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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Main Authors: Todd, Claire E, Stone, John O, Conway, Howard, Hall, Brenda L, Bromley, Gordon RM
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
ipy
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.786188
https://doi.pangaea.de/10.1594/PANGAEA.786188
id ftdatacite:10.1594/pangaea.786188
record_format openpolar
spelling 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)
institution 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
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