{"@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/1360574096047686016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.geomorph.2006.02.005"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0169555X06000791?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0169555X06000791?httpAccept=text/plain"}}],"dc:title":[{"@value":"Supervised landform classification of Northeast Honshu from DEM-derived thematic maps"}],"description":[{"notation":[{"@value":"This paper proposes a quantitative method to classify landforms using four morphometric parameters from DEM-derived thematic raster maps of slope and topographic openness. Because the different surficial processes and stages in the evolution of slopes create landscapes with different shapes, these parameters may lead to a genetic interpretation of topography. The raster maps of slope and topographic openness were constructed for Northeast Honshu, Japan, from 50-m DEMs. The mean and standard deviation of morphometric parameters within a 3050m by 3050m moving window on the raster maps were calculated. The results for some training areas show that constructional/depositional and erosional landforms with different relief have different morphometric characteristics. A supervised landform classification for Northeast Honshu using the knowledge from the training areas revealed a ladder geomorphological structure composed of high mountains, ranges and volcanoes. The close relationship between the ladder geomorphological structure and volcano distribution indicates that the structure reflects the magmatic plumbing system from the upper mantle to the crust of the Northeast Honshu arc."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574096047685888","@type":"Researcher","foaf:name":[{"@value":"Oky Dicky Ardiansyah Prima"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096047686018","@type":"Researcher","foaf:name":[{"@value":"Ayako Echigo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096047686016","@type":"Researcher","foaf:name":[{"@value":"Ryuzo Yokoyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096047686017","@type":"Researcher","foaf:name":[{"@value":"Takeyoshi Yoshida"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0169555X"}],"prism:publicationName":[{"@value":"Geomorphology"}],"dc:publisher":[{"@value":"Elsevier 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