Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ...
Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five site...
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ftdatacite:10.1594/pangaea.786188 2024-04-28T08:02:52+00:00 Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... Todd, Claire E Stone, John O Conway, Howard Hall, Brenda L Bromley, Gordon RM 2010 application/zip https://dx.doi.org/10.1594/pangaea.786188 https://doi.pangaea.de/10.1594/PANGAEA.786188 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2010.02.001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 ipy Ice measurement International Polar Year 2007-2008 IPY article Supplementary Publication Series of Datasets Collection 2010 ftdatacite https://doi.org/10.1594/pangaea.78618810.1016/j.quascirev.2010.02.001 2024-04-02T10:46:54Z Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five sites along its margin show that Reedy Glacier and its tributaries thickened asynchronously between 17 and 7 kyr BP At the Quartz Hills, located midway along the glacier, maximum ice levels were reached during the period 17-14 kyr BP. Farther up-glacier the ice surface reached its maximum elevation more recently: 14.7-10.2 kyr BP at the Caloplaca Hills; 9.1-7.7 kyr BP at Mims Spur; and around 7 kyr BP at Hatcher Bluffs. We attribute this time-transgressive behavior to two different processes: At the glacier mouth, growth of grounded ice and subsequent deglaciation in the Ross Sea embayment caused a wave of thickening and then thinning to propagate up-glacier. During the Lateglacial and Holocene, increased snow ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper Antarc* Antarctica International Polar Year IPY Reedy Glacier Ross Sea DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
ipy Ice measurement International Polar Year 2007-2008 IPY |
spellingShingle |
ipy Ice measurement International Polar Year 2007-2008 IPY Todd, Claire E Stone, John O Conway, Howard Hall, Brenda L Bromley, Gordon RM Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
topic_facet |
ipy Ice measurement International Polar Year 2007-2008 IPY |
description |
Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five sites along its margin show that Reedy Glacier and its tributaries thickened asynchronously between 17 and 7 kyr BP At the Quartz Hills, located midway along the glacier, maximum ice levels were reached during the period 17-14 kyr BP. Farther up-glacier the ice surface reached its maximum elevation more recently: 14.7-10.2 kyr BP at the Caloplaca Hills; 9.1-7.7 kyr BP at Mims Spur; and around 7 kyr BP at Hatcher Bluffs. We attribute this time-transgressive behavior to two different processes: At the glacier mouth, growth of grounded ice and subsequent deglaciation in the Ross Sea embayment caused a wave of thickening and then thinning to propagate up-glacier. During the Lateglacial and Holocene, increased snow ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... |
format |
Article in Journal/Newspaper |
author |
Todd, Claire E Stone, John O Conway, Howard Hall, Brenda L Bromley, Gordon RM |
author_facet |
Todd, Claire E Stone, John O Conway, Howard Hall, Brenda L Bromley, Gordon RM |
author_sort |
Todd, Claire E |
title |
Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
title_short |
Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
title_full |
Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
title_fullStr |
Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
title_full_unstemmed |
Surface exposure ages of samples obtained from Reedy Glacier, Antarctica ... |
title_sort |
surface exposure ages of samples obtained from reedy glacier, antarctica ... |
publisher |
PANGAEA |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.786188 https://doi.pangaea.de/10.1594/PANGAEA.786188 |
genre |
Antarc* Antarctica International Polar Year IPY Reedy Glacier Ross Sea |
genre_facet |
Antarc* Antarctica International Polar Year IPY Reedy Glacier Ross Sea |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2010.02.001 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.78618810.1016/j.quascirev.2010.02.001 |
_version_ |
1797574109236822016 |