Glacial Isostatic Adjustment in response to changing Late Holocene behaviour of ice streams on the Siple Coast, West Antarctica.

The Siple Coast region of Antarctica contains a number of fast-flowing ice streams, which control the dynamics and mass balance of the region. These ice streams are known to undergo stagnation and reactivation cycles, which lead to ice thickness changes that may be sufficient to excite a viscous sol...

Full description

Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Nield, G.A., Whitehouse, P.L., King, M.K., Clarke, P.J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Oxford University Press 2016
Subjects:
Online Access:http://dro.dur.ac.uk/18129/
http://dro.dur.ac.uk/18129/1/18129.pdf
https://doi.org/10.1093/gji/ggv532