Titlebook: Marine Geology and Oceanography of the Arctic Seas; Yvonne Herman Conference proceedings 1974 Springer-Verlag New York Inc. 1974 Arctic.Ar

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Geological Oceanography of the Bering Shelf,f is extremely smooth, with a gentle uniform gradient. The climate is dominated by extratropical cyclonic and arctic anticyclonic storms which tend to be brief but violent. During winter most of the Bering Sea shelf is covered by ice..The Bering Sea exchanges waters with both the Pacific and the Arc

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Sedimentation in the Beaufort Sea: A Synthesis,itial waters of the Beaufort Sea are presented..Generally, bottom sediments are extremely poorly sorted muds or sandy muds. Gravels are frequently encountered on the shelf, sporadically on the upper slope, and never on the lower slope and abyssal basin. Invariably size distribution curves of shelf s

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Holocene History of the Laptev Sea Continental Shelf,sent sea level. The five large submarine valleys traversing the shelf do not continuously grade seaward, but contain elongated, closed basins. These terraces and closed basins plus deltaic sediments associated with the submarine valleys quite possibly mark sea level Stillstands, and enable reconstru

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Sediment Distribution in Deep Areas of the Northern Kara Sea,h to the west is the larger (140,000 square kilometers at the 200-m isobath) and deeper (exceeding 640 m) of the two troughs with a general U-shape. The Central Kara Plateau, a shallow area which contains two islands and several shoal areas, separates the St. Arm Trough from the Voronin Trough (20,0

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