Morphostratigraphy of the Sázava river terraces in the Bohemian Massif

dc.contributor.author	Gibbard, Philip L.
dc.contributor.author	Kalvoda, Jan
dc.contributor.author	Balatka, Břetislav
dc.coverage.spatial	Sázava, řeka (Česko)	cs
dc.coverage.spatial	Český masiv	cs
dc.date.accessioned	2021-11-25T04:23:59Z
dc.date.available	2021-11-25T04:23:59Z
dc.date.issued	2010
dc.identifier.uri	http://hdl.handle.net/20.500.11956/165863
dc.description.abstract	The results of geomorphological research into the Sázava river terraces are presented. This terrace system is characteristic by its variable structure which is conditioned by specific hydrodynamic processes that existed during the late Cenozoic evolution of the river valley. Two levels of Neogene fluvial sediments and seven Quaternary terrace accumulations along the Sázava course are distinguished. In the paper is also established their chronostratigraphical relation to the Vltava-Labe terrace systems.	en
dc.language.iso	en
dc.relation.uri	http://web.natur.cuni.cz/ksgrrsek/acta/2010/2010_kalvoda%20.pdf
dc.title	Morphostratigraphy of the Sázava river terraces in the Bohemian Massif	en
dc.type	Příspěvek v časopisu	cs
dc.description.startPage	3
dc.description.endPage	34
dcterms.isPartOf.name	Acta Universitatis Carolinae. Geographica	en
dcterms.isPartOf.journalYear	2010
dcterms.isPartOf.journalVolume	45
dcterms.isPartOf.journalIssue	1
dcterms.isPartOf.issn	0300-5402
dc.identifier.lisID	000161212