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Scientific American Supplement, No. 447, July 26, 1884 by Various
page 72 of 141 (51%)
they were for the most part of a loose, succulent texture, and that they
grew very rapidly indeed.

You will have noticed that there is one step more wanted to make good
this theory of the growth of coal on the spot where we now find it.
The coal is found, as already described, interbedded with shales and
sandstones. These shales and sandstones, as shown, were formed beneath
the water of the sea, and as long as they remained there of course no
plants could grow upon them. The question is, How was the land surface
formed for the growth of plants? It must have been formed in some way or
other by the sea bottom having been raised above the level of the water.
Now, we have distinct proof in many cases that elevation of the sea
bottom and depression of the land is now going on in many parts of the
earth's surface. And, therefore, we shall be assuming nothing beyond the
range of experience if we say that such elevations and depressions went
on during coal measure times. The coal measure times must have been
times during which the same spot was now below the sea, and now dry
land, over and over again. There was a land surface on which plants grew
fast and multiplied rapidly, and as they died fell and accumulated in
a great heap of dead vegetable matter. After a time this layer of
vegetable matter was slowly and gently let down beneath the waters of
the sea--so slowly that the water flowing over it did not, as a rule,
disturb the loose, pasty mass; and then, by the method I have described
to you, shales and sandstones were deposited on the top of this mass
of dead vegetable matter. By their weight they compressed it, and
by certain chemical changes (which we have not time to go into this
evening) this dense mass of vegetable matter became converted into coal.
After a time the shales and sandstones which had been piled above this
stuff, which was to form coal for the future, were again elevated to
form a land surface; upon this another forest sprang up, and by its
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