Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
Generelli then describes the continual waste of mountains and
continents, by the action of rivers and torrents, and concludes with
these eloquent and original observations:--"Is it possible that this
waste should have continued for six thousand, and _perhaps_ a greater
number of years, and that the mountains should remain so great, unless
their ruins have been repaired? Is it credible that the Author of Nature
should have founded the world upon such laws, as that the dry land
should forever be growing smaller, and at last become wholly submerged
beneath the waters? Is it credible that, amid so many created things,
the mountains alone should daily diminish in number and bulk, without
there being any repair of their losses? This would be contrary to that
order of Providence which is seen to reign in all other things in the
universe. Wherefore I deem it just to conclude, that the same cause
which, in the beginning of time, raised mountains from the abyss, has
down to the present day continued to produce others, in order to restore
from time to time the losses of all such as sink down in different
places, or are rent asunder, or in other way suffer disintegration. If
this be admitted, we can easily understand why there should now be found
upon many mountains so great a number of crustacea and other marine
animals."
In the above extract, I have not merely enumerated the opinions and
facts which are confirmed by recent observation, suppressing all that
has since proved to be erroneous, but have given a faithful abridgment
of the entire treatise, with the omission only of Moro's hypothesis,
which Generelli adopted, with all its faults and excellences. The reader
will therefore remark, that although this admirable essay embraces so
large a portion of the principal objects of geological research, it
makes no allusion to the extinction of certain classes of animals; and
it is evident that no opinions on this head had, at that time, gained a
firm footing in Italy. That Lister and other English naturalists should
long before have declared in favor of the loss of species, while Scilla
and most of his countrymen hesitated, was perhaps natural, since the
Italian museums were filled with fossil shells belonging to species of
which a great portion did actually exist in the Mediterranean; whereas
the English collectors could obtain no recent species from such of their
own strata as were then explored.
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