Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope.
Sea-floor landforms and acoustic-stratigraphic records allow interpretation of the past form and flow of a westward-draining ice stream of the Greenland Ice Sheet, Rink Isbrae. The Late Pliocene–Pleistocene glacial package is several hundred metres thick and down-laps onto an upper Miocene horizon....
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2014
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Online Access: | http://dro.dur.ac.uk/14004/ http://dro.dur.ac.uk/14004/1/14004.pdf https://doi.org/10.1016/j.quascirev.2013.09.007 |
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ftunivdurham:oai:dro.dur.ac.uk.OAI2:14004 2023-05-15T15:16:21+02:00 Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. Dowdeswell, J.A. Hogan, K.A. Ó Cofaigh, C. Fugelli, E.M.G. Evans, J. Noormets, R. 2014-05-15 application/pdf http://dro.dur.ac.uk/14004/ http://dro.dur.ac.uk/14004/1/14004.pdf https://doi.org/10.1016/j.quascirev.2013.09.007 unknown Elsevier dro:14004 issn:0277-3791 doi:10.1016/j.quascirev.2013.09.007 http://dro.dur.ac.uk/14004/ http://dx.doi.org/10.1016/j.quascirev.2013.09.007 http://dro.dur.ac.uk/14004/1/14004.pdf © 2013 The Authors. Published by Elsevier Ltd. Open access under CC BY license. CC-BY Quaternary science reviews, 2014, Vol.92, pp.292-309 [Peer Reviewed Journal] Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland Article PeerReviewed 2014 ftunivdurham https://doi.org/10.1016/j.quascirev.2013.09.007 2020-05-28T22:31:40Z Sea-floor landforms and acoustic-stratigraphic records allow interpretation of the past form and flow of a westward-draining ice stream of the Greenland Ice Sheet, Rink Isbrae. The Late Pliocene–Pleistocene glacial package is several hundred metres thick and down-laps onto an upper Miocene horizon. Several acoustic facies are mapped from sub-bottom profiler records of the 400 km-long Uummannaq fjord-shelf-slope system. An acoustically stratified facies covers much of the fjord and trough floor, interpreted as glacimarine sediment from rain-out of fine-grained debris in turbid meltwater. Beneath this facies is a semi-transparent deformation-till unit, which includes buried streamlined landforms. Landform distribution in the Uummannaq system is used to reconstruct past ice extent and flow directions. The presence of streamlined landforms (mega-scale glacial lineations, drumlins, crag-and-tails) shows that an ice stream advanced through the fjord system to fill Uummannaq Trough, reaching the shelf edge at the Last Glacial Maximum. Beyond the trough there is a major fan built mainly of glacigenic debris flows. Turbidity-current channels were not observed on Uummannaq Fan, contrasting with well-developed channels on Disko Fan, 300 km to the south. Ice retreat had begun by 14.8 cal. ka ago. Grounding-zone wedges (GZW) in Uummannaq Trough imply that retreat was episodic, punctuated by several still-stands. Ice retreat between GZWs may have been relatively rapid. There is little sedimentary evidence for still-stands in the inner fjords, except for a major moraine ridge marking a Little Ice Age maximum position. On the shallow banks either side of Uummannaq Trough, iceberg ploughing has reworked any morphological evidence of earlier ice-sheet activity. Article in Journal/Newspaper Arctic Greenland Ice Sheet Iceberg* Rink Isbrae Uummannaq Durham University: Durham Research Online Arctic Greenland Moraine Ridge ENVELOPE(168.050,168.050,-72.300,-72.300) South Ice ENVELOPE(-29.867,-29.867,-81.950,-81.950) Uummannaq Fjord ENVELOPE(-52.968,-52.968,70.925,70.925) Quaternary Science Reviews 92 292 309 |
institution |
Open Polar |
collection |
Durham University: Durham Research Online |
op_collection_id |
ftunivdurham |
language |
unknown |
topic |
Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland |
spellingShingle |
Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland Dowdeswell, J.A. Hogan, K.A. Ó Cofaigh, C. Fugelli, E.M.G. Evans, J. Noormets, R. Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
