Submarine glacial-landform distribution along an Antarctic Peninsula palaeo-ice stream: a shelf-slope transect through the Marguerite Trough system (66° to 70°S)
The Antarctic Peninsula comprises a thin spine of mountains and islands presently covered by an ice sheet up to 500 m thick that drains eastwards and westwards via outlet glaciers (Davies et al. 2012). Recently, the Peninsula has undergone rapid warming, resulting in the collapse of fringing ice she...
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Format: | Text |
Language: | English |
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Apollo - University of Cambridge Repository
2016
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Online Access: | https://dx.doi.org/10.17863/cam.252 https://www.repository.cam.ac.uk/handle/1810/256310 |