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Subsequently, the behaviour and depositional processes of bottom currents upstream and downstream the seamount are discussed.
From the Middle Pleistocene onwards, separated mounded drift deposits were formed due to intensified bottom currents.
The measurements showed unexpectedly that bottom currents were relatively stronger than surface currents during May-99.
The bottles, as well as seabed drifters that Mr. Bumpus used to measure bottom currents, traveled near and far.
These animals were solitary suspension feeders that grew in such great profusion that they affected bottom currents and water circulation.
Combined with the known oceanographic setting, the bottom currents could belong to the anticyclonic South China Sea Intermediate Water circulation.
Similar(11)
The bottom current, moving out into the Atlantic, is even stronger.
Undertow, a strong seaward bottom current returning the water of broken waves back out to sea.
The succession was deposited during varying bottom current intensities and the depositional architecture indicates a complex and dynamic environment.
Deposition within this extensional growth slope is dominated by either platform-derived downslope sedimentation or bottom current sedimentation.
A moat formed north of the seamount as a result of bottom current intensification after being deflected by an obstacle morphology, indicating a major eastward flowing current.
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