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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Bibliographic Details
Main Authors: Livingstone, SJ, Cofaigh, CÓ, Hogan, KA, Dowdeswell, Julian
Format: Text
Language:English
Published: Apollo - University of Cambridge Repository 2016
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.252
https://www.repository.cam.ac.uk/handle/1810/256310