{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362544420187652224.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001gl013110"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001GL013110"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL013110"}}],"dc:title":[{"@value":"Cumbre Vieja Volcano—Potential collapse and tsunami at La Palma, Canary Islands"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Geological evidence suggests that during a future eruption, Cumbre Vieja Volcano on the Island of La Palma may experience a catastrophic failure of its west flank, dropping 150 to 500 km³ of rock into the sea. Using a geologically reasonable estimate of landslide motion, we model tsunami waves produced by such a collapse. Waves generated by the run‐out of a 500 km³ (150 km³) slide block at 100 m/s could transit the entire Atlantic Basin and arrive on the coasts of the Americas with 10–25 m (3–8 m) height.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544420187652224","@type":"Researcher","foaf:name":[{"@value":"Steven N. Ward"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420187652225","@type":"Researcher","foaf:name":[{"@value":"Simon Day"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2001-09","prism:volume":"28","prism:number":"17","prism:startingPage":"3397","prism:endingPage":"3400"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001GL013110"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL013110"}],"createdAt":"2004-02-05","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285706225063936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics of diffuse carbon dioxide emissions from Cumbre Vieja volcano, La Palma, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869603328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Combinations of volcanic-flank and seafloor-sediment failure offshore Montserrat, and their implications for tsunami generation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654731944448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Submarine record of volcanic island construction and collapse in the <scp>L</scp>esser <scp>A</scp>ntilles arc: First scientific drilling of submarine volcanic island landslides by <scp>IODP</scp><scp>E</scp>xpedition 340"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2001gl013110"},{"@type":"CROSSREF","@value":"10.1007/s00445-015-0914-2_references_DOI_DkaITOQtY6qVLS7UPtyGAe1PK44"},{"@type":"CROSSREF","@value":"10.1002/2014gc005652_references_DOI_DkaITOQtY6qVLS7UPtyGAe1PK44"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.11.032_references_DOI_DkaITOQtY6qVLS7UPtyGAe1PK44"}]}