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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:24:23Z</responseDate> <request identifier=oai:HAL:halshs-01291496v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:halshs-01291496v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:COMM</setSpec> <setSpec>subject:shs</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:SHS</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-LYON3</setSpec> <setSpec>collection:EMSE</setSpec> <setSpec>collection:ENTPE</setSpec> <setSpec>collection:ENS-LYON</setSpec> <setSpec>collection:BRGM</setSpec> <setSpec>collection:UNIV-ST-ETIENNE</setSpec> <setSpec>collection:UNIV-LYON2</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UPMC</setSpec> <setSpec>collection:IJLRDA</setSpec> <setSpec>collection:EVS_UMR5600</setSpec> <setSpec>collection:UPMC_POLE_1</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Potential for landslide-related tsunami in the Dover Strait area (English Chanel) based on numerical modelling</title> <creator>Rogers, J.</creator> <creator>Gunnell, Yanni</creator> <creator>Krien, Yann</creator> <creator>Ray, P.</creator> <contributor>Laboratoire de Recherche en Géosciences et Énergies (LaRGE) ; Université des Antilles et de la Guyane (UAG)</contributor> <contributor>Environnement Ville Société (EVS) ; Centre National de la Recherche Scientifique (CNRS) - École nationale supérieure d'architecture de Lyon (ENSAL) - Ecole Nationale Supérieure des Mines de Saint-Etienne - École Nationale des Travaux Publics de l'État (ENTPE) - Université Jean Monnet [Saint-Étienne] (UJM) - Université Jean Moulin - Lyon III - Université Lumière - Lyon 2 (UL2) - École normale supérieure - Lyon (ENS Lyon)</contributor> <contributor>Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)</contributor> <contributor>Institut Jean Le Rond d'Alembert (DALEMBERT) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS)</contributor> <description>International audience</description> <source>Proceedings of the 15th World Conference on Earthquake Engineering</source> <source>Proceedings of the 15th World Conference on Eaerthquake Engineering, 2012</source> <coverage>Lisbonne, Portugal</coverage> <identifier>halshs-01291496</identifier> <identifier>https://halshs.archives-ouvertes.fr/halshs-01291496</identifier> <source>https://halshs.archives-ouvertes.fr/halshs-01291496</source> <source>Proceedings of the 15th World Conference on Eaerthquake Engineering, 2012, 2012, Lisbonne, Portugal. Proceedings of the 15th World Conference on Earthquake Engineering, 7 p., 2012</source> <language>en</language> <subject lang=en>tsunami</subject> <subject lang=en> landslide tusnamis</subject> <subject lang=en> English Channel</subject> <subject lang=en> numerical modelling</subject> <subject>[SHS] Humanities and Social Sciences</subject> <subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject> <type>info:eu-repo/semantics/conferenceObject</type> <type>Conference papers</type> <description lang=en>Although earthquakes and tsunamis are less frequent in the Dover Straitthan over active subduction zones, a plausible potential exists for intraplate earthquakes of magnitude Mw=6.9 generating a tsunami with damaging consequences. In April 1580, an earthquake shook the region violently and destructions were reported as far as London in the north andRouen in the south. Despite fair weather conditions, a series of abnormal sea waves was reported in several harbours (Calais, Boulogne and Dover) on the same day. A first step was to produce a range of numerical coseismic tsunami simulations and to compare them with historical witness accounts. Results raise the question of whether such earthquakes could also triggerchalk flow-generated tsunamis along cliff lines on both sides of the Strait. Gravity-driven collapses affect thechalk cliffs periodically, but local tsunami waves caused by very large mass movements could reach heights of several meters and, for example, strike Dover.</description> <date>2012</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>