Whether this mysterious cataclysm occurred before or within the modern
epoch is a question which, as yet, has not by any means been determined.
The few organic remains detected in the deposit are of marine origin—one
or two species of shells—but all identical with species now existing.
The presumption is that the climate which prevailed over these northern
regions during the period was extremely low. But how long it lasted, and
why there are no types preserved, in all that congeries of materials
of the _terrestrial_ fauna and flora of the period, are points both of
them of a very perplexing kind. Whether just dawning upon the advent
of man, or within the actual era of his history, certain it is that
these are the results of a chaotic condition over a large portion of
our planet, of which, if we except the deluge, we have no record nor
memorials in any of the after changes and modifications of its surface.
Shall we add, as indicative of a FINAL CAUSE appearing in and overruling
the tumultuous agitation, that to this source is to be traced great
part of the soil which covers the valleys and mountain sides of all the
submerged districts? that hereby extensive lakes were silted up, the
flinty rock concealed by fertile earth, and the steep acclivity made
accessible to the husbandman? One thing is clear, that all the latest
tertiary strata in this alpine region have, after their consolidation,
been disturbed and broken up: it is upon their inverted edges that the
superficial accumulations have been deposited and now rest: and whether
the submergence of Europe, and other parts of the globe, was simultaneous
or not with the cause of their movement and overthrow, a superintending
wisdom and purpose are unquestionably discernible in those accessions of
soil and other economic arrangements that resulted from the change.
There is another theory, however, which has been applied to the
explanation of these phenomena—namely, the THEORY OF GLACIERS, as
illustrated in the works of Venetz, Charpentier, Agassiz, and Forbes.
Public-domain text, read in full here on John Shaqi.
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