The Euro-Mediterranean Submarine landSlide database (EMSS21)
The Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitiz...
Main Authors: | , , , , , |
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Other Authors: | , , , , , , |
Format: | Dataset |
Language: | English |
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DIGITAL.CSIC
2021
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Subjects: | |
Online Access: | http://hdl.handle.net/10261/247742 |
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ftcsic:oai:digital.csic.es:10261/247742 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Submarine landslide Geohazard Landslide scar Landslide deposit Trigger mechanism |
spellingShingle |
Submarine landslide Geohazard Landslide scar Landslide deposit Trigger mechanism Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda The Euro-Mediterranean Submarine landSlide database (EMSS21) |
topic_facet |
Submarine landslide Geohazard Landslide scar Landslide deposit Trigger mechanism |
description |
The Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only. Disclaimer: The EMSS21 is open to later additions and improvements. For these reasons and due to its intrinsic nature, the EMSS21 cannot be guaranteed to be complete, accurate and updated in any part, and will be subjected to successive revisions. Although the Institut de Ciències del Mar of CSIC makes every effort to supply the best available information, no warranty, expressed or implied, is provided as to the accuracy and reliability of all the data supplied in the EMSS21. Users are cautioned to consider carefully the nature of the data and information before using it for decisions that concern personal or public safety. Conclusions drawn from the EMSS21, or actions undertaken on the basis of its contents, are the sole responsibility of the user. The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as these events are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard. The EMSS21 displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only. Data compilation has been possible thanks to projects: Submarine landslides and Their impact on European continental margins (SLATE) - H2020-MSCA-ITN-2016-721403. ImagiNg large SeismogenIc and tsunamiGenic structures of the Gulf of Cadiz with ultra-High resolution Technologies (INSIGHT). - CTM2015-70155-R. The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as theseevents are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard. Peer reviewed |
author2 |
European Commission Ministerio de Economía y Competitividad (España) Urgeles, Roger 0000-0001-9438-1753 Camerlenghi, Angelo 0000-0002-8128-9533 Rüther, Denise C. 0000-0002-3938-5708 de Pro Díaz, Yolanda 0000-0001-9807-3627 Urgeles, Roger urgeles@icm.csic.es Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda |
format |
Dataset |
author |
Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda |
author_facet |
Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda |
author_sort |
Urgeles, Roger |
title |
The Euro-Mediterranean Submarine landSlide database (EMSS21) |
title_short |
The Euro-Mediterranean Submarine landSlide database (EMSS21) |
title_full |
The Euro-Mediterranean Submarine landSlide database (EMSS21) |
title_fullStr |
The Euro-Mediterranean Submarine landSlide database (EMSS21) |
title_full_unstemmed |
The Euro-Mediterranean Submarine landSlide database (EMSS21) |
title_sort |
euro-mediterranean submarine landslide database (emss21) |
publisher |
DIGITAL.CSIC |
publishDate |
2021 |
url |
http://hdl.handle.net/10261/247742 |
op_coverage |
North: 84ºN, South: 30ºN, West: 33ºW, East: 43ºE start=Miocene; end=Present |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
info:eu-repo/grantAgreement/EC/H2020/721403 MINECO/ICTI2013-2016/CTM2015-70155-R Collico, S., Arroyo; M., Urgeles, R., Gràcia E:, De Vincenzi, M., Peréz, N. (2020): Probabilistic mapping of earthquake-induced submarine landslide susceptibility in the South-West Iberian margin. Marine Geology, 429: 106296. https://doi.org/10.1016/j.margeo.2020.106296 . http://hdl.handle.net/10261/219760 Urgeles, R., Camerlenghi, A. (2013): Submarine landslides of the Mediterranean Sea: trigger mechanisms, dynamics and frequency‐magnitude distribution, Journal of Geophysical Research Earth Surface, 118: 2600-2618. http://dx.doi.org/10.1002/2013JF002720 . http://hdl.handle.net/10261/92232 Sallarès, V., Gràcia, E., Urgeles, R. (2011): Active faulting and slope failure in the Iberian margins: towards offshore geohazard mitigation. In Briand, G. (Ed.) Marine geo-hazards in the Mediterranean, CIESM Workshop Monograph nº 42, pp. 101-112. http://hdl.handle.net/10261/57350 Camerlenghi, A., Urgeles, R., Fantoni, L. (2010): A Database on Submarine Landslides of the Mediterranean Sea. In Mosher, D.C., Moscardelli, L., Shipp, R.C., Chaytor, J.D., Baxter, C.D.P., Lee, H.J., Urgeles, R. (Eds.) Submarine Mass Movements and Their Consequences, Advances in Natural and Technological Hazards Research, 28, Spinger, Dordrecht (The Netherlands), pp. 491-501. http://dx.doi.org/10.1007/978-90-481-3071-9_41 . http://hdl.handle.net/10261/76715 https://ls3gp.icm.csic.es/?page_id=553 Sí Urgeles, Roger; Camerlenghi, Angelo; Rüther, Denise C.; Fantoni, L.; Brückner, Nils W.; de Pro Díaz, Yolanda; 2021; The Euro-Mediterranean Submarine landSlide database (EMSS21); DIGITAL.CSIC; DOI http://hdl.handle.net/10261/247742 |
