Submarine glacial-landform distribution along an Antarctic Peninsula palaeo-ice stream: a shelf-slope transect through the Marguerite Trough system (66-70 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 eastward and westward via outlet glaciers (Davies et al. 2012). The peninsula has undergone recent rapid warming, resulting in the collapse of fringing ice shelves...

Full description

Bibliographic Details
Published in:Geological Society, London, Memoirs
Main Authors: Livingstone, S. J., O Cofaigh, C., Hogan, K. A., Dowdeswell, J. A.
Other Authors: Dowdeswell, J.A., Canals, M., Jakobsson, M., Todd, B.J., Dowdeswell, E.K., Hogan, K.A.
Format: Book Part
Language:unknown
Published: Geological Society of London 2016
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/515715/
https://doi.org/10.1144/M46.180