<efrbr:recordSet xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:efrbr="http://vfrbr.info/efrbr/1.1" xmlns:efrbr-work="http://vfrbr.info/efrbr/1.1/work" xmlns:efrbr-expression="http://vfrbr.info/efrbr/1.1/expression" xmlns:efrbr-manifestation="http://vfrbr.info/efrbr/1.1/manifestation" xmlns:efrbr-person="http://vfrbr.info/efrbr/1.1/person" xmlns:efrbr-corporateBody="http://vfrbr.info/efrbr/1.1/corporateBody" xmlns:efrbr-concept="http://vfrbr.info/efrbr/1.1/concept" xmlns:efrbr-structure="http://vfrbr.info/efrbr/1.1/structure" xmlns:efrbr-responsible="http://vfrbr.info/efrbr/1.1/responsible" xmlns:efrbr-subject="http://vfrbr.info/efrbr/1.1/subject" xmlns:efrbr-other="http://vfrbr.info/efrbr/1.1/other" xsi:schemaLocation="http://vfrbr.info/efrbr/1.1 http://vfrbr.info/schemas/1.1/efrbr.xsd"><efrbr:entities><efrbr-work:work identifier="http://purl.tuc.gr/dl/dias/CFF5C996-4659-4261-86B9-4A0DE032C61E"><efrbr-work:titleOfTheWork>Tsunami sources within the Eastern Santa  Barbara channel</efrbr-work:titleOfTheWork></efrbr-work:work><efrbr-expression:expression identifier="http://purl.tuc.gr/dl/dias/CFF5C996-4659-4261-86B9-4A0DE032C61E"><efrbr-expression:titleOfTheExpression>Tsunami sources within the Eastern Santa  Barbara channel</efrbr-expression:titleOfTheExpression><efrbr-expression:formOfExpression vocabulary="DIAS:TYPES">
            Peer-Reviewed Journal Publication
            Δημοσίευση σε Περιοδικό με Κριτές
         </efrbr-expression:formOfExpression><efrbr-expression:dateOfExpression type="issued">2015-10-11</efrbr-expression:dateOfExpression><efrbr-expression:dateOfExpression type="published">2001</efrbr-expression:dateOfExpression><efrbr-expression:languageOfExpression vocabulary="iso639-1">en</efrbr-expression:languageOfExpression><efrbr-expression:summarizationOfContent>Several locally generated tsunamis have been reported in Southern California during the past 200 years, yet the hazard from locally generated tsunamis has received considerably little attention. We consider here tsunamis generated by coseismic displacements on the Channel Islands Thrust (CIT) system, as well as waves generated by slope failures along the walls of the Santa Barbara Channel. We find that purely tectonic sources could generate regional tsunamis with ≈ 2m runup, whereas combinations of tectonic sources and submarine mass movements could generate local runup as large as ≈ 15m.</efrbr-expression:summarizationOfContent><efrbr-expression:useRestrictionsOnTheExpression type="creative-commons">http://creativecommons.org/licenses/by/4.0/</efrbr-expression:useRestrictionsOnTheExpression><efrbr-expression:note type="journal name">Geophysical Research Letters</efrbr-expression:note><efrbr-expression:note type="journal volume">4</efrbr-expression:note><efrbr-expression:note type="journal number">28</efrbr-expression:note><efrbr-expression:note type="page range">643–646</efrbr-expression:note></efrbr-expression:expression><efrbr-person:person identifier="http://users.isc.tuc.gr/~ksynolakis"><efrbr-person:nameOfPerson vocabulary="TUC:LDAP">
            Synolakis Kostas
            Συνολακης Κωστας
         </efrbr-person:nameOfPerson></efrbr-person:person><efrbr-person:person identifier="AF22BF11-B3F6-43AB-A37F-9CCB785C1E6F"><efrbr-person:nameOfPerson vocabulary="">
            James F. Dolan
         </efrbr-person:nameOfPerson></efrbr-person:person><efrbr-person:person identifier="06AB1892-283B-4661-9D34-8B636CDD3159"><efrbr-person:nameOfPerson vocabulary="">
            Jose C. Borrero
         </efrbr-person:nameOfPerson></efrbr-person:person><efrbr-concept:concept identifier="http://id.loc.gov/authorities/subjects/sh85138348"><efrbr-concept:termForTheConcept>
            Earthquake sea waves
            Seismic sea waves
            Seismic surges
            Tidal waves
            Tunamis
            tsunamis
            earthquake sea waves
            seismic sea waves
            seismic surges
            tidal waves
            tunamis
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