Classics of modern science : $b (Copernicus to Pasteur)
History
Classics of modern science : $b (Copernicus to Pasteur)
Science; Science -- History
In the first place, the chances are nearly as three to one against
the mere emergence of the mass above the waters, because nearly
three-fourths of the globe are covered by the ocean. But if it be
upheaved and made to constitute part of the dry land, it must also,
before it can be available for our instruction, become part of that
area already surveyed by geologists. In this small fraction of land
already explored, and still very imperfectly known, we are required to
find a set of strata deposited under peculiar conditions, and which,
having been originally of limited extent, would have been probably much
lessened by subsequent denudation.
Yet it is precisely because we do not encounter at every step the
evidence of such gradations from one state of the organic world to
another, that so many geologists have embraced the doctrine of great
and sudden revolutions in the history of the animate world. Not content
with simply availing themselves, for the convenience of classification,
of those gaps and chasms which here and there interrupt the continuity
of the chronological series, as at present known, they deduce, from the
frequency of these breaks in the chain of records, an irregular mode of
succession in the events themselves, both in the organic and inorganic
world. But, besides that some links of the chain which once existed are
now entirely lost and others concealed from view, we have good reason
to suspect that it was never complete originally. It may undoubtedly be
said that strata have been always forming somewhere, and therefore at
every moment of past time Nature has added a page to her archives; but,
in reference to this subject, it should be remembered that we can never
hope to compile a consecutive history by gathering together monuments
which were originally detached and scattered over the globe. For, as
the species of organic beings contemporaneously inhabiting remote
regions are distinct, the fossils of the first of several periods which
may be preserved in any one country, as in America for example, will
have no connection with those of a second period found in India, and
will therefore no more enable us to trace the signs of a gradual change
in the living creation, than a fragment of Chinese history will fill up
a blank in the political annals of Europe.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account