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There is a general flow of the Black-Sea water through the Bosphorus, Marmara, and Dardanelles to the Mediterranean, probably caused by the combination of three things:—first, the prevalence of N. E. winds in the Black Sea; secondly, the excess of water received from the large rivers over the amount lost by temperature at some seasons; and, thirdly, the difference of specific gravities in the two seas. Of these, observation goes to prove that the wind has by far the greatest influence.

proceedings of the royal society of london

IX. Observations on the currents and undercurrents of the Dardanelles and Bosphorus, made by Commander J. L. Wharton, of H. M. Surveying-Ship 'Shearwater,' between the months of June and October, 1872. From a report of that officer to the hydrographer of the admiralty. Communicated by Admiralty