Subglacial melt channels and fracture in the floating part of Pine Island Glacier, Antarctica

A dense grid of ice-penetrating radar sections acquired over Pine Island Glacier, West Antarctica has revealed a network of sinuous subglacial channels, typically 500m to 3km wide, and up to 200m high, in the ice-shelf base. These subglacial channels develop while the ice is floating and result from...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Vaughan, David, Corr, Hugh, Bindschadler, Robert, Dutrieux, Pierre, Gudmundsson, Hilmar, Jenkins, Adrian, Newman, Thomas, Vornberger, Patricia, Wingham, Duncan
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2012
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/37393/
https://doi.org/10.1029/2012JF002360