Corrigendum to "Switching of a paleo-ice stream in northwest Svalbard" [Quat. Sci. Rev. 30 (2011), 1710-1725]

• Published in: Quaternary Science Reviews
• Main Authors: Sarkar, Sudipta, Berndt, Christian, Chabert, Anne, Masson, Douglas G., Minshull, Timothy A., Westbrook, Graham K.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2013
• Subjects: Svalbard; Yermak Plateau; Ice Sheet; Kongsfjord*; Kongsfjorden; Svalbard margin; Van Mijenfjord; Yermak plateau; Spitsbergen
• Online Access: http://nora.nerc.ac.uk/id/eprint/502175/

Ice streams are the fast-flowing zones of ice sheets that can discharge a large flux of ice. The glaciated western Svalbard margin consists of several cross-shelf troughs which are the former ice stream drainage pathways during the Pliocene–Pleistocene glaciations. From an integrated analysis of hig...