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- W1979226117 abstract "A detailed study of the eastern margin of the Rockall Plateau using topographic and seismic profiler data has revealed two large slumps on the upper parts of the slope. The upper of the two slumps can be traced for 160 km, has an average width of 14 km and an estimated volume of 2.96·1011 m3. Interpretation of the seismic profiles and the available geological data suggests the slumps may be as young as Pleistocene in age and developed in a slope of 2°. Their origin is not clear; they may have developed as a consequence of lower sea level during the Pleistocene although they may also be indirectly related to the subsidence of the Rockall Plateau." @default.
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- W1979226117 date "1972-11-01" @default.
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- W1979226117 title "Slumping on the eastern margin of the Rockall Bank, North Atlantic Ocean" @default.
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- W1979226117 doi "https://doi.org/10.1016/0025-3227(72)90052-7" @default.
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