Matthew Fontaine Maury, Lieutenant, U.S.N.

Summary

Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

In that great inland basin of Asia which holds the Caspian Sea, and embraces an area of one million and a half of geo graphical square miles, we see the water-surface so exquisitely adjusted that it is just sufficient, and no more, to return to the atmosphere as vapor exactly as much moisture as the atmosphere lends in rain to the rivers of that basin.
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Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

In the Mediterranean, the evaporation is greater than the precipitation. Upon the Red Sea there never falls a drop of rain; it is all evaporation. Are we not, therefore, entitled to regard the Red Sea as a xnake-weight, thrown in to regulate the proportion of cloud and sunshine, and to dispense rain to certain parts of the earth in due season and in proper quantities? Have we not, in these two facts, evidence conclusive that the winds which blow over these two seas come, for the most part, from a dry country — from regions which contain few or no pools to furnish supplies of vapor?
Source: Wikisource

Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

But is it probable that, throughout all the geological periods, during all the changes which have taken place in the distribution of land and water surface over the earth, the winds, which in the general channels of circulation pass over the Dead Sea, have alone been unchanged? Throughout all ages, periods, and formations, is it probable that the winds have brought us just as much moisture to that sea as they now bring, and have just taken up as much water from it as they now carry off?
Source: Wikisource

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