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
88. But, if the intensity of volcanic heat be such as is here
stated, it will be found very difficult to account for a fire of
such activity, and of such long continuance in the same spot, by any
decomposition of mineral substances near the surface. In the place
where this combustion is supposed to exist, it must be remembered,
that there is no fresh supply of materials to replace those that have
been consumed, and that, therefore, the original accumulation of these
materials in one spot, must have been very unlike any thing that has
ever been observed concerning the disposition of minerals in the bowels
of the earth.
89. If, on the other hand, we ascribe the phenomena of volcanoes to
the central heat, the account that may be given of them is simple, and
consistent with itself. According to all the appearances from which the
existence of such heat has been inferred above, it is of a nature so
far different from ordinary fire, that it may require no circulation
of air, and no supply of combustible materials to support it. It is
not accompanied with inflammation or combustion, the great pressure
preventing any separation of parts in the substances on which it acts,
and the absence of that elastic fluid without which heat seems to have
no power to decompose bodies, even the most combustible, contributing
to the unalterable nature of all the substances in the mineral regions.
There, of consequence, the only effects of heat are fusion and
expansion; and that which forms the nucleus of the globe may therefore
be a fluid mass, melted, but unchanged by the action of heat.
Public-domain text, read in full here on John Shaqi.
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