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| | Deepwater Sediments (Site not responding. Last check: 2007-11-03) |
 | | The majority of modern deepwater system sediments collect in bathyal water depths (200 - 2000 meters) on the outer margin of the continental shelf, down the continental slope and often to its base on the continental rise flanking the abyssal plain, and also on this plain (2,000 to 6,000 meters) itself. |
 | | The term "deep-water" refers to bathyal water-depth (>200 m) seaward of continental shelf break on the slope, and basin where sediment-gravity processes "slides, slumps, debris flows, and turbidity currents), and bottom currents are dominant depositional mechanisms. |
 | | These cohesive and non-cohesive end members collect as deepwater fans and other mass movement sediment bodies at the base of the breaks in slope on the sea floor. |
| strata.geol.sc.edu /terminology/deepWaterSediments.html (439 words) |
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