op_rights |
openAccess http://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.margeo.2020.106296 https://doi.org/10.1002/2013JF002720 https://doi.org/10.1007/978-90-481-3071-9_41 |
_version_ |
1766349836901154816 |
spelling |
ftcsic:oai:digital.csic.es:10261/247742 2023-05-15T15:19:38+02:00 The Euro-Mediterranean Submarine landSlide database (EMSS21) Euro-Mediterranean submarine landslide database (EMSS21): online data Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda European Commission Ministerio de Economía y Competitividad (España) Urgeles, Roger 0000-0001-9438-1753 Camerlenghi, Angelo 0000-0002-8128-9533 Rüther, Denise C. 0000-0002-3938-5708 de Pro Díaz, Yolanda 0000-0001-9807-3627 Urgeles, Roger urgeles@icm.csic.es Urgeles, Roger Camerlenghi, Angelo Rüther, Denise C. Fantoni, L. Brückner, Nils W. de Pro Díaz, Yolanda North: 84ºN, South: 30ºN, West: 33ºW, East: 43ºE start=Miocene; end=Present 2021-07-01 application/vnd.shp application/vnd.google-earth.kml+xml http://hdl.handle.net/10261/247742 eng eng DIGITAL.CSIC info:eu-repo/grantAgreement/EC/H2020/721403 MINECO/ICTI2013-2016/CTM2015-70155-R Collico, S., Arroyo; M., Urgeles, R., Gràcia E:, De Vincenzi, M., Peréz, N. (2020): Probabilistic mapping of earthquake-induced submarine landslide susceptibility in the South-West Iberian margin. Marine Geology, 429: 106296. https://doi.org/10.1016/j.margeo.2020.106296 . http://hdl.handle.net/10261/219760 Urgeles, R., Camerlenghi, A. (2013): Submarine landslides of the Mediterranean Sea: trigger mechanisms, dynamics and frequency‐magnitude distribution, Journal of Geophysical Research Earth Surface, 118: 2600-2618. http://dx.doi.org/10.1002/2013JF002720 . http://hdl.handle.net/10261/92232 Sallarès, V., Gràcia, E., Urgeles, R. (2011): Active faulting and slope failure in the Iberian margins: towards offshore geohazard mitigation. In Briand, G. (Ed.) Marine geo-hazards in the Mediterranean, CIESM Workshop Monograph nº 42, pp. 101-112. http://hdl.handle.net/10261/57350 Camerlenghi, A., Urgeles, R., Fantoni, L. (2010): A Database on Submarine Landslides of the Mediterranean Sea. In Mosher, D.C., Moscardelli, L., Shipp, R.C., Chaytor, J.D., Baxter, C.D.P., Lee, H.J., Urgeles, R. (Eds.) Submarine Mass Movements and Their Consequences, Advances in Natural and Technological Hazards Research, 28, Spinger, Dordrecht (The Netherlands), pp. 491-501. http://dx.doi.org/10.1007/978-90-481-3071-9_41 . http://hdl.handle.net/10261/76715 https://ls3gp.icm.csic.es/?page_id=553 Sí Urgeles, Roger; Camerlenghi, Angelo; Rüther, Denise C.; Fantoni, L.; Brückner, Nils W.; de Pro Díaz, Yolanda; 2021; The Euro-Mediterranean Submarine landSlide database (EMSS21); DIGITAL.CSIC; DOI http://hdl.handle.net/10261/247742 openAccess http://creativecommons.org/licenses/by/4.0/ CC-BY Submarine landslide Geohazard Landslide scar Landslide deposit Trigger mechanism dataset 2021 ftcsic https://doi.org/10.1016/j.margeo.2020.106296 https://doi.org/10.1002/2013JF002720 https://doi.org/10.1007/978-90-481-3071-9_41 2021-08-17T23:35:20Z The Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only. Disclaimer: The EMSS21 is open to later additions and improvements. For these reasons and due to its intrinsic nature, the EMSS21 cannot be guaranteed to be complete, accurate and updated in any part, and will be subjected to successive revisions. Although the Institut de Ciències del Mar of CSIC makes every effort to supply the best available information, no warranty, expressed or implied, is provided as to the accuracy and reliability of all the data supplied in the EMSS21. Users are cautioned to consider carefully the nature of the data and information before using it for decisions that concern personal or public safety. Conclusions drawn from the EMSS21, or actions undertaken on the basis of its contents, are the sole responsibility of the user. The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as these events are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard. The EMSS21 displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only. Data compilation has been possible thanks to projects: Submarine landslides and Their impact on European continental margins (SLATE) - H2020-MSCA-ITN-2016-721403. ImagiNg large SeismogenIc and tsunamiGenic structures of the Gulf of Cadiz with ultra-High resolution Technologies (INSIGHT). - CTM2015-70155-R. The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as theseevents are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard. Peer reviewed Dataset Arctic Digital.CSIC (Spanish National Research Council) Arctic |