Evidence of surges on the Barnes Ice Cap, Baffin Island

The morphology of the Barnes Ice Cap is studied on the basis of detailed topographic maps. Two anomalous areas characterized by an apparent excess of mass at lower elevations and a similar deficit at higher altitudes are identified. Local surges affecting these two parts of the ice cap could have ca...

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Published in:Canadian Journal of Earth Sciences
Main Author: Løken, O. H.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1969
Subjects:
Online Access:http://dx.doi.org/10.1139/e69-093
http://www.nrcresearchpress.com/doi/pdf/10.1139/e69-093
id crcansciencepubl:10.1139/e69-093
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spelling crcansciencepubl:10.1139/e69-093 2023-12-17T10:27:35+01:00 Evidence of surges on the Barnes Ice Cap, Baffin Island Løken, O. H. 1969 http://dx.doi.org/10.1139/e69-093 http://www.nrcresearchpress.com/doi/pdf/10.1139/e69-093 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 6, issue 4, page 899-901 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1969 crcansciencepubl https://doi.org/10.1139/e69-093 2023-11-19T13:38:45Z The morphology of the Barnes Ice Cap is studied on the basis of detailed topographic maps. Two anomalous areas characterized by an apparent excess of mass at lower elevations and a similar deficit at higher altitudes are identified. Local surges affecting these two parts of the ice cap could have caused this mass distribution. The moraine patterns adjacent to the ice cap show that the ice margin in the two areas has recently advanced in distinct contrast to the general retreat in adjacent areas. Article in Journal/Newspaper Baffin Island Baffin Barnes Ice Cap Ice cap Canadian Science Publishing (via Crossref) Baffin Island Barnes Ice Cap ENVELOPE(-73.498,-73.498,70.001,70.001) Canadian Journal of Earth Sciences 6 4 899 901
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Løken, O. H.
Evidence of surges on the Barnes Ice Cap, Baffin Island
topic_facet General Earth and Planetary Sciences
description The morphology of the Barnes Ice Cap is studied on the basis of detailed topographic maps. Two anomalous areas characterized by an apparent excess of mass at lower elevations and a similar deficit at higher altitudes are identified. Local surges affecting these two parts of the ice cap could have caused this mass distribution. The moraine patterns adjacent to the ice cap show that the ice margin in the two areas has recently advanced in distinct contrast to the general retreat in adjacent areas.
format Article in Journal/Newspaper
author Løken, O. H.
author_facet Løken, O. H.
author_sort Løken, O. H.
title Evidence of surges on the Barnes Ice Cap, Baffin Island
title_short Evidence of surges on the Barnes Ice Cap, Baffin Island
title_full Evidence of surges on the Barnes Ice Cap, Baffin Island
title_fullStr Evidence of surges on the Barnes Ice Cap, Baffin Island
title_full_unstemmed Evidence of surges on the Barnes Ice Cap, Baffin Island
title_sort evidence of surges on the barnes ice cap, baffin island
publisher Canadian Science Publishing
publishDate 1969
url http://dx.doi.org/10.1139/e69-093
http://www.nrcresearchpress.com/doi/pdf/10.1139/e69-093
long_lat ENVELOPE(-73.498,-73.498,70.001,70.001)
geographic Baffin Island
Barnes Ice Cap
geographic_facet Baffin Island
Barnes Ice Cap
genre Baffin Island
Baffin
Barnes Ice Cap
Ice cap
genre_facet Baffin Island
Baffin
Barnes Ice Cap
Ice cap
op_source Canadian Journal of Earth Sciences
volume 6, issue 4, page 899-901
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e69-093
container_title Canadian Journal of Earth Sciences
container_volume 6
container_issue 4
container_start_page 899
op_container_end_page 901
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