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Support Force Glacier
The Ministry for the Future / Kim Stanley Robinson
Davis Valley and Forlidas Pond, Dufek Massif
Coastal-Change and Glaciological Map of the Ronne Ice Shelf Area, Antarctica: 1974–2002
Reconstruction of Changes in the Weddell Sea Sector of the Antarctic Ice Sheet Since the Last Glacial Maximum
(ASPA) No. 119 DAVIS VALLEY and FORLIDAS POND
Greenbaum-Dissertation-2015
Reconstruction of Changes in the Weddell Sea Sector of the Antarctic Ice Sheet Since the Last Glacial Maximumq
Scientific Programme Tuesday, 19 June 2018 Opening Ceremony C I
Scaling of Instability Time-Scales of Antarctic Outlet Glaciers Based On
Glaciological Properties of the Antarctic Ice Sheet from RADARSAT-1 Synthetic Aperture Radar Imagery
Subglacial Sediment Transport Upstream of a Basal Channel in the Ice Shelf of Support Force Glacier (West Antarctica), Identified by Reflection Seismics
The Antarctic Treaty Cm 7166
Antarctic Ice Sheet Balance Velocities from Merged Point and Vector Data Abstract
Controls on Last Glacial Maximum Ice Extent in the Weddell Sea Embayment, Antarctica
FRISP) 15-18 September 2019, the Queen’S College, Oxford, UK
Scaling of Instability Timescales of Antarctic Outlet Glaciers Based on One-Dimensional Similitude Analysis
Petroleum and Mineral Resources of Antarctica
A New Bathymetry for the Southeastern Filchner-Ronne Ice 10.1029/2018JC013982 Shelf: Implications for Modern Oceanographic Processes
Top View
Ambio Annexe 1
Science Summaries 2016-17
Berichte 716 2018
Final Report of the Thirty-Sixth Antarctic Treaty Consultative Meeting
Scaling of Instability Time-Scales of Antarctic Outlet Glaciers Based On
The Limnology and Biology of the Dufek Massif, Transantarctic Mountains 82° South. D. A. Hodgson, P. Convey, E. Verleyen, W. Vy
ASPA) No. 119 DAVIS VALLEY and FORLIDAS POND, DUFEK MASSIF, PENSACOLA MOUNTAINS (51° 05' W, 82° 29' S
Hard Rock Landforms Generate 130€‰Km Ice Shelf Channels Through
The Antarctic Treaty
Instability Time-Scales of Antarctic Outlet Glaciers from Similitude Analysis
Organized Flow from the South Pole to the Filchner-Ronne Ice Shelf
COMPOSITE GAZETTEER of ANTARCTICA (CGA) Draft Of