Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations
Rare jkulhlaup events, also known as subglacial lake outburst flood events, have been observed at the Law Dome ice margin and provide an insight into the physical characteristics of subglacial meltwater and drainage. The subglacial topography based on data from the BEDMAP2 and ICECAP projects, toget...
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Online Access: | https://doi.org/10.1144/SP461.16 http://ecite.utas.edu.au/118721 |
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ftunivtasecite:oai:ecite.utas.edu.au:118721 2023-05-15T13:49:03+02:00 Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations Goodwin, ID Roberts, JL Etheridge, DM Hellstrom, J Moy, AD Ribo, M Smith, AM 2017 https://doi.org/10.1144/SP461.16 http://ecite.utas.edu.au/118721 en eng Geological Society Publishing House http://dx.doi.org/10.1144/SP461.16 Goodwin, ID and Roberts, JL and Etheridge, DM and Hellstrom, J and Moy, AD and Ribo, M and Smith, AM, Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations, Geological Society Special Publication, 461 Article SP461.16. ISSN 0305-8719 (2017) [Refereed Article] http://ecite.utas.edu.au/118721 Earth Sciences Physical Geography and Environmental Geoscience Glaciology Refereed Article PeerReviewed 2017 ftunivtasecite https://doi.org/10.1144/SP461.16 2019-12-13T22:17:57Z Rare jkulhlaup events, also known as subglacial lake outburst flood events, have been observed at the Law Dome ice margin and provide an insight into the physical characteristics of subglacial meltwater and drainage. The subglacial topography based on data from the BEDMAP2 and ICECAP projects, together with subsurface transects of the ice margin obtained using groundpenetrating radar, reveal several lakes and lake-like depressions and the drainage pathways of two jkulhlaup events. Oxygen isotope typing of the meltwater during the most recent (2014) jkulhlaup event, combined with ice margin stratigraphy, enable the identification of ice tunnel melt pathways that exploit the 3090 dipping basal ice layering. The presence of subglacial meltwater beneath Law Dome during the Holocene to Glacial periods is confirmed by the dendritic drainage pattern in the subglacial morphology and extensive layers of basal regelation ice and subglacial carbonate precipitate deposits found within the Lken Moraines sediments. These subglacial carbonates, including ooid layers, formed from the mixing of glacial meltwater and seawater at 72 ka BP. The combined evidence indicates that the ocean discharge of subglacial meltwater may be variable and/or is periodically blocked by basal freezing events near the ice sheet terminus. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet eCite UTAS (University of Tasmania) East Antarctica Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733) Geological Society, London, Special Publications 461 1 215 230 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology Goodwin, ID Roberts, JL Etheridge, DM Hellstrom, J Moy, AD Ribo, M Smith, AM Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
description |
Rare jkulhlaup events, also known as subglacial lake outburst flood events, have been observed at the Law Dome ice margin and provide an insight into the physical characteristics of subglacial meltwater and drainage. The subglacial topography based on data from the BEDMAP2 and ICECAP projects, together with subsurface transects of the ice margin obtained using groundpenetrating radar, reveal several lakes and lake-like depressions and the drainage pathways of two jkulhlaup events. Oxygen isotope typing of the meltwater during the most recent (2014) jkulhlaup event, combined with ice margin stratigraphy, enable the identification of ice tunnel melt pathways that exploit the 3090 dipping basal ice layering. The presence of subglacial meltwater beneath Law Dome during the Holocene to Glacial periods is confirmed by the dendritic drainage pattern in the subglacial morphology and extensive layers of basal regelation ice and subglacial carbonate precipitate deposits found within the Lken Moraines sediments. These subglacial carbonates, including ooid layers, formed from the mixing of glacial meltwater and seawater at 72 ka BP. The combined evidence indicates that the ocean discharge of subglacial meltwater may be variable and/or is periodically blocked by basal freezing events near the ice sheet terminus. |
format |
Article in Journal/Newspaper |
author |
Goodwin, ID Roberts, JL Etheridge, DM Hellstrom, J Moy, AD Ribo, M Smith, AM |
author_facet |
Goodwin, ID Roberts, JL Etheridge, DM Hellstrom, J Moy, AD Ribo, M Smith, AM |
author_sort |
Goodwin, ID |
title |
Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
title_short |
Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
title_full |
Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
title_fullStr |
Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
title_full_unstemmed |
Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations |
title_sort |
modern to glacial age subglacial meltwater drainage at law dome, coastal east antarctica from topography, sediments and jokulhlaup observations |
publisher |
Geological Society Publishing House |
publishDate |
2017 |
url |
https://doi.org/10.1144/SP461.16 http://ecite.utas.edu.au/118721 |
long_lat |
ENVELOPE(112.833,112.833,-66.733,-66.733) |
geographic |
East Antarctica Law Dome |
geographic_facet |
East Antarctica Law Dome |
genre |
Antarc* Antarctica East Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet |
op_relation |
http://dx.doi.org/10.1144/SP461.16 Goodwin, ID and Roberts, JL and Etheridge, DM and Hellstrom, J and Moy, AD and Ribo, M and Smith, AM, Modern to glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jokulhlaup observations, Geological Society Special Publication, 461 Article SP461.16. ISSN 0305-8719 (2017) [Refereed Article] http://ecite.utas.edu.au/118721 |
op_doi |
https://doi.org/10.1144/SP461.16 |
container_title |
Geological Society, London, Special Publications |
container_volume |
461 |
container_issue |
1 |
container_start_page |
215 |
op_container_end_page |
230 |
_version_ |
1766250710810230784 |