Unconfined Creep of Polar Snow

Abstract Snow samples from the Amundsen-Scott South Pole station and “Byrd” station, Antarctica, and “Camp Century”, Greenland were tested for creep under low stresses for various periods of time up to two years. Creep was analyzed as a function of density. Comparisons of compressive viscosities plo...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: O. Ramseier, René, L. Pavlak, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1964
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029063
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029063
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spelling crcambridgeupr:10.1017/s0022143000029063 2024-03-03T08:36:38+00:00 Unconfined Creep of Polar Snow O. Ramseier, René L. Pavlak, Thomas 1964 http://dx.doi.org/10.1017/s0022143000029063 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029063 en eng Cambridge University Press (CUP) Journal of Glaciology volume 5, issue 39, page 325-332 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1964 crcambridgeupr https://doi.org/10.1017/s0022143000029063 2024-02-08T08:39:08Z Abstract Snow samples from the Amundsen-Scott South Pole station and “Byrd” station, Antarctica, and “Camp Century”, Greenland were tested for creep under low stresses for various periods of time up to two years. Creep was analyzed as a function of density. Comparisons of compressive viscosities plotted against densities for all three sites showed three distinct regions representing three different mechanisms of densification. Article in Journal/Newspaper Amundsen-Scott Antarc* Antarctica Greenland Journal of Glaciology South pole South pole Cambridge University Press Greenland South Pole Byrd Amundsen-Scott ENVELOPE(0.000,0.000,-90.000,-90.000) Byrd Station ENVELOPE(-119.533,-119.533,-80.017,-80.017) Amundsen Scott South Pole Station ENVELOPE(0.000,0.000,-90.000,-90.000) Amundsen-Scott South Pole Station ENVELOPE(139.273,139.273,-89.998,-89.998) Journal of Glaciology 5 39 325 332
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
O. Ramseier, René
L. Pavlak, Thomas
Unconfined Creep of Polar Snow
topic_facet Earth-Surface Processes
description Abstract Snow samples from the Amundsen-Scott South Pole station and “Byrd” station, Antarctica, and “Camp Century”, Greenland were tested for creep under low stresses for various periods of time up to two years. Creep was analyzed as a function of density. Comparisons of compressive viscosities plotted against densities for all three sites showed three distinct regions representing three different mechanisms of densification.
format Article in Journal/Newspaper
author O. Ramseier, René
L. Pavlak, Thomas
author_facet O. Ramseier, René
L. Pavlak, Thomas
author_sort O. Ramseier, René
title Unconfined Creep of Polar Snow
title_short Unconfined Creep of Polar Snow
title_full Unconfined Creep of Polar Snow
title_fullStr Unconfined Creep of Polar Snow
title_full_unstemmed Unconfined Creep of Polar Snow
title_sort unconfined creep of polar snow
publisher Cambridge University Press (CUP)
publishDate 1964
url http://dx.doi.org/10.1017/s0022143000029063
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029063
long_lat ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(-119.533,-119.533,-80.017,-80.017)
ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(139.273,139.273,-89.998,-89.998)
geographic Greenland
South Pole
Byrd
Amundsen-Scott
Byrd Station
Amundsen Scott South Pole Station
Amundsen-Scott South Pole Station
geographic_facet Greenland
South Pole
Byrd
Amundsen-Scott
Byrd Station
Amundsen Scott South Pole Station
Amundsen-Scott South Pole Station
genre Amundsen-Scott
Antarc*
Antarctica
Greenland
Journal of Glaciology
South pole
South pole
genre_facet Amundsen-Scott
Antarc*
Antarctica
Greenland
Journal of Glaciology
South pole
South pole
op_source Journal of Glaciology
volume 5, issue 39, page 325-332
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029063
container_title Journal of Glaciology
container_volume 5
container_issue 39
container_start_page 325
op_container_end_page 332
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