Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation
The Laurentide Ice Sheet was characterized by a dynamic polythermal base. However, important data and knowledge gaps have led to contrasting reconstructions in areas such as the Labrador Ice Divide. In this study, detailed fieldwork was conducted at the southeastern edge of a major landform boundary...
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Online Access: | http://hdl.handle.net/10197/11094 https://doi.org/10.1002/jqs.3138 |
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ftunivcolldublin:oai:researchrepository.ucd.ie:10197/11094 2023-05-15T16:40:29+02:00 Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation Rice, Jessey M. Ross, Martin Paulen, Roger C. Kelley, Samuel E. 2019-10-01T12:21:07Z http://hdl.handle.net/10197/11094 https://doi.org/10.1002/jqs.3138 en eng Wiley Journal of Quaternary Science 0267-8179 http://hdl.handle.net/10197/11094 34 7 519 535 doi:10.1002/jqs.3138 This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. CC-BY Deglaciation Ice flow chronology Laurentide Ice Sheet (LIS) Quebec-Labrador Dome Journal Article 2019 ftunivcolldublin https://doi.org/10.1002/jqs.3138 2022-04-08T14:19:36Z The Laurentide Ice Sheet was characterized by a dynamic polythermal base. However, important data and knowledge gaps have led to contrasting reconstructions in areas such as the Labrador Ice Divide. In this study, detailed fieldwork was conducted at the southeastern edge of a major landform boundary to resolve the relative ice flow chronology and constrain the evolution of the subglacial dynamics, including the migration and collapse of the Labrador Ice Divide. Surficial mapping and analysis of 94 outcrop‐scale ice flow indicators were used to develop a relative ice flow chronology. 10Be exposure ages were used with optical ages to confine the timing of deglaciation within the study area. Four phases of ice flow were identified. Flow 1 was a northeasterly ice flow preserved under non‐erosive subglacial conditions associated with the development of an ice divide. Flow 2 was a northwest ice flow, which we correlate to the Ungava Bay Ice Stream and led to a westward migration of the ice divide, preserving Flow 2 features and resulting in Flow 3's eastward‐trending indicators. Flow 4 is limited to sparse fine striations within and around the regional uplands. The new optical ages and 10Be exposure ages add to the regional geochronology dataset, which further constrains the timing of ice margin retreat in the area to around 8.0 ka. Geological Survey of Canada's Geo‐Mapping for Energy and Minerals II (GEM2) Program (2013–2020) Polar Continental Support Program under the Core Zone Surficial Activity (Hudson–Ungava Project) Northern Scientific Training Program (NSTP) Ontario Graduate Scholarship (OGS) fund Natural Science and Engineering Research Council (NSERC) of Canada Discovery Grant NSERC Research Tools and Instruments Grant Peer-review status unspecified Update citation details during checkdate report - AC Article in Journal/Newspaper Ice Sheet Ungava Bay University College Dublin: Research Repository UCD Canada Hudson Ungava Bay ENVELOPE(-67.489,-67.489,59.498,59.498) Journal of Quaternary Science 34 7 519 535 |
institution |
Open Polar |
collection |
University College Dublin: Research Repository UCD |
op_collection_id |
ftunivcolldublin |
language |
English |
topic |
Deglaciation Ice flow chronology Laurentide Ice Sheet (LIS) Quebec-Labrador Dome |
spellingShingle |
Deglaciation Ice flow chronology Laurentide Ice Sheet (LIS) Quebec-Labrador Dome Rice, Jessey M. Ross, Martin Paulen, Roger C. Kelley, Samuel E. Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
topic_facet |
Deglaciation Ice flow chronology Laurentide Ice Sheet (LIS) Quebec-Labrador Dome |
description |
The Laurentide Ice Sheet was characterized by a dynamic polythermal base. However, important data and knowledge gaps have led to contrasting reconstructions in areas such as the Labrador Ice Divide. In this study, detailed fieldwork was conducted at the southeastern edge of a major landform boundary to resolve the relative ice flow chronology and constrain the evolution of the subglacial dynamics, including the migration and collapse of the Labrador Ice Divide. Surficial mapping and analysis of 94 outcrop‐scale ice flow indicators were used to develop a relative ice flow chronology. 10Be exposure ages were used with optical ages to confine the timing of deglaciation within the study area. Four phases of ice flow were identified. Flow 1 was a northeasterly ice flow preserved under non‐erosive subglacial conditions associated with the development of an ice divide. Flow 2 was a northwest ice flow, which we correlate to the Ungava Bay Ice Stream and led to a westward migration of the ice divide, preserving Flow 2 features and resulting in Flow 3's eastward‐trending indicators. Flow 4 is limited to sparse fine striations within and around the regional uplands. The new optical ages and 10Be exposure ages add to the regional geochronology dataset, which further constrains the timing of ice margin retreat in the area to around 8.0 ka. Geological Survey of Canada's Geo‐Mapping for Energy and Minerals II (GEM2) Program (2013–2020) Polar Continental Support Program under the Core Zone Surficial Activity (Hudson–Ungava Project) Northern Scientific Training Program (NSTP) Ontario Graduate Scholarship (OGS) fund Natural Science and Engineering Research Council (NSERC) of Canada Discovery Grant NSERC Research Tools and Instruments Grant Peer-review status unspecified Update citation details during checkdate report - AC |
format |
Article in Journal/Newspaper |
author |
Rice, Jessey M. Ross, Martin Paulen, Roger C. Kelley, Samuel E. |
author_facet |
Rice, Jessey M. Ross, Martin Paulen, Roger C. Kelley, Samuel E. |
author_sort |
Rice, Jessey M. |
title |
Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
title_short |
Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
title_full |
Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
title_fullStr |
Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
title_full_unstemmed |
Refining the ice flow chronology and subglacial dynamics across the migrating Labrador Divide of the Laurentide Ice Sheet with age constraints on deglaciation |
title_sort |
refining the ice flow chronology and subglacial dynamics across the migrating labrador divide of the laurentide ice sheet with age constraints on deglaciation |
publisher |
Wiley |
publishDate |
2019 |
url |
http://hdl.handle.net/10197/11094 https://doi.org/10.1002/jqs.3138 |
long_lat |
ENVELOPE(-67.489,-67.489,59.498,59.498) |
geographic |
Canada Hudson Ungava Bay |
geographic_facet |
Canada Hudson Ungava Bay |
genre |
Ice Sheet Ungava Bay |
genre_facet |
Ice Sheet Ungava Bay |
op_relation |
Journal of Quaternary Science 0267-8179 http://hdl.handle.net/10197/11094 34 7 519 535 doi:10.1002/jqs.3138 |
op_rights |
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1002/jqs.3138 |
container_title |
Journal of Quaternary Science |
container_volume |
34 |
container_issue |
7 |
container_start_page |
519 |
op_container_end_page |
535 |
_version_ |
1766030878451957760 |