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Published byLenard Walker Modified over 6 years ago
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Disturbance of seafloor sediments on high-latitude shelves.
Disturbance of seafloor sediments on high-latitude shelves. (a) Pockmarks in the SW Barents Sea (modified from Chand et al. 2016). (b) Trawl marks and possible whale-feeding marks in the Barents Sea (modified from Thorsnes et al. 2016). (c) Pipeline (1.5 m wide) crossing an otherwise flat area of the Baltic Sea floor (courtesy of UK Seafloor Mapping Ltd.). J. A. Dowdeswell et al. Geological Society, London, Memoirs 2016;46: © 2016 The Author(s). Published by The Geological Society of London
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