ARCTIC Internal Structure and Environmental Significance of a
ABSTRACT. A perennial snowbank located in the continuous permafrost zone was cored to obtain details of its internal structure and history. In spring the snowbank is up to 10 m thick and composed of deep snow accumulated during the previous winter, overlying ice developed by basal ice accretion over...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.546.7384 2023-05-15T14:19:37+02:00 ARCTIC Internal Structure and Environmental Significance of a Anton G Lewkowicz David G. Harry The Pennsylvania State University CiteSeerX Archives 1990 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7384 http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7384 http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf text 1990 ftciteseerx 2016-01-08T11:19:27Z ABSTRACT. A perennial snowbank located in the continuous permafrost zone was cored to obtain details of its internal structure and history. In spring the snowbank is up to 10 m thick and composed of deep snow accumulated during the previous winter, overlying ice developed by basal ice accretion over many years. The perennial ice exhibits a layered structure with alternating clear and milky bands and contains randomly oriented, variably shaped bubbles. Horizons of aeolian and mudflow deposits occur at irregular intervals and correspond to periods of aggradation and thaw truncation of the snowbank. ’Ititium concentrations in a core from the deepest portion of the snowbank indicate that the basal 2 m of ice pre-dates 1957. Other layers Text Arctic Arctic Ice permafrost Unknown Arctic |
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Open Polar |
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Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
ABSTRACT. A perennial snowbank located in the continuous permafrost zone was cored to obtain details of its internal structure and history. In spring the snowbank is up to 10 m thick and composed of deep snow accumulated during the previous winter, overlying ice developed by basal ice accretion over many years. The perennial ice exhibits a layered structure with alternating clear and milky bands and contains randomly oriented, variably shaped bubbles. Horizons of aeolian and mudflow deposits occur at irregular intervals and correspond to periods of aggradation and thaw truncation of the snowbank. ’Ititium concentrations in a core from the deepest portion of the snowbank indicate that the basal 2 m of ice pre-dates 1957. Other layers |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Anton G Lewkowicz David G. Harry |
spellingShingle |
Anton G Lewkowicz David G. Harry ARCTIC Internal Structure and Environmental Significance of a |
author_facet |
Anton G Lewkowicz David G. Harry |
author_sort |
Anton G Lewkowicz |
title |
ARCTIC Internal Structure and Environmental Significance of a |
title_short |
ARCTIC Internal Structure and Environmental Significance of a |
title_full |
ARCTIC Internal Structure and Environmental Significance of a |
title_fullStr |
ARCTIC Internal Structure and Environmental Significance of a |
title_full_unstemmed |
ARCTIC Internal Structure and Environmental Significance of a |
title_sort |
arctic internal structure and environmental significance of a |
publishDate |
1990 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7384 http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Arctic Ice permafrost |
genre_facet |
Arctic Arctic Ice permafrost |
op_source |
http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7384 http://pubs.aina.ucalgary.ca/arctic/Arctic44-1-74.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766291404981534720 |