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Formation of a large submarine crack during the final stage of retrogressive mass wasting on the continental slope offshore northern Norway
(2013)
High-resolution swath-bathymetry data integrated with sub-bottom profiles and single-channel seismics reveal an 18 km long, up to 1000 m wide and 10–15 m deep crack located approx. 4 km upslope from a slide scar on the ...