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Tsunami sources within the Eastern Santa Barbara channel

Synolakis Kostas, James F. Dolan, Jose C. Borrero

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URIhttp://purl.tuc.gr/dl/dias/CFF5C996-4659-4261-86B9-4A0DE032C61E-
Identifierhttps://doi.org/10.1029/2000GL011980-
Languageen-
Extent4 pagesen
TitleTsunami sources within the Eastern Santa Barbara channelen
CreatorSynolakis Kostasen
CreatorΣυνολακης Κωσταςel
CreatorJames F. Dolanen
CreatorJose C. Borreroen
Content SummarySeveral 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.en
Type of ItemPeer-Reviewed Journal Publicationen
Type of ItemΔημοσίευση σε Περιοδικό με Κριτέςel
Licensehttp://creativecommons.org/licenses/by/4.0/en
Date of Item2015-10-11-
Date of Publication2001-
SubjectEarthquake sea wavesen
SubjectSeismic sea wavesen
SubjectSeismic surgesen
SubjectTidal wavesen
SubjectTunamisen
Subjecttsunamisen
Subjectearthquake sea wavesen
Subjectseismic sea wavesen
Subjectseismic surgesen
Subjecttidal wavesen
Subjecttunamisen
Bibliographic CitationJ. Borrero, J. Dolan ,C. E. Synolakis, " Tsunami sources within the Eastern Santa Barbara channel," Geoph. Res. Letters,vol. 28,no. 4 pp. 643–647,2001.doi:10.1029/2000GL011980en

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