topic_facet |
Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland |
description |
Sea-floor landforms and acoustic-stratigraphic records allow interpretation of the past form and flow of a westward-draining ice stream of the Greenland Ice Sheet, Rink Isbrae. The Late Pliocene–Pleistocene glacial package is several hundred metres thick and down-laps onto an upper Miocene horizon. Several acoustic facies are mapped from sub-bottom profiler records of the 400 km-long Uummannaq fjord-shelf-slope system. An acoustically stratified facies covers much of the fjord and trough floor, interpreted as glacimarine sediment from rain-out of fine-grained debris in turbid meltwater. Beneath this facies is a semi-transparent deformation-till unit, which includes buried streamlined landforms. Landform distribution in the Uummannaq system is used to reconstruct past ice extent and flow directions. The presence of streamlined landforms (mega-scale glacial lineations, drumlins, crag-and-tails) shows that an ice stream advanced through the fjord system to fill Uummannaq Trough, reaching the shelf edge at the Last Glacial Maximum. Beyond the trough there is a major fan built mainly of glacigenic debris flows. Turbidity-current channels were not observed on Uummannaq Fan, contrasting with well-developed channels on Disko Fan, 300 km to the south. Ice retreat had begun by 14.8 cal. ka ago. Grounding-zone wedges (GZW) in Uummannaq Trough imply that retreat was episodic, punctuated by several still-stands. Ice retreat between GZWs may have been relatively rapid. There is little sedimentary evidence for still-stands in the inner fjords, except for a major moraine ridge marking a Little Ice Age maximum position. On the shallow banks either side of Uummannaq Trough, iceberg ploughing has reworked any morphological evidence of earlier ice-sheet activity. |
format |
Article in Journal/Newspaper |
author |
Dowdeswell, J.A. Hogan, K.A. Ó Cofaigh, C. Fugelli, E.M.G. Evans, J. Noormets, R. |
author_facet |
Dowdeswell, J.A. Hogan, K.A. Ó Cofaigh, C. Fugelli, E.M.G. Evans, J. Noormets, R. |
author_sort |
Dowdeswell, J.A. |
title |
Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
title_short |
Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
title_full |
Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
title_fullStr |
Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
title_full_unstemmed |
Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system : submarine landforms from Rink Isbrae to Uummannaq shelf and slope. |
title_sort |
late quaternary ice flow in a west greenland fjord and cross-shelf trough system : submarine landforms from rink isbrae to uummannaq shelf and slope. |
publisher |
Elsevier |
publishDate |
2014 |
url |
http://dro.dur.ac.uk/14004/ http://dro.dur.ac.uk/14004/1/14004.pdf https://doi.org/10.1016/j.quascirev.2013.09.007 |
long_lat |
ENVELOPE(168.050,168.050,-72.300,-72.300) ENVELOPE(-29.867,-29.867,-81.950,-81.950) ENVELOPE(-52.968,-52.968,70.925,70.925) |
geographic |
Arctic Greenland Moraine Ridge South Ice Uummannaq Fjord |
geographic_facet |
Arctic Greenland Moraine Ridge South Ice Uummannaq Fjord |
genre |
Arctic Greenland Ice Sheet Iceberg* Rink Isbrae Uummannaq |
genre_facet |
Arctic Greenland Ice Sheet Iceberg* Rink Isbrae Uummannaq |
op_source |
Quaternary science reviews, 2014, Vol.92, pp.292-309 [Peer Reviewed Journal] |
op_relation |
dro:14004 issn:0277-3791 doi:10.1016/j.quascirev.2013.09.007 http://dro.dur.ac.uk/14004/ http://dx.doi.org/10.1016/j.quascirev.2013.09.007 http://dro.dur.ac.uk/14004/1/14004.pdf |
op_rights |
© 2013 The Authors. Published by Elsevier Ltd. Open access under CC BY license. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.quascirev.2013.09.007 |
container_title |
Quaternary Science Reviews |
container_volume |
92 |
container_start_page |
292 |
op_container_end_page |
309 |
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1766346640726163456 |