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The modern sedimentation regime at the snout of the Ferrar Glacier, New Harbour
Entry ID: K042_1985_1986_NZ_1

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Summary
Abstract: The modern sedimentation regime at the snout of the Ferrar Glacier was investigated for comparison with the upper sediments cored in the CIROS-2 hole and to determine the modern sedimentation processes on the McMurdo Sound sea floor. Seafloor sediments were taken near the outfall of two meltwater channels on the Ferrar Glacier snout to compare with sediments from the CIROS-2 core. A grid pattern ... View entire text
Related URL
Description: The Victoria University of Wellington Antarctic Research Centre homepage. All publications and data will be available through this group.
Geographic Coverage
Spatial coordinates   
  N: -77.67   S: -77.75   E: 164.0   W: 163.3

Temporal Coverage
Start Date: 1985-11-17
Stop Date: 1985-12-06
ISO Topic Category
Quality This study was completed for a BSc thesis. All the data is in the thesis and related publication.
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
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Publications/References
Kelly, D.N. 1986. Modern sedimentation in Ferrar Fjord, Antarctica. BSc Hons. Thesis. Victoria University of Wellington, New Zealand.

Pyne, A.R. 1986.McMurdo Sound Sediment Studies. In: Barrett, P. (comps) 1983 Immediate report of Victoria University of Wellington Antarctic Expedition 30, 1985-86. Wellington Antarctic Research Centre, Victoria University of Wellington pg 2-5.
Creation and Review Dates
DIF Creation Date: 2009-03-17
Last DIF Revision Date: 2009-03-17

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