Abstract
Vast areas of the deep-sea floor are covered with distinctive bed forms that Have been produced by strong near-bottom current. Sediment drifts in the North Atlantic, and associated bedforms are discussed. (From paper)
| Original language | English |
|---|---|
| Pages (from-to) | 613 |
| Number of pages | 1 |
| Journal | OCEANUS |
| Volume | 21 |
| Issue number | 1 , 1978 |
| State | Published - 1978 |
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