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The northern mid-Norwegian continental slope was studied based on high-resolution side-scan sonar data, multibeam bathymetry, high-resolution and multichannel seismics together with gravity cores. Sedimentary provinces identified include a partly buried slide on the eastern, inner Voring Plateau, an area dominated by glacigenic debris flows south-west of the Traenadjupet Slide, the Traenadjupet Slide,...
Shallow-seismic surveys around the Storegga Slide off western Norway have allowed greater understanding of the development of this part of the European margin. The northern flank of the scarp is formed of seismically well-layered, hemipelagic and distal-glaciomarine deposits in which a variety of fluid-escape structures, probably due to gas, are locally abundant. There is evidence of slides that...
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