque ouverture considérable.
Public-domain text, read in full here on John Shaqi.
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