{"@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/1362825894987811200.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1146/annurev.earth.32.101802.120201"}},{"identifier":{"@type":"URI","@value":"https://www.annualreviews.org/doi/pdf/10.1146/annurev.earth.32.101802.120201"}}],"dc:title":[{"@value":"RIVER AVULSIONS AND THEIR DEPOSITS"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>▪ Abstract  Avulsion is the natural process by which flow diverts out of an established river channel into a new permanent course on the adjacent floodplain. Avulsions are primarily features of aggrading floodplains. Their recurrence interval varies widely among the few modern rivers for which such data exist, ranging from as low as 28 years for the Kosi River (India) to up to 1400 years for the Mississippi. Avulsions cause loss of life, property damage, destabilization of shipping and irrigation channels, and even coastal erosion as sediment is temporarily sequestered on the floodplain. They are also the main process that builds alluvial stratigraphy. Their causes remain relatively unknown, but stability analyses of bifurcating channels suggest that thresholds in the relative energy slope and Shields parameter of the bifurcating channel system are key factors.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825894987811201","@type":"Researcher","foaf:name":[{"@value":"Rudy Slingerland"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences, Penn State University, University Park, Pennsylvania 16802;"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894987811200","@type":"Researcher","foaf:name":[{"@value":"Norman D. Smith"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588-0340;"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00846597"},{"@type":"EISSN","@value":"15454495"}],"prism:publicationName":[{"@value":"Annual Review of Earth and Planetary Sciences"}],"dc:publisher":[{"@value":"Annual Reviews"}],"prism:publicationDate":"2004-05-19","prism:volume":"32","prism:number":"1","prism:startingPage":"257","prism:endingPage":"285"},"reviewed":"false","url":[{"@id":"https://www.annualreviews.org/doi/pdf/10.1146/annurev.earth.32.101802.120201"}],"createdAt":"2004-04-21","modifiedAt":"2024-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845763735820032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Middle to late-Holocene decreased fluvial aggradation and widespread peat initiation in the Ishikari lowland (northern Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707445730816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Holocene fluvial and anthropogenic processes in the region of Uruk in southern Mesopotamia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643714716928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abandonment and rapid infilling of a tide-dominated distributary channel at 0.7 ka in the Mekong River Delta"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182123053824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Holocene floodplain evolution in the Shiribeshi-Toshibetsu River lowland, northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131644152098048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Valley-Confinement and River-Tidal Controls on Channel Morphology Along the Fluvial to Marine Transition Zone of the Ðồng Nai River System, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266988438016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentary facies analysis of the fluvial environment in the Siwalik Group of eastern Nepal : deciphering its relation to contemporary Himalayan tectonics, climate and sea-level change"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1146/annurev.earth.32.101802.120201"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-90268-6_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"},{"@type":"CROSSREF","@value":"10.1177/0959683616646189_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00444-5_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"},{"@type":"CROSSREF","@value":"10.3389/feart.2019.00202_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2017.04.040_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2017.11.037_references_DOI_KjAXKz8e9dRlVqZx4WvJOuN40Bb"}]}