2003Unpublished venueRequires access

HOLLISTER69: Sediments on the Shelf South of Martha's Vineyard

Lawrence J. Poppe

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Abstract

An unusual accumulation of incohesive fine-grained sediment (silt and clay) occurs in the midst of the sand-covered continental shelf south of artha's Vineyard. This 4000 square mile deposit of soft material is assumed to overlie relict Pleistocene sands. The objective of this study was to determine the distribution, thickness, and engineering properties of this fine grained deposit.

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What this paper is about

An unusual accumulation of incohesive fine-grained sediment (silt and clay) occurs in the midst of the sand-covered continental shelf south of artha's Vineyard. This 4000 square mile deposit of soft material is assumed to overlie relict Pleistocene sands. The objective of this study was to determine the distribution, thickness, and engineering properties of this fine grained deposit.

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Available abstract

An unusual accumulation of incohesive fine-grained sediment (silt and clay) occurs in the midst of the sand-covered continental shelf south of artha's Vineyard. This 4000 square mile deposit of soft material is assumed to overlie relict Pleistocene sands. The objective of this study was to determine the distribution, thickness, and engineering properties of this fine grained deposit.

Key concepts: Geology, Continental shelf, Silt, Vineyard, Pleistocene, Sediment, Square (algebra), Geomorphology

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