Geomorphology and sediment stability of a segment of the U.S. continental slope off New Jersey

James M. Robb; J.C. Hampson; D.C. Twichell

doi:10.1126/science.211.4485.935

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Geomorphology and sediment stability of a segment of the U.S. continental slope off New Jersey

James M. Robb·J.C. Hampson·D.C. Twichell

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Abstract

The morphology of complex deposits of Pleistocene sediments covering the upper continental slope between Lindenkohl Canyon and South Toms Canyon results from both depositional and erosional processes. Small slump or slide features were detected primarily on the flanks of canyons or valleys and were observed to occur only within Pleistocene-aged sediments. Eocene to Miocene sediments are exposed over much of the mid- and lower slope in this area.

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Source-reported bounding extent: 38.46903077827153° to 40.40015120680235° latitude; -74.37367385915496° to -72.66231852711805° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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James M. Robb, J.C. Hampson, D.C. Twichell. 1981. Geomorphology and sediment stability of a segment of the U.S. continental slope off New Jersey. https://doi.org/10.1126/science.211.4485.935

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