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The eastern flank of the Rockall Bank is dominated by the scarps of a large slide complex with unusual low aspect ratio (120km wide and 150km long). With the use of an extensive 2D seismic dataset, re-processed high-resolution multibeam bathymetry, a TOBI mosaic and one piston core we demonstrate that the headwall of the Rockall Bank Slide Complex (previously referred to as the Rockall Bank Mass Flow)...
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