water, according to _Stevinus_ and _Varenius_, and as I have
since found pretty true by making trial my self, is as 46. to 45. that is,
46. Ounces of the salt Water will take up no more room then 45. of the
fresh. Or reciprocally 45 pints of salt-water weigh as much as 46 of fresh.

But I found the proportion of Brine to fresh Water to be near 13 to 12:
Supposing therefore GHM to represent the Sea, and FI the height of the
Mountain above the Superficies of the Sea, FM a Cavern in the Earth,
beginning at the bottom of the Sea, and terminated at the top of the
Mountain, LM the Sand at the bottom, through which the Water is as it were
strained, so as that the fresher parts are only permitted to transude, and
the saline kept back; if therefore the proportion of G M to FM be as 45 to
46, then may the Cylinder of Salt-water GM make the Cylinder of Fresh-water
to rise as high as E, and to run over at N. I cannot here stand to examine
or confute their Opinion, who make the depth of the Sea, below its
Superficies, to be no more perpendicularly measured then the height of the
Mountains above it: 'Tis enough for me to say, there is no one of those
that have asserted it, have experimentally known the perpendicular of
either; nor shall I here determine, whether there may not be many other
causes of the separation of the fresh water from the salt, as perhaps some
parts of the Earth through which it is to pass, may contain a Salt, that
mixing and uniting with the Sea-salt, may precipitate it; much after the
same manner as the _Alkalizate_ and _Acid Salts_ mix and precipitate each
other in the preparation of _Tartarum Vitriolatum._ I know not also whether
the exceeding cold (that must necessarily be) at the bottom of the Water,
may not help towards this separation, for we find, that warm Water is able
to dissolve and contain more Salt, then the same cold; insomuch that Brines
strongly impregnated by heat, if let cool, do suffer much of their Salt to
subside and crystallize about the bottom and sides. I know not also whether
the exceeding pressure of the parts of the Water one against another, may
not keep the Salt from descending to the very bottom, as finding little or
no room to insert it self between those parts, protruded so violently
together, or else squeeze it upwads into the superiour parts of the Sea,
where it may more easily obtain room for it self, amongst the parts of the
Water, by reason that there is more heat and less press