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Hutton, James, 1726-1797

"Theory of the Earth, Volume 1 (of 4)"


If coal, like other mineral strata, have been inspissated and
consolidated by subterranean heat, we should find them traversed with
veins and fissures; and, if the matter found in those veins and fissures
corresponds to that found in similar places of other strata, every
confirmation will be hence given to the theory that can be expected from
the consideration of those bituminous strata. But this is the case; we
find those fissures filled both with calcareous, gypseous, and pyritous
substances. Therefore, we have reason to conclude, that the strata of
fossil coal, like every other indurated or consolidated body in the
earth, has been produced, _first_, by means of water preparing and
collecting materials proper for the construction of land; and,
_secondly_, by the operation of internal fire or subterranean heat
melting and thus consolidating every known substance of the globe.
Not only are those sparry and pyritous substances, which are more
natural to coal strata, found forming veins traversing those strata in
various directions, but also every other mineral vein may occasionally
be found pervading coal mines, or traversing bituminous strata.


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