The Ocean World: Being a Description of the Sea and Its Living Inhabitants.Figuier, Louis
Science
The Ocean World: Being a Description of the Sea and Its Living Inhabitants.
Figuier, Louis
Marine animals; Ocean
It had long been admitted, on the faith of inexact observation, that the
level of the Red Sea was higher than that of the Mediterranean. It has
also been said that the level of the Pacific Ocean at Panama is higher
by about forty inches than the mean level of the Atlantic at Chagres,
and that, at the moment of high water, this difference is increased to
about thirteen feet, while at low it is over six feet in the opposite
direction. This has been proved, so far as the evidence goes, to be
error in what concerns the difference in level of the Red Sea and
Mediterranean; and the opening of the Suez Canal, which is near at hand,
will probably furnish still more convincing proofs. Recent soundings
show that the mean level of the Pacific and Atlantic Oceans are
identical.
* * * * *
It has been calculated that all the waters of the several seas gathered
together would form a sphere of fifty or sixty leagues in diameter, and,
supposing the surface of the globe perfectly level, that these waters
would submerge it to the depth of more than six hundred feet. Again,
admitting the mean depth of the sea to be thirteen thousand feet, its
estimated contents ought to be nearly two thousand two hundred and fifty
millions of cubic miles of water; and, if the sea could be imagined to
be dried up, all the sewers of the earth would require to pour their
waters into it for forty thousand years, in order to fill the vast
basins anew.
* * * * *
If we could imagine the entire globe to be divided into one thousand
seven hundred and eighty-six parts by weight, we should find
approximately, according to Sir John Herschel, that the total weight of
the oceanic waters is equivalent to one of these parts.
The specific weight of sea water is a little above that of fresh water,
the proportion being as a thousand to a thousand and twenty-seven. The
Dead Sea, which receives no fresh water into its bosom to maintain
itself at the same level as other seas, acquires a higher degree of
saltness, and is equal to a thousand and twenty-eight. The specific
gravity of sea water is about the same as the milk of a healthy woman.
* * * * *
Public-domain text, read in full here on John Shaqi.
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