Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea

Bibliographic Details
Title: Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea
Authors: B. Bellwald, S. Planke, S. Polteau, N. Lebedeva-Ivanova, J.I. Faleide, S.M. Morris, S. Morse, S. Castelltort
Source: Journal of Glaciology, Vol 67, Pp 404-420 (2021)
Publisher Information: Cambridge University Press, 2021.
Publication Year: 2021
Collection: LCC:Environmental sciences
LCC:Meteorology. Climatology
Subject Terms: Arctic glaciology, climate change, fluvial transport, glacier hydrology, Jökulhlaups (GLOFs), Environmental sciences, GE1-350, Meteorology. Climatology, QC851-999
More Details: Proglacial braided river systems discharge large volumes of meltwater from ice sheets and transport coarse-grained sediments from the glaciated areas to the oceans. Here, we test the hypothesis if high-energy hydrological events can leave distinctive signatures in the sedimentary record of braided river systems. We characterize the morphology and infer a mode of formation of a 25 km long and 1–3 km wide Early Pleistocene incised valley recently imaged in 3-D seismic data in the Hoop area, SW Barents Sea. The fluvial system, named Bjørnelva River Valley, carved 20 m deep channels into Lower Cretaceous bedrock at a glacial paleo-surface and deposited 28 channel bars along a paleo-slope gradient of ~0.64 m km−1. The landform morphologies and position relative to the paleo-surface support that Bjørnelva River Valley was formed in the proglacial domain of the Barents Sea Ice Sheet. Based on valley width and valley depth, we suggest that Bjørnelva River Valley represents a braided river system fed by violent outburst floods from a glacial lake, with estimated outburst discharges of ~160 000 m3 s−1. The morphological configuration of Bjørnelva River Valley can inform geohazard assessments in areas at risk of outburst flooding today and is an analogue for landscapes evolving in areas currently covered by the Greenland and Antarctic ice sheets.
Document Type: article
File Description: electronic resource
Language: English
ISSN: 0022-1430
1727-5652
Relation: https://www.cambridge.org/core/product/identifier/S002214302000115X/type/journal_article; https://doaj.org/toc/0022-1430; https://doaj.org/toc/1727-5652
DOI: 10.1017/jog.2020.115
Access URL: https://doaj.org/article/a70cb099c1224eb396559458aa93bba6
Accession Number: edsdoj.70cb099c1224eb396559458aa93bba6
Database: Directory of Open Access Journals
More Details
ISSN:00221430
17275652
DOI:10.1017/jog.2020.115
Published in:Journal of Glaciology
Language:English