[Location: Location_Category='CONTINENT', Location_Type='ANTARCTICA', Detailed_Location='BEACON VALLEY']
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Soil pit description and analysis (thin sections, cation and anion chemistry of soluble salts) from Beacon, Arena and Pearce Valley to determine the origin of ground ice at high elevations in the Dry Valleys
Entry ID:
K047_2001_2002_NZ_1
Summary
Abstract:
The origin of ground ice at high elevations (>1000m) throughout the Dry Valleys of Antarctica was investigated as the origin is unclear because there is no obvious comtemporary source of water. A model to explain the occurrence of ground ice in glacial sediments and bedrock was developed from previous work at Table Mountain. The model is based on mineralogical, chemical and isotopic analyses of ...
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Spatial coordinates
Temporal Coverage
Start Date:
2001-11-15
Stop Date:
2001-12-05
Location Keywords
Science Keywords
ISO Topic Category
Instrument
Quality
The data remains with the investigator. Please contact him for more information.
Data Set Progress
COMPLETE
Data Center
Personnel
Publications/References
Dickinson, W.W. Rosen, M.R. Antarctica permafrost: an analogue for water and diagenetic minerals on Mars. Geology 31(3): 199-202, 2003.
Creation and Review Dates
DIF Creation Date:
2009-03-03
Last DIF Revision Date:
2009-03-03
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