{"@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/1362825895835382912.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.sedgeo.2012.08.005"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S003707381200231X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S003707381200231X?httpAccept=text/plain"}}],"dc:title":[{"@value":"Erosion, deposition and landscape change on the Sendai coastal plain, Japan, resulting from the March 11, 2011 Tohoku-oki tsunami"}],"description":[{"notation":[{"@value":"Case studies of recent tsunami impacts have proven to be extremely useful in understanding the geologic processes involved during inundation and return flow, and refining the criteria used to identify paleotsunami deposits in the geologic record. Here, we report on erosion, deposition and associated landscape change resulting from the March 11, 2011 Tohoku-oki tsunami along a nearly 4.5 km shore-normal transect on the coastal plain near Sendai, Japan. The study area on the broad, low-relief prograding coastal Sendai plain comprised a sand beach backed by ~ 3 m high sand dunes and a forest, a wetland, the Teizan canal, agricultural rice fields, buildings and roads.    Field observations focused on measurements of tsunami flow characteristics (height and direction), mapping of erosion features and assessing sediment deposition based on shallow trenches at 50–100 m spacing. Recorded tsunami inundation heights reached up to about 11 m above mean sea level within the first 500 m from the shoreline and then ranged between 3 and 5 m for the next 2 km, gradually decreasing to about 3 m close to the inundation limit. The tsunami deposit generally thinned landward from an average maximum ~ 30 cm thick sand deposit in the coastal forest to a thin mud drape several mm thick near the inundation limit. A discontinuous sand-dominated sheet was prevalent to about 2800 m from the shoreline where mud content then gradually increased further landward eventually resulting in a mud-dominated deposit ranging from 3.5 cm to a few mm thickness. The overall thinning and fining of the deposit was often interrupted by localized features that led to complex sedimentological relationships over short distances.    Satellite imagery taken on 14 March 2011, 3 days after the Tohoku-oki Tsunami shows prominent foreshore incisions with 100 s + meters spacing alongshore, a foredune ridge that underwent severe erosion and development of a prominent shore-parallel elongated scour depression. Our field survey in early May 2011 revealed that the foreshore recovered quickly with rapid post-tsunami sediment deposition from incident waves, whereas the dune–ridge complex had undergone only minor re-working from eolian processes."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895835382915","@type":"Researcher","foaf:name":[{"@value":"Bruce Richmond"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382785","@type":"Researcher","foaf:name":[{"@value":"Witold Szczuciński"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382916","@type":"Researcher","foaf:name":[{"@value":"Catherine Chagué-Goff"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382786","@type":"Researcher","foaf:name":[{"@value":"Kazuhisa Goto"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382919","@type":"Researcher","foaf:name":[{"@value":"Daisuke Sugawara"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382917","@type":"Researcher","foaf:name":[{"@value":"Rob Witter"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382784","@type":"Researcher","foaf:name":[{"@value":"David R. Tappin"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382912","@type":"Researcher","foaf:name":[{"@value":"Bruce Jaffe"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382913","@type":"Researcher","foaf:name":[{"@value":"Shigehiro Fujino"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382918","@type":"Researcher","foaf:name":[{"@value":"Yuichi Nishimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895835382914","@type":"Researcher","foaf:name":[{"@value":"James Goff"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-12","prism:volume":"282","prism:startingPage":"27","prism:endingPage":"39"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S003707381200231X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S003707381200231X?httpAccept=text/plain"}],"createdAt":"2012-08-30","modifiedAt":"2025-09-22","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813846346112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Examination of the largest-possible tsunamis (Level 2) generated along the Nankai and Suruga troughs during the past 4000years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"},{"@value":"Examination of the largest-possible tsunamis (Level 2 tsunami) generated along the Nankai and Suruga troughs during the past 4000 years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"}]},{"@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/1360005517247973632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami deposits refine great earthquake rupture extent and recurrence over the past 1300 years along the Nankai and Tokai fault segments of the Nankai Trough, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168758225152","@type":"Article","resourceType":"学術雑誌論文(journal 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707446168960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stratigraphic evidence of historical and prehistoric tsunamis on the Pacific coast of central Japan: Implications for the variable recurrence of tsunamis in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643802233600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical estimation of maximum possible sizes of paleo-earthquakes and tsunamis from storm-derived boulders"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865726231808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine inundation history during the last 3000 years at Lake Kogare-ike, a coastal lake on the Pacific coast of central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360303782143371136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-precision estimation of a paleo-tsunami inundation area by identifying tsunami traces beyond sandy tsunami deposits: A case study of the 869 CE Jogan tsunami in Fukushima, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166017452672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial thickness variability of the 2011 Tohoku-oki tsunami deposits along the coastline of Sendai Bay"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180532124800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Restoration Measures After the 2011 Tohoku-oki Tsunami and Their Impact on Tsunami Research"}]},{"@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/1360567182451575424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Are inundation limit and maximum extent of sand useful for differentiating tsunamis and storms? An example from sediment transport simulations on the Sendai Plain, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092458494080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical modeling of tsunami: advances and future challenges after the 2011 Tohoku earthquake and tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567450716160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A geochemical approach for identifying marine incursions: Implications for tsunami geology on the Pacific coast of northeast Japan"}]},{"@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? 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