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
Now, in the first place, the high degree of temperature which is
here understood, is probably not necessary to the purposes of
mineralization, as has just been shown; and, in the second place, it is
not FIRE, in the usual sense of the word, but HEAT, which is required
for that purpose; and there is nothing chimerical in supposing, that
nature has the means of producing heat, even in a very great degree,
without the assistance of fuel or of vital air. Friction is a source
of heat, unlimited, for what we know, in its extent, and so perhaps
are other operations, both chemical and mechanical; nor are either
combustible substances, or vital air, concerned in the heat thus
produced. So also the heat of the sun's rays in the focus of a burning
glass, the most intense that is known, is independent of the substances
just mentioned; and, though that heat certainly could not calcine a
metal, nor even burn a piece of wood, without oxygenous gas, it would
doubtless produce as high a temperature in the absence as in the
presence of that gas.
It is true, that it is not by the solar rays that subterraneous heat
is produced; but still, from this instance, we see, that there is no
incongruity in supposing the production of heat to be independent of
combustible bodies, and of vital air. We are indeed, in all cases,
strangers to the origin of heat; philosophers dispute, at this moment,
concerning the source of that which is produced by burning; and much
more are they at a loss to determine, what upholds the light and heat
of the great luminary, which animates all nature by its influence. If
we would form any opinion on this object, we shall do well to attend
to the suggestions of that great philosopher, who was hardly less from
others by his doubts and conjectures, than by his most rigorous and
profound investigations. "May not great, dense, and fixed bodies, when
heated beyond a certain degree, emit light so copiously, as, by the
emission and reaction of its light, and the reflections and refractions
of its rays within its pores, to grow still hotter, till it comes to
a certain period of heat, such as is that of the sun? And, are not
the sun and fixed stars great earths, vehemently hot, whose heat is
conserved by the greatness of the bodies, and the mutual action and
reaction between them and the light which they emit?"[76]
[Footnote 76: Newton's Optics, _ubi supra_.]
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