Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project
Holocene and slightly pre-Holocene submarine landslide are found both in high-latitude glacial-dominated margins and in lower latitude, river-dominated margins. This paper constitutes a major assessment on some of the best-studied submarine instabilities in the world. We review and update from origi...
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ftunivgent:oai:archive.ugent.be:298430 2023-10-01T03:51:56+02:00 Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project Canals, M Lastras, G Urgeles, R Casamor, JL Mienert, J Cattaneo, A De Batist, Marc Haflidason, H Imbo, Yannick Laberg, JS Locat, J Long, D Longva, O Masson, DG Sultan, N Trincardi, F Bryn, P 2004 https://biblio.ugent.be/publication/298430 http://hdl.handle.net/1854/LU-298430 eng eng Elsevier Science https://biblio.ugent.be/publication/298430 http://hdl.handle.net/1854/LU-298430 MARINE GEOLOGY ISSN: 0025-3227 Earth and Environmental Sciences COSTA project BIG’95 Slide mid-Norwegian margin journalArticle info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2004 ftunivgent 2023-09-06T22:32:32Z Holocene and slightly pre-Holocene submarine landslide are found both in high-latitude glacial-dominated margins and in lower latitude, river-dominated margins. This paper constitutes a major assessment on some of the best-studied submarine instabilities in the world. We review and update from original data and literature reports the current state of knowledge of Storegga, Traenadjupet and Finneidfjord slides from the mid-Norwegian margin, Afen Slide from the Faeroe-Shetland Channel, BIG’95 Slide and Central Adriatic Deformation Belt (CADEB) from continental slope and inner continental shelf settings off the Ebro and Po rivers in the Mediterranean Sea, Canary Slide west of the westernmost, youngest Canary Islands and Gebra Slide off the northern tip of the Antarctic Peninsula in the southern hemisphere, i.e. those studied in the Continental Slope Stability (COSTA) project. The investigated slides range in size from the gigantic 90,000 km2 and almost 3000 km3 Storegga Slide to the tiny 1 km2 and 0.001 km3 Finneidfjord Slide. Not only do individual submarine landslides rarely involve processes precisely fitting with pre-established categories, mostly based on subaerial research, but also they display complex mechanical behaviors within the elastic and plastic fields. Individual events can involve simultaneous or successive vertical to translational movements including block detachment, block gliding, debris flow, mud flow and turbidity currents. The need for an in-depth revision of the classification criteria, and eventually for a new classification system, based on the new imaging capabilities provided by modern techniques, is more than obvious. We suggest a new system, which, for the moment, is restricted to debris flows and debris avalanches. Volume calculation methods are critically reviewed and the relations between some key geomorphic parameters are established for the selected slides. The assumed volume missing from scar areas does not necessarily match the actual volume of sediment remobilised by an ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ghent University Academic Bibliography Antarctic The Antarctic Antarctic Peninsula Storegga ENVELOPE(18.251,18.251,68.645,68.645) Finneidfjord ENVELOPE(13.801,13.801,66.180,66.180) |
institution |
Open Polar |
collection |
Ghent University Academic Bibliography |
op_collection_id |
ftunivgent |
language |
English |
topic |
Earth and Environmental Sciences COSTA project BIG’95 Slide mid-Norwegian margin |
spellingShingle |
Earth and Environmental Sciences COSTA project BIG’95 Slide mid-Norwegian margin Canals, M Lastras, G Urgeles, R Casamor, JL Mienert, J Cattaneo, A De Batist, Marc Haflidason, H Imbo, Yannick Laberg, JS Locat, J Long, D Longva, O Masson, DG Sultan, N Trincardi, F Bryn, P Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
topic_facet |
Earth and Environmental Sciences COSTA project BIG’95 Slide mid-Norwegian margin |
description |
Holocene and slightly pre-Holocene submarine landslide are found both in high-latitude glacial-dominated margins and in lower latitude, river-dominated margins. This paper constitutes a major assessment on some of the best-studied submarine instabilities in the world. We review and update from original data and literature reports the current state of knowledge of Storegga, Traenadjupet and Finneidfjord slides from the mid-Norwegian margin, Afen Slide from the Faeroe-Shetland Channel, BIG’95 Slide and Central Adriatic Deformation Belt (CADEB) from continental slope and inner continental shelf settings off the Ebro and Po rivers in the Mediterranean Sea, Canary Slide west of the westernmost, youngest Canary Islands and Gebra Slide off the northern tip of the Antarctic Peninsula in the southern hemisphere, i.e. those studied in the Continental Slope Stability (COSTA) project. The investigated slides range in size from the gigantic 90,000 km2 and almost 3000 km3 Storegga Slide to the tiny 1 km2 and 0.001 km3 Finneidfjord Slide. Not only do individual submarine landslides rarely involve processes precisely fitting with pre-established categories, mostly based on subaerial research, but also they display complex mechanical behaviors within the elastic and plastic fields. Individual events can involve simultaneous or successive vertical to translational movements including block detachment, block gliding, debris flow, mud flow and turbidity currents. The need for an in-depth revision of the classification criteria, and eventually for a new classification system, based on the new imaging capabilities provided by modern techniques, is more than obvious. We suggest a new system, which, for the moment, is restricted to debris flows and debris avalanches. Volume calculation methods are critically reviewed and the relations between some key geomorphic parameters are established for the selected slides. The assumed volume missing from scar areas does not necessarily match the actual volume of sediment remobilised by an ... |
format |
Article in Journal/Newspaper |
author |
Canals, M Lastras, G Urgeles, R Casamor, JL Mienert, J Cattaneo, A De Batist, Marc Haflidason, H Imbo, Yannick Laberg, JS Locat, J Long, D Longva, O Masson, DG Sultan, N Trincardi, F Bryn, P |
author_facet |
Canals, M Lastras, G Urgeles, R Casamor, JL Mienert, J Cattaneo, A De Batist, Marc Haflidason, H Imbo, Yannick Laberg, JS Locat, J Long, D Longva, O Masson, DG Sultan, N Trincardi, F Bryn, P |
author_sort |
Canals, M |
title |
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
title_short |
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
title_full |
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
title_fullStr |
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
title_full_unstemmed |
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project |
title_sort |
slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the costa project |
publisher |
Elsevier Science |
publishDate |
2004 |
url |
https://biblio.ugent.be/publication/298430 http://hdl.handle.net/1854/LU-298430 |
long_lat |
ENVELOPE(18.251,18.251,68.645,68.645) ENVELOPE(13.801,13.801,66.180,66.180) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Storegga Finneidfjord |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Storegga Finneidfjord |
genre |
Antarc* Antarctic Antarctic Peninsula |
genre_facet |
Antarc* Antarctic Antarctic Peninsula |
op_source |
MARINE GEOLOGY ISSN: 0025-3227 |
op_relation |
https://biblio.ugent.be/publication/298430 http://hdl.handle.net/1854/LU-298430 |
_version_ |
1778517305113706496 |