Divergent flow of the West Antarctic Ice Sheet on the outer continental shelf of the Amundsen Sea during the late Quaternary

Authors

T. J. Deen, British Antarctic SurveyFollow
R. D. Larter, British Antarctic Survey
K. Gohl, Alfred Wegener Institute for Polar and Marine ResearchFollow
A. G.C. Graham, British Antarctic SurveyFollow
C.-D. Hillenbrand, British Antarctic Survey
G. Kuhn, Alfred Wegener Institute for Polar and Marine ResearchFollow
J. A. Smith, British Antarctic Survey

Date of this Version

2007

Comments

Citation: Deen, T.J., R.D. Larter, K. Gohl, A.G.C. Graham, C.-D. Hillenbrand, G. Kuhn, and J.A. Smith, (2007), Divergent flow of the West Antarctic Ice Sheet on the outer continental shelf of the Amundsen Sea during the late Quaternary: in Antarctica: A Keystone in a Changing World -Online Proceedings of the 10th ISAES, edited by A.K. Cooper and C.R. Raymond et al., USGS Open-File Report 2007-1047, Extended Abstract 213, 3 p.

Abstract

Understanding the past glacial history of regions undergoing potential rapid deglaciation is essential in order to estimate the possible threat of sea level rise. Recently acquired data have given new images of mega-scale glacial lineations on the sea floor of the Amundsen Sea, which provide us a new understanding of the direction of glacial flow on the continental shelf of the Amundsen Sea region. Two adjacent areas of seafloor on the outer shelf of the Amundsen Sea embayment exhibit remarkably different styles of glacial lineations, and allow the interpretation of a divergent glacial trough for the Pine Island Glacier during the last glacial maximum, whereas ice flow from the Abbot Ice Shelf probably converged with that from the Pine Island Glacier to the north of a grounding zone wedge.