(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ...
High-resolution geophysical and sediment core data are used to investigate the pattern and dynamics of former ice flow in Kvitøya Trough, northwestern Barents Sea. A new swath-bathymetric dataset identifies three types of submarine landform in the study area (streamlined landforms, meltwater channel...
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ftdatacite:10.1594/pangaea.811288 2024-09-15T17:57:58+00:00 (Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... Hogan, Kelly A Dowdeswell, Julian A Noormets, R Evans, Jeffrey Ó Cofaigh, Colm Jakobsson, Martin 2010 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.811288 https://doi.pangaea.de/10.1594/PANGAEA.811288 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2010.08.015 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Core DEPTH, sediment/rock Age, dated material Age, dated Age, dated standard deviation Gravity corer Age, 14C AMS JR20060728 James Clark Ross International Polar Year 2007-2008 IPY dataset Supplementary Dataset Dataset 2010 ftdatacite https://doi.org/10.1594/pangaea.81128810.1016/j.quascirev.2010.08.015 2024-08-01T10:57:41Z High-resolution geophysical and sediment core data are used to investigate the pattern and dynamics of former ice flow in Kvitøya Trough, northwestern Barents Sea. A new swath-bathymetric dataset identifies three types of submarine landform in the study area (streamlined landforms, meltwater channels and cavities, iceberg scours). Subglacially produced streamlined landforms provide a record of ice flow through Kvitøya Trough during the last glaciation. Flow directions are inferred from the orientations of streamlined landforms (drumlins, crag-and-tail features). Ice flowed northward for at least 135 km from an ice divide at the southern end of Kvitøya Trough. A large channel-cavity system incised into bedrock in the southern trough indicates that subglacial meltwater was present at the former ice-sheet base. Modest landform elongation ratios and a lack of mega-scale glacial lineations suggest that, although ice in Kvitøya Trough was melting at the bed and flowed faster than the likely thin and cold-based ice ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Dataset Barents Sea Ice Sheet International Polar Year IPY Kvitøya DataCite |
institution |
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collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Core DEPTH, sediment/rock Age, dated material Age, dated Age, dated standard deviation Gravity corer Age, 14C AMS JR20060728 James Clark Ross International Polar Year 2007-2008 IPY |
spellingShingle |
Event label Latitude of event Longitude of event Core DEPTH, sediment/rock Age, dated material Age, dated Age, dated standard deviation Gravity corer Age, 14C AMS JR20060728 James Clark Ross International Polar Year 2007-2008 IPY Hogan, Kelly A Dowdeswell, Julian A Noormets, R Evans, Jeffrey Ó Cofaigh, Colm Jakobsson, Martin (Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
topic_facet |
Event label Latitude of event Longitude of event Core DEPTH, sediment/rock Age, dated material Age, dated Age, dated standard deviation Gravity corer Age, 14C AMS JR20060728 James Clark Ross International Polar Year 2007-2008 IPY |
description |
High-resolution geophysical and sediment core data are used to investigate the pattern and dynamics of former ice flow in Kvitøya Trough, northwestern Barents Sea. A new swath-bathymetric dataset identifies three types of submarine landform in the study area (streamlined landforms, meltwater channels and cavities, iceberg scours). Subglacially produced streamlined landforms provide a record of ice flow through Kvitøya Trough during the last glaciation. Flow directions are inferred from the orientations of streamlined landforms (drumlins, crag-and-tail features). Ice flowed northward for at least 135 km from an ice divide at the southern end of Kvitøya Trough. A large channel-cavity system incised into bedrock in the southern trough indicates that subglacial meltwater was present at the former ice-sheet base. Modest landform elongation ratios and a lack of mega-scale glacial lineations suggest that, although ice in Kvitøya Trough was melting at the bed and flowed faster than the likely thin and cold-based ice ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... |
format |
Dataset |
author |
Hogan, Kelly A Dowdeswell, Julian A Noormets, R Evans, Jeffrey Ó Cofaigh, Colm Jakobsson, Martin |
author_facet |
Hogan, Kelly A Dowdeswell, Julian A Noormets, R Evans, Jeffrey Ó Cofaigh, Colm Jakobsson, Martin |
author_sort |
Hogan, Kelly A |
title |
(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
title_short |
(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
title_full |
(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
title_fullStr |
(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
title_full_unstemmed |
(Table 2) AMS radiocarbon dates from sediment cores obtained during James Clark Ross cruise JR142, Kvitøya Trough ... |
title_sort |
(table 2) ams radiocarbon dates from sediment cores obtained during james clark ross cruise jr142, kvitøya trough ... |
publisher |
PANGAEA |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.811288 https://doi.pangaea.de/10.1594/PANGAEA.811288 |
genre |
Barents Sea Ice Sheet International Polar Year IPY Kvitøya |
genre_facet |
Barents Sea Ice Sheet International Polar Year IPY Kvitøya |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2010.08.015 |
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.81128810.1016/j.quascirev.2010.08.015 |
_version_ |
1810434178883256320 |