The Chautauquan, Vol. 04, March 1884, No. 6Chautauqua Literary and Scientific Circle
History
The Chautauquan, Vol. 04, March 1884, No. 6
Chautauqua Literary and Scientific Circle
Chautauqua Institution -- Periodicals; Chautauqua Literary and Scientific Circle -- Periodicals
So we find in this large aquarium, the great sea, the same processes
going on—the same material manufactured that took place in what is termed
the older geological formation. Can we say that creation is complete?
That the earth is finished, and, like a ship we read about the other day,
to be disposed of for the old iron it contains? Not long since I visited
a marble quarry, from which very curious and beautiful marble, resembling
the onyx, was being taken. There were thick strata cropping out; and the
air, and rain, and frost had disintegrated the exposed parts, so they
looked as old as the earth. But just beneath, and in various places, were
little springs of warm water, and as these bubbled out of the earth they
deposited on cooling and exposure to the air, the same kind of marble—and
there I saw going on the process of marble making that had continued
doubtless for thousands of years.
On the shores, in the tide, pools and lagoons of Monterey bay we often
gather little plants classed with the _Algæ_, or sea-moss, which we call
diatoms. They are exceedingly small—some of them—so that we have to
magnify them with the microscope several hundred diameters, in order to
see how they are formed. Some kinds grow on the larger sea weeds, some
on the rocks, and some appear to be free in the water, coming ashore in
large quantities with the foam of the surf, and giving a greenish brown
color to the sand of the shore. These diatoms are composed mainly of
silex—flint. If we examine the rocks of our highest ridges and mountains
and the cliffs of our shores in places, with the microscope, we shall
find them largely composed of fragments of diatoms and spiculæ of
sponges. And these are chiefly of the same species that we find alive
to-day. Thus while the “chalk rocks” on our shores, the sand stones and
harder rocks are melting away under the pounding waves of the sea, and
being carried to the lower bottoms, fresh supplies of diatoms and sponges
are mixed therewith, and we have a continuation, under our eyes, of what
was begun thousands of years ago.
Public-domain text, read in full here on John Shaqi.
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