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High-resolution multibeam bathymetry acquired on the steep continental slope off Lofoten-Vesterålen (LV), North Norway, reveals approximately 15 canyons, some of which are incised 500–1100 m into a sedimentary succession of mainly Quaternary–Cenozoic age. The shape and size of canyons vary considerably, particularly in the southwest where the average slope gradient is 3–5° and where two of the canyons...
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