Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea
Proglacial braided river systems discharge large volumes of meltwater from ice sheets and trans-port coarse-grained sediments from the glaciated areas to the oceans. Here, we test the hypothesisif high-energy hydrological events can leave distinctive signatures in the sedimentary record ofbraided ri...
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ftunivgeneve:oai:unige.ch:unige:152392 2023-05-15T13:51:22+02:00 Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea Bellwald, B. Planke, S. Polteau, S. Lebedeva-Ivanova, N. Faleide, J.I. Morris, S.M. Morse, S. Castelltort, Sébastien 2021 https://archive-ouverte.unige.ch/unige:152392 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2020.115 unige:152392 https://archive-ouverte.unige.ch/unige:152392 info:eu-repo/semantics/openAccess ISSN: 0022-1430 Journal of Glaciology, Vol. 67, No 263 (2021) pp. 404-420 info:eu-repo/classification/ddc/550 Text info:eu-repo/semantics/article Article scientifique info:eu-repo/semantics/publishedVersion 2021 ftunivgeneve https://doi.org/10.1017/jog.2020.115 2022-02-08T22:31:09Z Proglacial braided river systems discharge large volumes of meltwater from ice sheets and trans-port coarse-grained sediments from the glaciated areas to the oceans. Here, we test the hypothesisif high-energy hydrological events can leave distinctive signatures in the sedimentary record ofbraided river systems. We characterize the morphology and infer a mode of formation of a25 km long and 1–3 km wide Early Pleistocene incised valley recently imaged in 3-D seismicdata in the Hoop area, SW Barents Sea. The fluvial system, named Bjørnelva River Valley, carved20 m deep channels into Lower Cretaceous bedrock at a glacial paleo-surface and deposited28 channel bars along a paleo-slope gradient of∼0.64 m km−1. The landform morphologiesand position relative to the paleo-surface support that Bjørnelva River Valley was formed inthe proglacial domain of the Barents Sea Ice Sheet. Based on valley width and valley depth, wesuggest that Bjørnelva River Valley represents a braided river system fed by violent outburstfloods from a glacial lake, with estimated outburst discharges of∼160 000 m3s−1. The morpho-logical configuration of Bjørnelva River Valley can inform geohazard assessments in areas at riskof outburst flooding today and is an analogue for landscapes evolving in areas currently coveredby the Greenland and Antarctic ice sheets. Article in Journal/Newspaper Antarc* Antarctic Barents Sea Greenland Ice Sheet Journal of Glaciology Sea ice Université de Genève: Archive ouverte UNIGE Antarctic Barents Sea Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Greenland Journal of Glaciology 67 263 404 420 |
institution |
Open Polar |
collection |
Université de Genève: Archive ouverte UNIGE |
op_collection_id |
ftunivgeneve |
language |
English |
topic |
info:eu-repo/classification/ddc/550 |
spellingShingle |
info:eu-repo/classification/ddc/550 Bellwald, B. Planke, S. Polteau, S. Lebedeva-Ivanova, N. Faleide, J.I. Morris, S.M. Morse, S. Castelltort, Sébastien Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
topic_facet |
info:eu-repo/classification/ddc/550 |
description |
Proglacial braided river systems discharge large volumes of meltwater from ice sheets and trans-port coarse-grained sediments from the glaciated areas to the oceans. Here, we test the hypothesisif high-energy hydrological events can leave distinctive signatures in the sedimentary record ofbraided river systems. We characterize the morphology and infer a mode of formation of a25 km long and 1–3 km wide Early Pleistocene incised valley recently imaged in 3-D seismicdata in the Hoop area, SW Barents Sea. The fluvial system, named Bjørnelva River Valley, carved20 m deep channels into Lower Cretaceous bedrock at a glacial paleo-surface and deposited28 channel bars along a paleo-slope gradient of∼0.64 m km−1. The landform morphologiesand position relative to the paleo-surface support that Bjørnelva River Valley was formed inthe proglacial domain of the Barents Sea Ice Sheet. Based on valley width and valley depth, wesuggest that Bjørnelva River Valley represents a braided river system fed by violent outburstfloods from a glacial lake, with estimated outburst discharges of∼160 000 m3s−1. The morpho-logical configuration of Bjørnelva River Valley can inform geohazard assessments in areas at riskof outburst flooding today and is an analogue for landscapes evolving in areas currently coveredby the Greenland and Antarctic ice sheets. |
format |
Article in Journal/Newspaper |
author |
Bellwald, B. Planke, S. Polteau, S. Lebedeva-Ivanova, N. Faleide, J.I. Morris, S.M. Morse, S. Castelltort, Sébastien |
author_facet |
Bellwald, B. Planke, S. Polteau, S. Lebedeva-Ivanova, N. Faleide, J.I. Morris, S.M. Morse, S. Castelltort, Sébastien |
author_sort |
Bellwald, B. |
title |
Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
title_short |
Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
title_full |
Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
title_fullStr |
Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
title_full_unstemmed |
Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea |
title_sort |
characterization of a glacial paleo-outburst flood using high-resolution 3-d seismic data: bjørnelva river valley, sw barents sea |
publishDate |
2021 |
url |
https://archive-ouverte.unige.ch/unige:152392 |
long_lat |
ENVELOPE(-129.463,-129.463,58.259,58.259) |
geographic |
Antarctic Barents Sea Glacial Lake Greenland |
geographic_facet |
Antarctic Barents Sea Glacial Lake Greenland |
genre |
Antarc* Antarctic Barents Sea Greenland Ice Sheet Journal of Glaciology Sea ice |
genre_facet |
Antarc* Antarctic Barents Sea Greenland Ice Sheet Journal of Glaciology Sea ice |
op_source |
ISSN: 0022-1430 Journal of Glaciology, Vol. 67, No 263 (2021) pp. 404-420 |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2020.115 unige:152392 https://archive-ouverte.unige.ch/unige:152392 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1017/jog.2020.115 |
container_title |
Journal of Glaciology |
container_volume |
67 |
container_issue |
263 |
container_start_page |
404 |
op_container_end_page |
420 |
_version_ |
1766255205954879488 |