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Science 26 April 2002:
Vol. 296. no. 5568, pp. 724 - 727
DOI: 10.1126/science.1069803

Reports

The Shaping of Continental Slopes by Internal Tides

D. A. Cacchione,1 L. F. Pratson,2 A. S. Ogston3

The angles of energy propagation of semidiurnal internal tides may determine the average gradient of continental slopes in ocean basins (~2 to 4 degrees). Intensification of near-bottom water velocities and bottom shear stresses caused by reflection of semi-diurnal internal tides affects sedimentation patterns and bottom gradients, as indicated by recent studies of continental slopes off northern California and New Jersey. Estimates of bottom shear velocities caused by semi-diurnal internal tides are high enough to inhibit deposition of fine-grained sediment onto the slopes.

1 Coastal and Marine Geology MS-999, U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.
2 Earth & Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, NC 27708, USA.
3 University of Washington, Box 357940, Seattle, WA 98195, USA.


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Science. ISSN 0036-8075 (print), 1095-9203 (online)