Seismic hazard assessment of Greenland

Earthquake activity in Greenland has been registered and mapped since 1907 (Larsen et al. 2006) and thus a long (albeit relatively sparse) record of seismic activity is available for evaluation of seismic hazard and risk. Seismic hazard assessment is carried out by judging the probability of future...

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Published in:Geological Survey of Denmark and Greenland (GEUS) Bulletin
Main Authors: Voss, Peter, Kildegaard Poulsen, Stine, Bjerregaard Simonsen, Sebastian, Gregersen, Søren
Format: Article in Journal/Newspaper
Language:English
Published: Geological Survey of Denmark and Greenland (GEUS) 2007
Subjects:
Online Access:https://geusbulletin.org/index.php/geusb/article/view/4976
https://doi.org/10.34194/geusb.v13.4976
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spelling ftjgeusbullet:oai:geusjournals.org:article/4976 2023-05-15T15:33:29+02:00 Seismic hazard assessment of Greenland Voss, Peter Kildegaard Poulsen, Stine Bjerregaard Simonsen, Sebastian Gregersen, Søren 2007-10-12 application/pdf https://geusbulletin.org/index.php/geusb/article/view/4976 https://doi.org/10.34194/geusb.v13.4976 eng eng Geological Survey of Denmark and Greenland (GEUS) https://geusbulletin.org/index.php/geusb/article/view/4976/10638 https://geusbulletin.org/index.php/geusb/article/view/4976 doi:10.34194/geusb.v13.4976 GEUS Bulletin; Vol. 13 (2007): Review of Survey activities 2006; 57-60 2597-2154 2597-2162 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Rapid Communication. Peer-reviewed Article. 2007 ftjgeusbullet https://doi.org/10.34194/geusb.v13.4976 2022-03-15T17:22:23Z Earthquake activity in Greenland has been registered and mapped since 1907 (Larsen et al. 2006) and thus a long (albeit relatively sparse) record of seismic activity is available for evaluation of seismic hazard and risk. Seismic hazard assessment is carried out by judging the probability of future earthquakes in a given region and is based on statistic treatment of earthquake data. The determination of the seismic hazard is the first step in an evaluation of seismic risk, i.e. the possible economic costs and loss of human life after an earthquake. The motivation for this seismic hazard study is the registration of four significant earthquakes in Greenland in 2005. The Geological Survey of Denmark and Greenland (GEUS) received reports of all four earthquakes from residents who had felt the shaking. The 2005 earthquakes were located at or near Qeqertarsuaq on 30 March, Sisimiut on 23 July, Station Nord on 30 August and Attu on 23 October (Fig. 1), with magnitudes on the Richter scale of 4.3, 4.1, 5.1 and 2.5, respectively. The earthquake in Attu led to the inhabitants fleeing in their boats. Article in Journal/Newspaper Attu Greenland Qeqertarsuaq Sisimiut GEUS Bulletin (Geological Survey of Denmark and Greenland) Greenland Sisimiut ENVELOPE(-53.674,-53.674,66.939,66.939) Qeqertarsuaq ENVELOPE(-56.867,-56.867,74.400,74.400) Station Nord ENVELOPE(-16.663,-16.663,81.599,81.599) Geological Survey of Denmark and Greenland (GEUS) Bulletin 13 57 60
institution Open Polar
collection GEUS Bulletin (Geological Survey of Denmark and Greenland)
op_collection_id ftjgeusbullet
language English
description Earthquake activity in Greenland has been registered and mapped since 1907 (Larsen et al. 2006) and thus a long (albeit relatively sparse) record of seismic activity is available for evaluation of seismic hazard and risk. Seismic hazard assessment is carried out by judging the probability of future earthquakes in a given region and is based on statistic treatment of earthquake data. The determination of the seismic hazard is the first step in an evaluation of seismic risk, i.e. the possible economic costs and loss of human life after an earthquake. The motivation for this seismic hazard study is the registration of four significant earthquakes in Greenland in 2005. The Geological Survey of Denmark and Greenland (GEUS) received reports of all four earthquakes from residents who had felt the shaking. The 2005 earthquakes were located at or near Qeqertarsuaq on 30 March, Sisimiut on 23 July, Station Nord on 30 August and Attu on 23 October (Fig. 1), with magnitudes on the Richter scale of 4.3, 4.1, 5.1 and 2.5, respectively. The earthquake in Attu led to the inhabitants fleeing in their boats.
format Article in Journal/Newspaper
author Voss, Peter
Kildegaard Poulsen, Stine
Bjerregaard Simonsen, Sebastian
Gregersen, Søren
spellingShingle Voss, Peter
Kildegaard Poulsen, Stine
Bjerregaard Simonsen, Sebastian
Gregersen, Søren
Seismic hazard assessment of Greenland
author_facet Voss, Peter
Kildegaard Poulsen, Stine
Bjerregaard Simonsen, Sebastian
Gregersen, Søren
author_sort Voss, Peter
title Seismic hazard assessment of Greenland
title_short Seismic hazard assessment of Greenland
title_full Seismic hazard assessment of Greenland
title_fullStr Seismic hazard assessment of Greenland
title_full_unstemmed Seismic hazard assessment of Greenland
title_sort seismic hazard assessment of greenland
publisher Geological Survey of Denmark and Greenland (GEUS)
publishDate 2007
url https://geusbulletin.org/index.php/geusb/article/view/4976
https://doi.org/10.34194/geusb.v13.4976
long_lat ENVELOPE(-53.674,-53.674,66.939,66.939)
ENVELOPE(-56.867,-56.867,74.400,74.400)
ENVELOPE(-16.663,-16.663,81.599,81.599)
geographic Greenland
Sisimiut
Qeqertarsuaq
Station Nord
geographic_facet Greenland
Sisimiut
Qeqertarsuaq
Station Nord
genre Attu
Greenland
Qeqertarsuaq
Sisimiut
genre_facet Attu
Greenland
Qeqertarsuaq
Sisimiut
op_source GEUS Bulletin; Vol. 13 (2007): Review of Survey activities 2006; 57-60
2597-2154
2597-2162
op_relation https://geusbulletin.org/index.php/geusb/article/view/4976/10638
https://geusbulletin.org/index.php/geusb/article/view/4976
doi:10.34194/geusb.v13.4976
op_doi https://doi.org/10.34194/geusb.v13.4976
container_title Geological Survey of Denmark and Greenland (GEUS) Bulletin
container_volume 13
container_start_page 57
op_container_end_page 60
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