Formation of a pronival rampart on sub-Antarctic Marion Island
Abstract The formation of a pronival (protalus) rampart on sub-Antarctic Marion Island is investigated. Morphological attributes show debris at the angle of repose on the rampart's proximal slope and at a lower angle on the distal slope. Relative-age dating, based on the percentage moss cover a...
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Language: | English |
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Cambridge University Press (CUP)
2007
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Online Access: | http://dx.doi.org/10.1017/s0954102007000582 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102007000582 |
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crcambridgeupr:10.1017/s0954102007000582 2024-09-09T19:09:42+00:00 Formation of a pronival rampart on sub-Antarctic Marion Island Hedding, David W. Sumner, Paul D. Holness, Stephen D. Meiklejohn, K. Ian 2007 http://dx.doi.org/10.1017/s0954102007000582 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102007000582 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 19, issue 4, page 443-450 ISSN 0954-1020 1365-2079 journal-article 2007 crcambridgeupr https://doi.org/10.1017/s0954102007000582 2024-06-19T04:03:41Z Abstract The formation of a pronival (protalus) rampart on sub-Antarctic Marion Island is investigated. Morphological attributes show debris at the angle of repose on the rampart's proximal slope and at a lower angle on the distal slope. Relative-age dating, based on the percentage moss cover and weathering rind thickness of the clastic component, indicates accumulation mainly on the proximal slope and rampart crest, implying upslope (retrogressive) accumulation. This contrasts with a previously published model for pronival ramparts, which proposes rampart growth by addition of material to the distal slope. Development of the Marion Island rampart is suggested to result from the control exerted by a relatively low-angled surface and a shrinking snowbed. A small debris step formed on the proximal slope appears to be a response to decreased snowfalls due to changing climate over the last c . 50 years. Growth rate of the rampart is considered to be variable during the Holocene in response to changes in climate and debris supply. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Marion Island Cambridge University Press Antarctic Antarctic Science 19 4 443 450 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract The formation of a pronival (protalus) rampart on sub-Antarctic Marion Island is investigated. Morphological attributes show debris at the angle of repose on the rampart's proximal slope and at a lower angle on the distal slope. Relative-age dating, based on the percentage moss cover and weathering rind thickness of the clastic component, indicates accumulation mainly on the proximal slope and rampart crest, implying upslope (retrogressive) accumulation. This contrasts with a previously published model for pronival ramparts, which proposes rampart growth by addition of material to the distal slope. Development of the Marion Island rampart is suggested to result from the control exerted by a relatively low-angled surface and a shrinking snowbed. A small debris step formed on the proximal slope appears to be a response to decreased snowfalls due to changing climate over the last c . 50 years. Growth rate of the rampart is considered to be variable during the Holocene in response to changes in climate and debris supply. |
format |
Article in Journal/Newspaper |
author |
Hedding, David W. Sumner, Paul D. Holness, Stephen D. Meiklejohn, K. Ian |
spellingShingle |
Hedding, David W. Sumner, Paul D. Holness, Stephen D. Meiklejohn, K. Ian Formation of a pronival rampart on sub-Antarctic Marion Island |
author_facet |
Hedding, David W. Sumner, Paul D. Holness, Stephen D. Meiklejohn, K. Ian |
author_sort |
Hedding, David W. |
title |
Formation of a pronival rampart on sub-Antarctic Marion Island |
title_short |
Formation of a pronival rampart on sub-Antarctic Marion Island |
title_full |
Formation of a pronival rampart on sub-Antarctic Marion Island |
title_fullStr |
Formation of a pronival rampart on sub-Antarctic Marion Island |
title_full_unstemmed |
Formation of a pronival rampart on sub-Antarctic Marion Island |
title_sort |
formation of a pronival rampart on sub-antarctic marion island |
publisher |
Cambridge University Press (CUP) |
publishDate |
2007 |
url |
http://dx.doi.org/10.1017/s0954102007000582 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102007000582 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctic Science Marion Island |
genre_facet |
Antarc* Antarctic Antarctic Science Marion Island |
op_source |
Antarctic Science volume 19, issue 4, page 443-450 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0954102007000582 |
container_title |
Antarctic Science |
container_volume |
19 |
container_issue |
4 |
container_start_page |
443 |
op_container_end_page |
450 |
_version_ |
1809823958894116864 |