The Voice of Science in Nineteenth-Century Literature: Representative Prose and Verse
Science
The Voice of Science in Nineteenth-Century Literature: Representative Prose and Verse
English literature -- 19th century; Literature, Modern; Science; Science in literature
It is so needful to form clear and distinct notions of what is really
meant by each of these hypotheses, that I will ask you to imagine what,
according to each, would have been visible to a spectator of the events
which constitute the history of the earth. On the first hypothesis,
however far back in time that spectator might be placed, he would see a
world essentially, though perhaps not in all its details, similar to that
which now exists. The animals which existed would be the ancestors of
those which now live, and similar to them; the plants, in like manner,
would be such as we know; and the mountains, plains, and waters would
foreshadow the salient features of our present land and water. This view
was held more or less distinctly, sometimes combined with the notion of
recurrent cycles of change, in ancient times; and its influence has been
felt down to the present day.
It is worthy of remark that it is a hypothesis which is not inconsistent
with the doctrine of Uniformitarianism, with which geologists are
familiar. That doctrine was held by Hutton, and in his earlier days by
Lyell. Hutton was struck by the demonstration of astronomers that the
perturbations of the planetary bodies, however great they may be, yet
sooner or later right themselves; and that the solar system possesses a
self-adjusting power by which these aberrations are all brought back to a
mean condition. Hutton imagined that the like might be true of terrestrial
changes; although no one recognized more clearly than he the fact that the
dry land is being constantly washed down by rain and rivers, and deposited
in the sea; and that thus, in a longer or shorter time, the inequalities
of the earth's surface must be leveled, and its high lands brought down to
the ocean. But, taking into account the internal forces of the earth,
which, upheaving the sea-bottom, give rise to new land, he thought that
these operations of degradation and elevation might compensate each other;
and that thus, for any assignable time, the general features of our
planet might remain what they are. And inasmuch as, under these
circumstances, there need be no limit to the propagation of animals and
plants, it is clear that the consistent working-out of the uniformitarian
idea might lead to the conception of the eternity of the world. Not that I
mean to say that either Hutton or Lyell held this conception--assuredly
not; they would have been the first to repudiate it. Nevertheless, the
logical development of their arguments tends directly toward this
hypothesis.
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