DEEP LAKE, CAPE BARNE-ANTARCTICA1

ablation, and a 3.3 m high ice cone to tilting of ice blocks beneath a gravel cover of varying thickness. The temperature of the lake water beneath the ice is thought to be a result of solar heating and the chemical stratification to bc an indication that there has been an arid period in the immedia...

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Main Authors: C. H. Hendy, M. J. Selby, A. T. Wilson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950
http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.581.9950 2023-05-15T14:03:09+02:00 DEEP LAKE, CAPE BARNE-ANTARCTICA1 C. H. Hendy M. J. Selby A. T. Wilson The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950 http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950 http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf text ftciteseerx 2016-08-28T00:02:12Z ablation, and a 3.3 m high ice cone to tilting of ice blocks beneath a gravel cover of varying thickness. The temperature of the lake water beneath the ice is thought to be a result of solar heating and the chemical stratification to bc an indication that there has been an arid period in the immediate past. Text Antarc* Unknown Barne ENVELOPE(166.233,166.233,-77.583,-77.583) Cape Barne ENVELOPE(166.433,166.433,-77.600,-77.600) Tilting ENVELOPE(-54.065,-54.065,49.700,49.700)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ablation, and a 3.3 m high ice cone to tilting of ice blocks beneath a gravel cover of varying thickness. The temperature of the lake water beneath the ice is thought to be a result of solar heating and the chemical stratification to bc an indication that there has been an arid period in the immediate past.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author C. H. Hendy
M. J. Selby
A. T. Wilson
spellingShingle C. H. Hendy
M. J. Selby
A. T. Wilson
DEEP LAKE, CAPE BARNE-ANTARCTICA1
author_facet C. H. Hendy
M. J. Selby
A. T. Wilson
author_sort C. H. Hendy
title DEEP LAKE, CAPE BARNE-ANTARCTICA1
title_short DEEP LAKE, CAPE BARNE-ANTARCTICA1
title_full DEEP LAKE, CAPE BARNE-ANTARCTICA1
title_fullStr DEEP LAKE, CAPE BARNE-ANTARCTICA1
title_full_unstemmed DEEP LAKE, CAPE BARNE-ANTARCTICA1
title_sort deep lake, cape barne-antarctica1
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950
http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf
long_lat ENVELOPE(166.233,166.233,-77.583,-77.583)
ENVELOPE(166.433,166.433,-77.600,-77.600)
ENVELOPE(-54.065,-54.065,49.700,49.700)
geographic Barne
Cape Barne
Tilting
geographic_facet Barne
Cape Barne
Tilting
genre Antarc*
genre_facet Antarc*
op_source http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950
http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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