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Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin

G. Almagor·R.H. Bennett·B.A. Mc Gregor·L.E. Shephard
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Abstract

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.

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G. Almagor, R.H. Bennett, B.A. Mc Gregor, L.E. Shephard. 1982. Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin. https://doi.org/10.1007/bf02462753

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