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Knoll and Sediment Drift near Hudson Canyon

Allen Lowrie, Jr. and Bruce C. Heezen
Science
New Series, Vol. 157, No. 3796 (Sep. 29, 1967), pp. 1552-1553
Stable URL: http://www.jstor.org/stable/1722924
Page Count: 2
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Abstract

A parallel-bedded accumulation of sediments forms a low ridge on the upcurrent side of a partially moated knoll. These sediments were deposited beneath a southwestward-flowing current where it is locally decelerated by the obstructing knoll.

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