e masses?--Such a conclusion could only be formed in
making a supposition, that every organised body deposited in a mass
of matter, whether homogeneous or heterogeneous, should be preserved
without change, while the collected mass, in which it had been
deposited, changes as much as possible by the operation both of fire and
water. But this supposition is erroneous, and cannot be admitted; and
the study of marbles will demonstrate this truth, that the calcareous
relics of organised bodies are changed, in the consolidating operations
of the globe, in every degree, from the smallest alteration to the
greatest, when they become indistinguishable any farther to our sight.
Therefore, from the supposition of no appearance of marine bodies in the
pretended primitive masses, there is no sufficient evidence or reason to
conclude, that those masses have not had a marine origin; because, the
traces of organised bodies may be obliterated by the many subsequent
operations of the mineral region; and which operations, the present
state of those masses certify beyond dispute.
We are now to examine the fact, how far the ground on which that false
reasoning had been founded is strictly true.
In the first place, then, it must be considered, that the alledged fact
is nothing but a negative assertion, importing that no mark of organised
bodies had been observed, in certain stones and strata which some
naturalists have examined with that view. But, though many naturalists
have looked for them without success, it does not follow that such marks
may not be found; it indeed proves that such a task is difficult, and
the success of it, to a particular, most precarious; accident, however,
may bring about what the greatest industry has not been able to attain.
Secondly, there is good reason to believe that this asserted negation
is not absolutely true; for I have in my possession what I consider as
proof of the contrary; I found it in Wales, and I think it is in what
may be considered as primitive mountains;--it is the mark of shells in a
stone of that kind.
Thus, I had formed my opinion with regard to this alleged fact, long
before I had seen any description either of the Alps or Pyrennean
mountains; and now I have no reason to change that opinion. It may
indeed be alleged, that the strata of marble or limestone, containing
marine bodies found in those mountains, are secondary strata, and not
the primitive. To this I can give no reply, as th
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