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Measurements of the effects of debris on the mechanical behaviour (deformation and motion) of ice of the Taylor Glacier, Taylor Valley, Antarctica
Entry ID: K053_1992_2000_NZ_1

Abstract: Debris-rich ice is a commonly observed basal ice facies found at the base of many temperate and polar glaciers and at the base of cores through major ice sheets. The effects of the presence of debris on the mechanical behaviour of ice was investigated and then the implication of those effects for the overall dynamics of ice masses was examined at the Taylor Glacier, Taylor Valley, Antarctica over ... View entire text
Geographic Coverage
Spatial coordinates   
  N: -77.73   S: -77.73   E: 162.17   W: 162.17

Temporal Coverage
Start Date: 1992-12-14
Stop Date: 1993-01-16
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ISO Topic Category
start here with 1 in span in link Ancillary Description
here with 2 in span in link Ancillary Description
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Data Center
Antarctica New Zealand, New Zealand Antarctic Institute, New Zealand Supplemental Info
Data Center URL: http://www.antarcticanz.govt.nz/

Data Center Personnel
Phone: +64 3 358 0200
Fax: +64 3 358 0211
Email: s.gordon at antarcticanz.govt.nz
Contact Address:
Antarctica New Zealand
Private Bag 4745
City: Christchurch
Country: New Zealand
Phone: +64 03 364 2920
Fax: +64 03 364 2907
Email: wendy.lawson at canterbury.ac.nz
Contact Address:
Geography Department
University of Canterbury
Private Bag 4745
City: Christchurch
Postal Code: 4800
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Lawson W J, 1996, The relative strengths of clean and debris-laden ice: evidence from Taylor Glacier, Antarctica, Annals of Glaciology, Vol 23, pp 270-276.

Lawson, W. Elliott, C. Strain-rate effects on the strength of debris-laden glacier ice. New Zealand journal of geology and geophysics 46(3): 323-330, 2003.

Hubbard, A., Lawson W., Anderson B., Hindmarsh R., Hubbard, ... View entire text
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Creation and Review Dates
DIF Creation Date: 2009-02-11
Last DIF Revision Date: 2017-08-23

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