Submarine evidence of the Aavatsmark and Dahl Glaciers fluctuations in the Kaffiøyra region, NW Spitsbergen
Abstract: Although the terrestrial marginal zones of some glaciers on Spitsbergen are rela− tively well described, we are largely ignorant about the morphology of their submarine forefields. Initial reconnaissance of the forefields of the Aavatsmark and Dahl glaciers in the Kaffiøyra region and soun...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.594.8939 http://www.polish.polar.pan.pl/ppr30/PPR30-143.pdf |