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
As to the first, it is acknowledged, that there is a certain regular
disposition of the substances in mineral veins, as stated § 59, but it
is one which has hardly any thing in common with the real phenomena
of stratification. It consists in the distribution of the principal
substances in coats parallel to the sides of the vein, each substance
forming a separate coat. In a vein, for instance, containing quartz,
fluor, calcareous spar, lead, &c. we might expect to find a lining of
quartz crystals, applied immediately to the walls of the mine, and
following exactly the irregularities of their surface; next, perhaps,
a coat of fluor, then of calcareous spar, and last of lead ore in the
centre of the vein, the same order being observed on the opposite
side. These successive coats, it is material to remark, are not in
planes, but in uneven surfaces, of which the inequalities are evidently
determined by those of the walls, that is, of the rock which forms
the sides of the vein; neither are they horizontal, but are parallel
to the walls, whether these be perpendicular or inclined. Here,
therefore, there is no appearance of the action of that statical law
which has directed the arrangement of the other strata, and which tends
to make the plane of every stratum deposited by water perpendicular
to the direction of gravity. The coating of the veins has therefore
been performed under the conduct of some other power than that which
presides over aqueous deposition. If, as the Neptunists maintain, the
materials in the veins were deposited by water, in the most perfect
tranquillity, it is wonderful that we do not find those materials
disposed in horizontal layers, across the vein, instead of being
parallel to its sides; and it seems very unaccountable, that the common
strata, deposited as we are told while the water was in a state of
great agitation, have so rigorously obeyed the laws of hydrostatics, (§
38.) and acquired a parallelism in the planes of their stratification,
which approaches so often to geometrical precision; while the materials
of the veins, in circumstances so much more favourable for doing the
same, have done nearly the reverse, and taken a position, often at
right angles to that which hydrostatical principles require. This is a
paradox which the Neptunian system has created, and which therefore it
is not very likely to resolve.
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