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
422. Some of the same observations apply to Mr Kirwan. His Geological
Essays have also for their object to explain the first origin of
things; and to say that he has not succeeded, in an attempt where no
man ever can succeed, implies no reproach on the execution of his
work, whatever it may do on the design. We have indeed no criterion by
which the execution of it can be estimated: what would in any other
place be a blemish, may be here deserving of praise; and if the work
is full of confusion and perplexity, these are qualities inherent in
the subject which it is intended to describe. It were, no doubt, to
be wished, that after emerging into the regions of day, Mr Kirwan had
been as successful in copying the beauty and simplicity of nature, as
in representing the disorder and inconsistency of the chaotic mass.
But his cosmology is without unity in its principles, or consistency
in its parts; the causes introduced, are, for the most part, such as
will account for one set of appearances just as well as for another;
or, if any of them is likely to prove inadequate to the effect ascribed
to it, a new and arbitrary hypothesis is always ready to come to its
assistance. The information given is seldom exact: a multitude of facts
brought together, without the order and discussion essential to precise
knowledge; and an infinity of quotations, amassed without criticism or
comparison, afford proofs of extensive reading, but of the most hasty
and superficial inquiry. Thus we have seen passages from ULLOA and
FRISI, produced in support of opinions, which, when fairly stated, they
had the most direct tendency to overthrow.
423. In one respect, the geological writings of Kirwan are far inferior
to De Luc's: They are evidently the productions of a man who has not
seen nature with his own eyes; who has studied mineralogy in cabinets,
or in books only; but who has seldom beheld fossils in their native
place. With the balance in his hand, and the external characters of
WERNER in his view, he has examined minerals with diligence, and has
discovered many of those marks which serve to ascertain their places,
in a system of artificial arrangement. But to _reason_ and to _arrange_
are very different occupations of the mind; and a man may deserve
praise as a mineralogist, who is but ill qualified for the researches
of geology.
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