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
457. The time indeed was, and we are not yet far removed from it,
when one of the most important principles involved in Dr Hutton's
theory was not only unknown, but could not be discovered. This was
before the causticity produced in limestone by exposure to fire was
understood, and when it was not known that it arose from the expulsion
of a certain aerial fluid, which before was a component part of the
stone. It could not then be perceived, that this aerial part might be
retained by pressure, even in spite of the action of fire, and that in
a region where great compression existed, the absence of causticity was
no proof that great heat had not been applied. The discoveries of Dr
BLACK, therefore, mark an era, before which men were not qualified to
judge of the nature of the powers that had acted in the consolidation
of mineral substances. Those discoveries were, indeed, destined to
produce a memorable change in chemistry, and in all the branches of
knowledge allied to it; and have been the foundation of that brilliant
progress, by which a collection of practical rules, and of insulated
facts, has in a few years risen to the rank of a very perfect science.
But even before they had explained the nature of carbonic gas, and its
affinity to calcareous earth, I am not sure but that Dr Hutton's theory
was, at least, partly formed, though it must certainly have remained,
even in his own opinion, exposed to great difficulties. His active and
penetrating genius soon perceived, in the experiments of his friend,
the solution of those difficulties, and formed that happy combination
of principles, which has enabled him to explain the most enigmatical
appearances in the natural history of the earth.
As we are not yet far removed from the time when our chemical knowledge
was too imperfect to admit of a satisfactory explanation of the
phenomena of mineralogy, so it is not unlikely that we are approaching
to other discoveries that are to throw new light on this science. It
would, however, be to argue strangely to say, that we must wait till
those discoveries are made before we begin any theoretical reasonings.
If this rule were followed, we should not know where the imperfections
of our science lay, nor when the remedies were found out, should we
be in a condition to avail ourselves of them. Such conduct would not
be caution, but timidity, and an excess of prudence fatal to all
philosophical inquiry.
Public-domain text, read in full here on John Shaqi.
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