The Irish Penny Journal, Vol. 1 No. 16, October 17, 1840Various
History
The Irish Penny Journal, Vol. 1 No. 16, October 17, 1840
Various
Ireland -- Periodicals
Although there are many places in the great Atlantic and Pacific Oceans
where the depth of water is very great, yet it has been deduced from
principles that are not liable to much error, that the general or average
depth does not exceed three miles. It may appear very strange that we
can assert any thing positive about the depth of water in those seas,
that are to the lines used for sounding quite unfathomable; but it is
effected very simply. Every person has seen a wave advancing along the
level surface of a canal, and by observing with a watch, it could easily
be found to move more quickly at some times than at others. The deeper
any part of the canal is, the more rapidly does the wave move along; and
partly by experiment, and partly by reasoning, the connection between the
depth of the water and velocity of the wave has been discovered. Now,
the tide which comes to Dublin every twelve hours is produced by the
influence of the sun and moon on the vast body of water in the Southern
Pacific Ocean; and the great wave there formed turns round Cape Horn,
and passes up the Atlantic Ocean, to arrive at the coasts of Europe and
North America. The time occupied by this great wave in passing from one
end to the other of the Atlantic can thus be known, and, precisely as in
a canal, the depth of water thus calculated.
The circumference of the earth at its widest part is about 25,000, and
its diameter 8000 miles. Hence the sheet of water which constitutes
the ocean forms but 3-4000ths of its thickness, or nearly the same
proportion as if we took an eighteen inch globe, and having spilled
water on its surface, allowed all the excess of water to drain off. The
remaining wetness would represent pretty nearly the condition of the
waters of the ocean on the surface of the earth. By this means we can
form, though obscurely, to our minds, an idea of the great magnitude of
the earth itself. This magnitude renders also very inconsiderable those
inequalities on the surface of the earth which constitute our highest
ridges of mountains. A true model of Mont Blanc, the highest of European
mountains, if constructed on the eighteen inch globe before referred to,
would be unfelt by a finger drawn along its surface, and it would be
only some of the highest peaks of the Andes and Himalayah that could be
distinctly felt. Where man also employs his most gigantic energies and
greatest efforts of skill to penetrate below the surface, forming mines
by which the supplies of coal, of iron, of copper, and other minerals,
have been obtained from the earliest times, the cavities that he makes
can only be compared with the trace given by the point of a pin that had
lightly touched the globe, and which would require a favourable incidence
of light to see.
Public-domain text, read in full here on John Shaqi.
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