. Biology of the seas of the Marine biology -- Soviet Union; Hydrology -- Soviet Union. THE BARENTS SEA 77 of the Sea lying adjacent to the great depths of the Greenland Sea and the Arctic basin. N. Zubov (1932) has calculated the distribution of depths in the Barents Sea in percentages as given in Table Fig. 22. Chart of Barents Sea, showing depths (Zubov) and currents (Zaytsev). 1 100 m; 2 100 to 200 m; 3 200 to 300 m; 4 300 to 400 m; 5 400 to 500 m; 6 >500 m; 7 Main directions of currents. In the opinion of F. Nansen (1922) the floor of the Barents Sea is an ela- borate sys
. Biology of the seas of the Marine biology -- Soviet Union; Hydrology -- Soviet Union. THE BARENTS SEA 77 of the Sea lying adjacent to the great depths of the Greenland Sea and the Arctic basin. N. Zubov (1932) has calculated the distribution of depths in the Barents Sea in percentages as given in Table Fig. 22. Chart of Barents Sea, showing depths (Zubov) and currents (Zaytsev). 1 100 m; 2 100 to 200 m; 3 200 to 300 m; 4 300 to 400 m; 5 400 to 500 m; 6 >500 m; 7 Main directions of currents. In the opinion of F. Nansen (1922) the floor of the Barents Sea is an ela- borate system of river valleys sunk under the sea surface. In fact if the sea- level were lowered 500 m the whole of the Barents Sea would become dry land. Bottom topography The bottom topography of the Barents Sea has the following features (Fig. 22). In three places troughs below 400 m enter the sea, the first lying between the. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Zenkevich, L. A. (Lev Aleksandrovich), 1889-1970. New York, Interscience Publishers
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