Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin
Stability analysis, based on infinite slope analysis and geotechnical data from a suite of 34 cores collected from the continental slope between Wilmington and Lindenkohl Canyons, indicates that the Quaternary surficial silty clay sediments on gentle slopes are stable; that sediment stability on steeper slopes (14??-19??) is marginal; and that on precipitous slopes (>50??) only a thin veneer of unconsolidated sediments can exist. Small earthquake-induced accelerations or the effects of internal waves can result in slope sediment instabilities. ?? 1982 A. M. Dowden, Inc.
Citation Information
Publication Year | 1982 |
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Title | Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin |
DOI | 10.1007/BF02462753 |
Authors | G. Almagor, R.H. Bennett, B.A. Mc Gregor, L.E. Shephard |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geo-Marine Letters |
Index ID | 70010391 |
Record Source | USGS Publications Warehouse |