several years, a Salt comes to be formed, that is called Fossile; and this Opinion is the more likely to be true, because from the mixture of Acids with some Alkali matter we always draw a substance very like unto Salt. Now stones are an Alkali. I add, that the long fermentation, and concocti∣on which is made in the stone, serves to digest, and perfectly unite the Acid with the stony parts, for the making of Salt.
This Fossile salt, which is called Gemma, by rea∣son of its transparency, is found in many high Mountains of Europe, such as those in Poland, Catalonia, and Persia, and in the Indies; it is al∣together like that we use for nourishment, which is called Sea salt, insomuch that the Waters of the Sea may be said to receive their saltishness from nothing else but this Salt dissolved in them.
Is it not likely enough that the bottom of the Sea, or its shores, may be much like the surface of the Earth we inhabit, and that there may be Moun∣tains, Rocks, different sorts of earth, and conse∣quently inexhaustible Mountains of Salt in a Milli∣on of places at the bottom of the Sea, whence it receives its brackishness?
And it may be there are Waters, which after taking Salt from several earths, do at last discharge themselves into the Sea through an infinite number of subterranean channels, which do much contri∣bute likewise to making Sea-water salt.
That which confirms me in this opinion is, be∣cause there are Lakes in Italy, Germany, Egypt, the Indies, and many other places, which are as Salt as the Sea, and can have no other cause but that their waters have hapned to run through Mines of Salt.