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dc.contributor.authorNovák, Václav
dc.date.accessioned2021-11-25T03:29:58Z
dc.date.available2021-11-25T03:29:58Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/20.500.11956/161275
dc.description.abstractRiver terraces originate in the course of the retrogressive water erosion that segregates gravel accumulations on the valley bottom from the stream. At the same time the stream descends to a lower level. In the upstream direction gravel accumulations of terraces are progressively younger. River terraces, however, are defined as bodies composed of deposits of an identical age. There are terraces in a "stratigraphical" sense and terraces in a "hydrological" sense. They have not been sufficiently differentiated up to now. That is why both these terms are introduced here by the author for the first timecs
dc.language.isocs
dc.language.isoen
dc.titlePříspěvek k poznání vzniku říčních teras =On the origin of river terracescs
dc.typePříspěvek v časopisucs
dc.description.startPage98
dc.description.endPage104
dcterms.isPartOf.nameSborník Československé geografické společnostics
dcterms.isPartOf.journalYear1987
dcterms.isPartOf.journalVolume92
dcterms.isPartOf.journalIssue2
dcterms.isPartOf.issn0231-5300
dc.identifier.lisID000120964
dc.subject.keywordgeologiecs
dc.subject.keywordgeografiecs


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