Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic

Glacigenic debris-flows represent successive mass-flow deposits that build out a prograding wedge of sediment beyond the grounding zone of an ice sheet (e.g. Laberg & Vorren 1995; King et al. 1998). A prograding sedimentary depocentre extending from the outer shelf to the upper slope has been ob...

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Published in:Geological Society, London, Memoirs
Main Authors: Stewart, Heather A, Long, David
Other Authors: British Geological Survey
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of London 2016
Subjects:
Online Access:http://hdl.handle.net/1893/27900
https://doi.org/10.1144/m46.94
http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf
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spelling ftunivstirling:oai:dspace.stir.ac.uk:1893/27900 2023-05-15T16:40:14+02:00 Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic Stewart, Heather A Long, David British Geological Survey 2016-12-31 application/pdf http://hdl.handle.net/1893/27900 https://doi.org/10.1144/m46.94 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf en eng Geological Society of London Stewart HA & Long D (2016) Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic. Geological Society, London, Memoirs, 46 (1), pp. 361-362. https://doi.org/10.1144/m46.94 http://hdl.handle.net/1893/27900 doi:10.1144/m46.94 956283 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf Copyright 2016 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics http://creativecommons.org/licenses/by/3.0/ CC-BY Journal Article VoR - Version of Record 2016 ftunivstirling https://doi.org/10.1144/m46.94 2022-06-13T18:43:41Z Glacigenic debris-flows represent successive mass-flow deposits that build out a prograding wedge of sediment beyond the grounding zone of an ice sheet (e.g. Laberg & Vorren 1995; King et al. 1998). A prograding sedimentary depocentre extending from the outer shelf to the upper slope has been observed in geophysical datasets from the West Shetland margin of the Faroe–Shetland Channel, NW of the UK in the NE Atlantic. Overlapping, glacigenic debris-flows comprise the Rona and Foula wedges and provide insight into the extent and stability of the northern sector of the British Ice Sheet during the last full-glacial period (Stoker & Varming 2011). Article in Journal/Newspaper Ice Sheet University of Stirling: Stirling Digital Research Repository Laberg ENVELOPE(17.820,17.820,68.862,68.862) Rona ENVELOPE(13.943,13.943,66.985,66.985) Geological Society, London, Memoirs 46 1 361 362
institution Open Polar
collection University of Stirling: Stirling Digital Research Repository
op_collection_id ftunivstirling
language English
description Glacigenic debris-flows represent successive mass-flow deposits that build out a prograding wedge of sediment beyond the grounding zone of an ice sheet (e.g. Laberg & Vorren 1995; King et al. 1998). A prograding sedimentary depocentre extending from the outer shelf to the upper slope has been observed in geophysical datasets from the West Shetland margin of the Faroe–Shetland Channel, NW of the UK in the NE Atlantic. Overlapping, glacigenic debris-flows comprise the Rona and Foula wedges and provide insight into the extent and stability of the northern sector of the British Ice Sheet during the last full-glacial period (Stoker & Varming 2011).
author2 British Geological Survey
format Article in Journal/Newspaper
author Stewart, Heather A
Long, David
spellingShingle Stewart, Heather A
Long, David
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
author_facet Stewart, Heather A
Long, David
author_sort Stewart, Heather A
title Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
title_short Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
title_full Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
title_fullStr Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
title_full_unstemmed Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
title_sort glacigenic debris-flows observed in 3d seismic high-resolution seafloor imagery, faroe–shetland channel, ne atlantic
publisher Geological Society of London
publishDate 2016
url http://hdl.handle.net/1893/27900
https://doi.org/10.1144/m46.94
http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf
long_lat ENVELOPE(17.820,17.820,68.862,68.862)
ENVELOPE(13.943,13.943,66.985,66.985)
geographic Laberg
Rona
geographic_facet Laberg
Rona
genre Ice Sheet
genre_facet Ice Sheet
op_relation Stewart HA & Long D (2016) Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic. Geological Society, London, Memoirs, 46 (1), pp. 361-362. https://doi.org/10.1144/m46.94
http://hdl.handle.net/1893/27900
doi:10.1144/m46.94
956283
http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf
op_rights Copyright 2016 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics
http://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1144/m46.94
container_title Geological Society, London, Memoirs
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container_start_page 361
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