Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica
Subglacial curved and winding meltwater channels, and Sichelwannen are recorded from Cape Jones in the Obruchev Hills. Such channels, sometimes referred to as P‐forms, may have a variety of origins. After briefly considering the origins, it is deduced that those at Cape Jones were formed subglaciall...
Published in: | Australian Geographical Studies |
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Language: | English |
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1989
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crwiley:10.1111/j.1467-8470.1989.tb00605.x 2024-06-02T07:58:32+00:00 Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica COLHOUN, ERIC A. ADAMSON, DONALD A. 1989 http://dx.doi.org/10.1111/j.1467-8470.1989.tb00605.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1467-8470.1989.tb00605.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1467-8470.1989.tb00605.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Australian Geographical Studies volume 27, issue 2, page 234-246 ISSN 0004-9190 1467-8470 journal-article 1989 crwiley https://doi.org/10.1111/j.1467-8470.1989.tb00605.x 2024-05-03T11:44:08Z Subglacial curved and winding meltwater channels, and Sichelwannen are recorded from Cape Jones in the Obruchev Hills. Such channels, sometimes referred to as P‐forms, may have a variety of origins. After briefly considering the origins, it is deduced that those at Cape Jones were formed subglacially while the ice surface of the Denman Glacier became lower and bedrock was exposed The presence of water‐laid glacial deposits on the summit of Cape Jones, and lakes on and adjacent to the eastern margin of the Denman Glacier suggests that the sudden release of impounded meltwater was important Article in Journal/Newspaper Antarc* Antarctica Denman Glacier Wiley Online Library Cape Jones ENVELOPE(-67.016,-67.016,-67.500,-67.500) Denman Glacier ENVELOPE(99.417,99.417,-66.750,-66.750) Obruchev ENVELOPE(154.200,154.200,-68.900,-68.900) Obruchev Hills ENVELOPE(99.767,99.767,-66.583,-66.583) Australian Geographical Studies 27 2 234 246 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Subglacial curved and winding meltwater channels, and Sichelwannen are recorded from Cape Jones in the Obruchev Hills. Such channels, sometimes referred to as P‐forms, may have a variety of origins. After briefly considering the origins, it is deduced that those at Cape Jones were formed subglacially while the ice surface of the Denman Glacier became lower and bedrock was exposed The presence of water‐laid glacial deposits on the summit of Cape Jones, and lakes on and adjacent to the eastern margin of the Denman Glacier suggests that the sudden release of impounded meltwater was important |
format |
Article in Journal/Newspaper |
author |
COLHOUN, ERIC A. ADAMSON, DONALD A. |
spellingShingle |
COLHOUN, ERIC A. ADAMSON, DONALD A. Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
author_facet |
COLHOUN, ERIC A. ADAMSON, DONALD A. |
author_sort |
COLHOUN, ERIC A. |
title |
Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
title_short |
Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
title_full |
Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
title_fullStr |
Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
title_full_unstemmed |
Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica |
title_sort |
subglacial meltwater channels at cape jones, obruchev hills, antarctica |
publisher |
Wiley |
publishDate |
1989 |
url |
http://dx.doi.org/10.1111/j.1467-8470.1989.tb00605.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1467-8470.1989.tb00605.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1467-8470.1989.tb00605.x |
long_lat |
ENVELOPE(-67.016,-67.016,-67.500,-67.500) ENVELOPE(99.417,99.417,-66.750,-66.750) ENVELOPE(154.200,154.200,-68.900,-68.900) ENVELOPE(99.767,99.767,-66.583,-66.583) |
geographic |
Cape Jones Denman Glacier Obruchev Obruchev Hills |
geographic_facet |
Cape Jones Denman Glacier Obruchev Obruchev Hills |
genre |
Antarc* Antarctica Denman Glacier |
genre_facet |
Antarc* Antarctica Denman Glacier |
op_source |
Australian Geographical Studies volume 27, issue 2, page 234-246 ISSN 0004-9190 1467-8470 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1467-8470.1989.tb00605.x |
container_title |
Australian Geographical Studies |
container_volume |
27 |
container_issue |
2 |
container_start_page |
234 |
op_container_end_page |
246 |
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1800741921999552512 |