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Record Search Query: [Parameters: Topic='SOLID EARTH', Term='GEOMORPHIC LANDFORMS/PROCESSES', Variable_Level_1='GLACIAL LANDFORMS']
The geology of the Northern Britannia Range between the Hatherton and Byrd Glaciers
Entry ID: K009_1978_1979_NZ_1

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Summary
Abstract: The geology of the Northern Britannia Range between the Hatherton and Byrd Glaciers was mapped and the landforms, soils and glacial history of the range was investigated. A four man team man-hauled a Nansen sledge down the Hatherton Glacier, making measurements of hard rocks outcropping within the northern Britannia Range along the way. A geological outcrop map was produced, the general geology of ... View entire text
Related URL
Description: The investigators homepage
Geographic Coverage
Spatial coordinates   
  N: -79.0   S: -81.0   E: 160.0   W: 155.0

Parent DIF
This data set description is a member of a collection. The collection is described in
K009_1969_1990_NZ_1

Temporal Coverage
Start Date: 1978-11-12
Stop Date: 1979-01-08
ISO Topic Category
Quality Please check the publications or contact the investigator for more information.
Ancillary Keywords
Data Set Progress
COMPLETE
Data Center
Antarctica New Zealand, New Zealand Antarctic Institute, New Zealand Supplemental Info
Data Center URL: http://www.antarcticanz.govt.nz/

Data Center Personnel
Name: SHULAMIT GORDON
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
Personnel
Role: INVESTIGATOR
Phone: +64 7 856 2889 Ext 4381 Or 4392
Fax: +64 7 838 4218
Email: c.hendy at waikato.ac.nz
Contact Address:
Department of Chemistry
University of Waikato
Private Bag 3105
City: Hamilton
Country: New Zealand
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Publications/References
Selby, M.J. Rock mass strength classification for geomorphic purposes: with tests from Antarctica and New Zealand. Zeitschrift für geomorphologie 24(1): 31-51, 1980.
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Creation and Review Dates
DIF Creation Date: 2009-04-15
Last DIF Revision Date: 2009-04-20

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