Modern Skepticism: A Course of Lectures Delivered at the Request of the Christian Evidence Society
Religion
Modern Skepticism: A Course of Lectures Delivered at the Request of the Christian Evidence Society
Church of England; Skepticism; Skepticism -- Controversial literature
The general evidence of geology is familiar probably to most of us,
and it is only the general evidence with which I can desire to deal on
such an occasion as this; but pray observe that while the particular
conclusions of geology, like those of other physical sciences, are
liable to continued modification and amendment, the general drift of
the conclusions is sufficiently clear and certain. No one can doubt,
for instance, the great antiquity of our globe, and the fact that it
has gone through successive changes with regard to the character of
its surface, the nature of its inhabitants, and the like. Undoubtedly
there was a time when civilized men did not dwell upon it; undoubtedly
there was a still more distant period when men did not dwell upon it
in any form, civilized or uncivilized; perhaps there was a period even
more distant, when life was not to be found upon the earth's surface at
all. And physical astronomy will take us even beyond geology, and will
make it probable that the earth was originally in a fluid condition,
in which from the excessive temperature no form of life could have
existed. Few problems are more curious than that which deduces the
present figure of our globe from the hypothesis of original fluidity.
Take a mass of fluid, and set it revolving slowly about an axis, as our
earth revolves, and it can be shown that it will assume such a form
as that which our earth has. I do not lay stress upon the remarkable
numerical coincidence of the ellipticity of the earth, as derived by
Laplace from theory, with that which is discovered by observation,
because this involves certain arbitrary hypotheses; but taking those
results which involve nothing arbitrary at all, it is almost impossible
not to believe that the earth was at one time a hot fluid mass, and
that it has gradually cooled down and hardened into its present
permanent condition.
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