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
114. Such, according to Dr Hutton's theory, are the changes which the
daily operations of waste have produced on the surface of the globe.
These operations, inconsiderable if taken separately, become great, by
conspiring all to the same end, never counteracting one another, but
proceeding, through a period of indefinite extent, continually in the
same direction. Thus every thing descends, nothing returns upward; the
hard and solid bodies every where dissolve, and the loose and soft no
where consolidate. The powers which tend to preserve, and those which
tend to change the condition of the earth's surface, are never _in
equilibrio_; the latter are, in all cases, the most powerful, and, in
respect of the former, are like living in comparison of dead forces.
Hence the law of decay is one which suffers no exception: The elements
of all bodies were once loose and unconnected, and to the same state
nature has appointed that they should all return.
115. It affords no presumption against the reality of this progress,
that, in respect of man, it is too slow to be immediately perceived:
The utmost portion of it to which our experience can extend, is
evanescent, in comparison with the whole, and must be regarded as the
momentary increment of a vast progression, circumscribed by no other
limits than the duration of the world. TIME performs the office of
integrating the infinitesimal parts of which this progression is made
up; it collects them into one sum, and produces from them an amount
greater than any that can be assigned.
116. While on the surface of the earth so much is every where going to
decay, no new production of mineral substances is found in any region
accessible to man. The instances of what are called petrifactions, or
the formation of stony substances by means of water, which we sometimes
observe, whether they be ferruginous concretions, or calcareous, or,
as happens in some rare cases, siliceous stalactites, are too few
in number, and too inconsiderable in extent, to be deemed material
exceptions to this general rule. The bodies thus generated, also, are
no sooner formed, than they become subject to waste and dissolution,
like all the other hard substances in nature; so that they but retard
for a while the progress by which they are all resolved into dust, and
sooner or later committed to the bosom of the deep.
Public-domain text, read in full here on John Shaqi.
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