{"@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/1362262946209537024.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1502-3885.1997.tb00649.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00649.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00649.x"}}],"dc:title":[{"@value":"The Storegga tsunami along the Norwegian coast, its age and run up"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The statigraphy in 25 coastal lakes shows that most of the Norwegian coastline was impacted by a large tsunami about 7200 <jats:sup>14</jats:sup>C BP. The methodology has been to core a staircase of lake basins above the contemporary sea level in several areas and to map the tsunami deposit to its maximum elevation. The tsunami was identified in the sedimentary record as an erosional unconformity overlain by graded or massive sand with shell fragments, followed by redeposited organic detritus. The greatest recorded runup along the coast (10–11 m above high tide) is found in areas most proximal to the Storegga slide scar on the Norwegian continental slope (Sunnmøre). To the north and south, runup is less, about 6–7 m at Bjugn (250 km north of Sunnmøre) and about 3–5 m in Austrheim (200 km to the south of Sunnmerre). This runup pattern supports the suggestion that the tsunami was generated by the Second Storegga Slide. The recorded runup heights are consistent within and between the investigated areas, and imply that the tsunami wave was not significantly influenced by the local topography, suggesting a very long wave length. The mapped runup estimates are in good agreement with a numerical model of the tsunami generated by the Second Storegga slide, and indicate that the slide was a single major event rather than a set of smaller slides.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262946209537027","@type":"Researcher","foaf:name":[{"@value":"STEIN BONDEVIK"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946209537026","@type":"Researcher","foaf:name":[{"@value":"JOHN INGE SVENDSEN"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946209537024","@type":"Researcher","foaf:name":[{"@value":"GEIR JOHNSEN"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946209537025","@type":"Researcher","foaf:name":[{"@value":"JAN MANGERUD"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946209537028","@type":"Researcher","foaf:name":[{"@value":"PETER EMIL KALAND"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03009483"},{"@type":"EISSN","@value":"15023885"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/03009483"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/03009483"}],"prism:publicationName":[{"@value":"Boreas"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1997-03","prism:volume":"26","prism:number":"1","prism:startingPage":"29","prism:endingPage":"53"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00649.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00649.x"}],"createdAt":"2010-07-22","modifiedAt":"2023-10-27","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232352906240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Non-destructive analyses to determine appropriate stratigraphic level for dating of tsunami deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516799846528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dating tsunami deposits: Present knowledge and challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168825818368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleotsunami history along the northern Japan trench based on sequential dating of the continuous geological record potentially inundated only by large tsunamis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182451569664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reducing the age range of tsunami deposits by 14C dating of rip-up clasts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814752045824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Can Mud Deposits Indicate Inundation Extent of Paleotsunamis? Insights From Sediment‐Transport Simulations for Sand and Mud"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277369651840","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"FUNDAMENTAL ANALYSIS ON TSUNAMI CHARACTERISTICS GENERATED BY SUBMARINE LANDSLIDE"},{"@language":"ja","@value":"海底地滑りによる津波の発生と地滑り諸元の関係に関する理論解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680196765824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"浅海域および沿岸低地に堆積した津波堆積物の識別基準"},{"@language":"en","@value":"A review on criteria for tsunami deposits recognition in shallow marineand coastal lowlands from geological records"},{"@language":"ja-Kana","@value":"センカイイキ オヨビ エンガン テイチ ニ タイセキ シタ ツナミ タイセキブツ ノ シキベツ キジュン"},{"@value":"A review on criteria for tsunami deposits recognition in shallow marine sand coastal lowlands from geological records"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217169792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Submarine slides and marine geohazards:"},{"@language":"ja","@value":"海底地すべりと災害"},{"@value":"海底地すべりと災害 : これまでの研究成果と現状の問題点"},{"@language":"ja-Kana","@value":"カイテイ ジスベリ ト サイガイ : コレマデ ノ ケンキュウ セイカ ト ゲンジョウ ノ モンダイテン"},{"@value":"Submarine slides and marine geohazards: the study results so far and current problems"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317035012224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three thousand year paleo-tsunami history of the southern part of the Japan Trench"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1502-3885.1997.tb00649.x"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2022.107381_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0031_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2019.102971_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2017.09.008_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00415-w_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.1029/2023jf007137_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2019.02.009_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.4096/jssj.71.119_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"},{"@type":"CROSSREF","@value":"10.2208/kaigan.75.i_325_references_DOI_HIy0hDtQo1PWAHDw4JKCwmutLxS"}]}