Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
The other circumstance, on which the stability of our system depends,
is the small eccentricity of the planetary orbits, or their near
approach to circles. Were their orbits very eccentric, an opening
would be given to progressive change, that might so far increase, as
to prove the destruction of the whole. But neither the movement of all
the planets in the same direction, nor the small eccentricity of their
orbits, can be ascribed to accident, since that either of these should
happen by chance, in as many instances as there are planets, both
primary and secondary, is almost infinitely improbable. Again, that any
necessity in the nature of things should have either determined the
_direction_ of the planetary motions, or proportioned the _quantity_
of them to the intensity of the central force, cannot be admitted, as
these are things unavoidably conceived to be quite independent of one
another. It remains, therefore, that we consider the laws, which make
the disturbances in our system correct themselves, and by that means
give firmness and permanence to it, as a proof of the consummate wisdom
with which the whole is constructed.
387. The geological system of Dr Hutton, resembles, in many respects,
that which appears to preside over the heavenly motions. In both, we
perceive continual vicissitude and change, but confined within certain
limits, and never from a certain, mean condition, which is such, that,
in the lapse of time, the deviations from it on the one side, must
become just equal to the deviations from it on the other. In both, a
provision is made for duration of unlimited extent, and the lapse of
time has no effect to wear out or destroy a machine, constructed with
so much wisdom. Where the movements are all so perfect, their beginning
and end must be alike invisible.
NOTE XXI. § 122.
_Changes in the apparent
Level of the Sea._
388. In speaking of the natural epochs marked out by the phenomena
of the mineral kingdom, we have supposed a greater simplicity, and
separation of effects from one another, than probably takes place in
nature. We have, for instance, abstracted, in speaking of the waste
and degradation of the land, from that elevation which may have been
carried on at the same time. This appeared necessary to be done, in
order to simplify as much as possible the view that was to be given of
the whole; but there can be no doubt, that, while the land has been
gradually worn down by the operations on its surface, it has been
raised up by the expansive forces acting from below. There is even
reason to think, that the elevation has not been uniform, but has been
subject to a kind of oscillation, insomuch, that the continents have
both ascended and descended, or have had their level alternately raised
and depressed, independently of all action at the surface, and this
within a period comparatively of no great extent.
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