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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ftloughboroughun:oai:figshare.com:article/9482345 2023-05-15T15:14:25+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 Julian A. Dowdeswell K.A. Hogan Colm O Cofaigh E.M.G. Fugelli Jeffrey Evans R. Noormets 2014-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/Late_Quaternary_ice_flow_in_a_West_Greenland_fjord_and_cross-shelf_trough_system_submarine_landforms_from_Rink_Isbrae_to_Uummannaq_shelf_and_slope/9482345 unknown 2134/17834 https://figshare.com/articles/journal_contribution/Late_Quaternary_ice_flow_in_a_West_Greenland_fjord_and_cross-shelf_trough_system_submarine_landforms_from_Rink_Isbrae_to_Uummannaq_shelf_and_slope/9482345 CC BY 3.0 CC-BY Earth Sciences not elsewhere classified Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland Text Journal contribution 2014 ftloughboroughun 2022-01-01T20:21:22Z 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 400km-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, 300km to the south. Ice retreat had begun by 14.8cal.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. © 2013 The Authors. Other Non-Article Part of Journal/Newspaper Arctic Greenland Ice Sheet Iceberg* Rink Isbrae Uummannaq Loughborough University: Figshare 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) |
institution |
Open Polar |
collection |
Loughborough University: Figshare |
op_collection_id |
ftloughboroughun |
language |
unknown |
topic |
Earth Sciences not elsewhere classified Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland |
spellingShingle |
Earth Sciences not elsewhere classified Arctic Ice flow Ice stream Late Quaternary Submarine landforms Trough-mouth fan West Greenland Julian A. Dowdeswell K.A. Hogan Colm O Cofaigh E.M.G. Fugelli Jeffrey Evans R. Noormets 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 |
Earth Sciences not elsewhere classified 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 400km-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, 300km to the south. Ice retreat had begun by 14.8cal.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. © 2013 The Authors. |
format |
Other Non-Article Part of Journal/Newspaper |
author |
Julian A. Dowdeswell K.A. Hogan Colm O Cofaigh E.M.G. Fugelli Jeffrey Evans R. Noormets |
author_facet |
Julian A. Dowdeswell K.A. Hogan Colm O Cofaigh E.M.G. Fugelli Jeffrey Evans R. Noormets |
author_sort |
Julian A. Dowdeswell |
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 |
publishDate |
2014 |
url |
https://figshare.com/articles/journal_contribution/Late_Quaternary_ice_flow_in_a_West_Greenland_fjord_and_cross-shelf_trough_system_submarine_landforms_from_Rink_Isbrae_to_Uummannaq_shelf_and_slope/9482345 |
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_relation |
2134/17834 https://figshare.com/articles/journal_contribution/Late_Quaternary_ice_flow_in_a_West_Greenland_fjord_and_cross-shelf_trough_system_submarine_landforms_from_Rink_Isbrae_to_Uummannaq_shelf_and_slope/9482345 |
op_rights |
CC BY 3.0 |
op_rightsnorm |
CC-BY |
_version_ |
1766344868939956224 |