| 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. Copyright ?? 1981 AAAS. |
| Genre: | Article |
| ProdID: | 70011712 |
| Citation Author: | Robb, J. M.; Hampson, Jr. , J. C.; Twichell, D. C. |
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| Citation End Page: | 937 |
| Citation Issue: | 4485 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | Geomorphology and sediment stability of a segment of the U.S. continental slope off New Jersey; 1981; Article; Journal; Science; Robb, J. M.; Hampson, Jr. , J. C.; Twichell, D. C. |
| Citation Start Page: | 935 |
| Citation Volume: | 211 |
| Citation Year: | 1981 |
| Type: | citation/reference |
| Text: | Geomorphology and sediment stability of a segment of the U.S. continental slope off New Jersey; 1981; Article; Journal; Science; Robb, J. M.; Hampson, Jr. , J. C.; Twichell, D. C. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1981 00:00 -0600 |
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