Bedrock channels in Pine Island Bay, West Antarctica

The seafloor of inner continental shelves on glaciated margins is sometimes stripped of most of the softer sediments, leaving bedrock exposed (Wellner et al. 2001). Examples of such exposed bedrock regions have been observed in the inner parts of several cross-shelf troughs on the West Antarctica margin, including those in the Amundsen Sea (Lowe & Anderson 2003; Graham et al. 2009) and Marguerite Bay (Anderson & Fretwell 2008). The detailed morphology of these areas consists of various features of glacial origin, predominantly parallel grooves or striations. These areas can also contain sinuous channels that are incised deeply into the rock substrate.

Details

Publication status:
Published
Author(s):
Authors: Nitsche, F.O., Larter, R.D., Gohl, K., Graham, A.G.C., Kuhn, G.

Editors: Dowdeswell, J.A., Canals, M., Jakobsson, M., Todd, B.J., Dowdeswell, E.K., Hogan, K.A.

On this site: Kelly Hogan, Robert Larter
Date:
1 January, 2016
Journal/Source:
In: Dowdeswell, J.A., Canals, M., Jakobsson, M., Todd, B.J., Dowdeswell, E.K., Hogan, K.A. (eds.). Atlas of Submarine Glacial Landforms: modern, Quaternary and ancient, London, Geological Society of London, 217-218.
Page(s):
217-218
Digital Object Identifier (DOI):
https://doi.org/10.1144/M46.1