Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
Let us resume in a few words. There is not perhaps one substance in the
mineral kingdom by which the operation of subterraneous heat is, to
common understanding, better exemplified than that of mineral coal.
Those strata are evidently a deposit of inflammable substances which all
come originally from vegetable bodies. In this state of their formation,
those coal strata must all be oleagenous or bituminous. In many of them,
however, these volatile parts are found wanting; and, the stratum is
found in the state of the most perfect coal or caput mortuum. There, is,
I presume, no other means to be found by which this eminent effect could
be produced, except by distillation; and, this distillation perhaps
proceeded under the restraining force of an immense compression.
To this theory it must not be objected, that all the strata of coal,
which are found in the same place or neighbourhood, are not reduced to
that caput mortuum or perfect coaly state. The change from a bituminous
to a coaly substance can only take place in proportion as the
distillation of the volatile parts is permitted. Now this distillation
must be permitted, if any passage can be procured from the inflammable
body submitted to the operation of subterraneous heat; and, one stratum
of coal may find vent for the passage of those vapours, through some
crevice which is not open to another. In this way, doubtless, some of
those bodies have been inspissated or reduced to a fixed coal, while
others, at a little distance, have retained most of their volatile
parts.
We cannot doubt of this distilling operation in the mineral regions,
when we consider that in most places of the earth we find the evident
effects of such distillation of oily substances in the naphta and
petroleum that are constantly emitted along with water in certain
springs. These oily substances are no other than such as may be
procured, in a similar manner, from the fusible or inflammable coal
strata; we have therefore every proof of this mineral operation that the
nature of things admit of. We have also sufficient evidence that those
fusible and inflammable coals, which have not been distilled to a caput
mortuum, had been subjected to the operation of subterraneous heat,
because we find those fusible coals subject to be injected with pyrites,
as well as the more perfect coal.
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