Large sand waves in Navarinsky Canyon head, Bering Sea

Geo-Marine Letters
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Sand waves are present in the heads of large submarine canyons in the northwestern Bering Sea. They vary in height between 2 to 15 m and have wavelengths of 600 m. They are not only expressed on the seafloor, but are also well defined in the subsurface and resemble enormous climbing bed forms. We conjecture that the sand waves originated during lower stands of sea level in the Pleistocene. Although we cannot explain the mechanics of formation of the sand waves, internal-wave generated currents are among four types of current that could account for these large structures. ?? 1982 A. M. Dowden, Inc.
Publication type Article
Publication Subtype Journal Article
Title Large sand waves in Navarinsky Canyon head, Bering Sea
Series title Geo-Marine Letters
DOI 10.1007/BF02462757
Volume 2
Issue 3-4
Year Published 1982
Language English
Publisher Springer-Verlag
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Geo-Marine Letters
First page 157
Last page 162
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