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continental rise

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continental rise
A wide, gentle incline from an ocean bottom to a continental slope. A continental rise consists mainly of silts, muds, and sand, and can be several hundreds of miles wide. Although it usually has a smooth surface, it is sometimes crosscut by submarine canyons.
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continental rise


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The continental rise is a layer of sediment from the base of the slope that forms a dip between the foot of the continental slope and the deep ocean floor.
Almost immediately, using conventional hydrography and a novel neutrally buoyant float that John Swallow (UK Institute of Ocean Sciences) had recently invented, Val Worthington (WHOI) and Swallow discovered the "Deep Western Boundary Current" part of the scheme on the Continental Rise south of Cape Cod.
Extending from the beach to the base of the continental rise, continental margin waters are the "ocean" most familiar to Earth's human population.
 
 
 
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