|
The structural glaciology, ice marginal landforms, sediments and movement of the Lower Wright Glacier, Wright Valley, Antarctica
Entry ID:
K064_1994_2005_NZ_2
Summary
Abstract:
The structural glaciology, ice marginal landforms, sediments and movement of the Lower Wright Glacier, Wright Valley, Antarctica was investigated over several seasons. Preliminary work was completed with mapping, surveying and logging ice marginal sediments and landforms of the Lower Wright Glacier. Ice was sampled from moraines at the left margin of the glacier and from the contact between ...
![]()
Related URL
Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
Parent DIF
This data set description is a member of a collection. The
collection is described in
K064_1994_2005_NZ Paleo Temporal Coverage
Chrono Unit:
Location Keywords
Science Keywords
TERRESTRIAL HYDROSPHERE
>
GLACIERS/ICE SHEETS
>
GLACIERS
TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER TOPOGRAPHY/ICE SHEET TOPOGRAPHY TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MOTION/ICE SHEET MOTION ISO Topic Category
Platform
Project
Quality
Any existing samples that have not been used are stored in a MAF-registered transitional facilities in the Geography department at the University of Otago, New Zealand. All data is in the thesis and publication. Please contact the investigator for more information.
Ancillary Keywords
Data Set Progress
COMPLETE
Data Center
Personnel
Publications/References
Mager, S. 2005. A compositional approach to understanding the formation of basal ice in cold Antarctic glaciers. Unpublished PhD thesis in Geography and Chemistry, University of Otago, Dunedin, New Zealand. 220 pp.
Mager, S. 1996. Sediment transport in dry-based glaciers : an assessment of sedimentary signatures imprinted by glacial transportation. Unpublished BSc (hons) ... ![]() Creation and Review Dates
DIF Creation Date:
2005-09-22
Last DIF Revision Date:
2009-03-27
|
||||||||||||||||||






