Theory of the Earth, With Proofs and Illustrations, Volume 2 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 2 (of 4)
Hutton, James
Geology -- Early works to 1800
It is singularly fortunate that such remarkable appearances, as are
found in the rocks of this place, had called the attention of M. de
Saussure to investigate a subject so interesting to the present theory;
and it is upon this, as well as on many other occasions, that the value
of those observations of natural history will appear. They are made by a
person eminent for knowledge; and they are recorded with an accuracy and
precision which leaves nothing more to be desired.
From _Martigny_ to _St. Maurice_, about three leagues, there is a most
interesting valley of the Rhône, through which this river makes its way
from the _Vallais_, or great valley above, among those mountains which
seem to have shut up the _Vallais_, and through which the river must
pass in running to the lake. M. de Saussure found some singular masses,
which attracted his attention, in examining the structure of the rocks
on the left side of this little valley. Like a true philosopher, and
accurate naturalist, he desired to compare what was to be observed
in the other side of this valley of the Rhône, which he had found so
singular and so interesting on that which he had examined. Accordingly,
in Spring 1785, he made a journey for that purpose. In this survey he
found the most perfect correspondence between the two sides of this
valley, so far as rocks of the same individual species, and precisely in
the same order, are found upon the one side and upon the other.
This author, after describing those particular appearances, sums up
the evidence which arises from this comparison of the two sides of the
valley; and he here gives an example of just reasoning, of accuracy, and
impartiality, which, independent of the subject, cannot be read without
pleasure and approbation. But when it is considered, that here is a
matter of the highest importance to the present theory, or to any other
system of geology, no less than a demonstration that the rocks, of which
the mountains on both sides of the valley of the Rhône are formed, are
the same, and must have been originally continued in one mass, the
following observations of our author will be most acceptable to every
person who inclines to read upon this subject.
«§ 1079. On voit par cet exposé, que bien que la vallée du Rlione ait
dans ce trajet près d'une lieue de largeur moyenne, les montagnes qui
la bordent sont en general du même genre, et dans la même situation sur
l'une et l'autre rive.
«Il y a cependant trois différences que je dois exposer et apprécier en
peu de mots.
Public-domain text, read in full here on John Shaqi.
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