Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
It is very singular to dig so deep without meeting with water: and this
circumstance is remarkable in many particulars. 1. It shews, that the
water of the sea does not communicate with the interior part of the
earth, by means of filtration. 2. That shells are found at the depth of
100 feet below the surface, and that consequently the soil of Holland
has been raised 100 feet by the sediment of the sea. 3. We may draw an
induction, that this strata of thick clay of 102 feet, and the bed of
sand below it, in which they dug to 31 feet, and whose entire thickness
is unknown, are perhaps not very far distant from the first strata of
the original earth, such as it was before the motion of the water had
changed its surface. We have said in the first article, that if we
desired to find the ancient earth, we should dig in the northern
countries, rather than towards the south; in plains rather than in
mountainous regions. The circumstances in this instance, appear to be
nearly so, only it is to be wished they had continued the digging to a
greater depth, and that the author had informed us, whether there were
not shells and other marine productions, in the last bed of clay, and in
that of sand below it. The experiment confirms what we have already
said; and the more we dig, the greater thickness we shall find the
strata.
The earth is composed of parallel and horizontal beds, not only in
plains, but hills and mountains are in general composed after the same
manner: it may be said, that the strata in hills and mountains are more
apparent there than in the plains, because the plains are generally
covered with a very considerable quantity of sand and earth, which the
water has brought from the higher grounds, and therefore, to find the
ancient strata, must dig deeper in the plains than in the mountains.
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