and upon the cliffs, leaving great crevices through the saline deposits, as chances to have been the case with the salt formations through which I passed with my guide, and have recently described to you."
"Even now I have my doubts as to the correctness of your explanations, especially concerning the liquid surfaces."
"They are facts, however; liquids capable of being mixed, if connected by porous arches (bibulous paper is convenient for illustrating by experiment) reverse the rule men have accepted to explain the phenomena of liquid equilibrium, for I repeat, the lighter one rushes into that which is heavier, and the surface of the heavier liquid rises. You can try the experiment with alcohol and water, taking precautions to prevent evaporation, or you can vary the experiment with solutions of various salts of different densities; the greater the difference in gravity between the two liquids, the more rapid will be the flow of the lighter one into the heavier, and after equilibrium, the greater will be the contrast in the final height of the resultant liquid surfaces."
"Men will yet explain this effect by natural laws," I said.
"Yes," he answered; "when they learn the facts; and they will then be able to solve certain phenomena connected with diffusion processes that they can not now understand. Did I not tell you that after the fact had been made plain it was easy to see how Columbus stood the egg on its end? What I have demonstrated by experiment is perhaps no new principle in hydrostatics. But I have applied it in a natural manner to the explanation of obscure natural phenomena, that men now seek unreasonable methods to explain."
"You may proceed with your narrative. I accept that when certain liquids are connected, as you have shown, by means of porous substances, one will pass into the other, and the surface of the lighter liquid in this case will assume a position below that of the heavier."
"You must also accept," said he, "that when solutions of salt are subjected to earth attraction, under proper conditions, the solids may by capillary attraction be left behind, and pure water finally pass through the porous medium. Were it not for this law, the only natural surface spring water on earth would be brine, for the superficial crust of the earth is filled with saline
