Answers are grounded in this paper and cite their sources.
Flume experiments on the erosion of abyssal calcareous ooze in shallow uniform flows of sea water show that erosion velocities range from 7–10 cm/sec soon after rapid deposition of the bed to 15–20 cm/sec after a few tens of hours. Continuing erosion produces shallow irregular longstream lineations but no sediment ripples. On the assumption of a hydrodynamically smooth boundary in the deep ocean, the measured erosion velocities can be approximately corrected for the effects of flow depth and water temperature different from oceanic conditions; even with this correction, the measured velocities are less than twice as great as current velocities common in the deep ocean.
No takes yet. Share an insight, caveat, or question.
Southard et al. (1971) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: