Vývoj údolí řeky Boyne (Irsko)

dc.contributor.author	Steklá, Tereza
dc.coverage.spatial	Boyne (Irsko : řeka)	cs
dc.date.accessioned	2021-11-25T05:07:59Z
dc.date.available	2021-11-25T05:07:59Z
dc.date.issued	2019
dc.identifier.uri	http://hdl.handle.net/20.500.11956/169465
dc.description.abstract	The evolution of the Boyne River valley (Ireland) was influenced by morphostructural conditions and glacial processes. The deranged drainage system of the upper Boyne River is an example of a glacially modified watershed. The lower Boyne valley was also influenced by a diverse bedrock and retrograde erosion caused by a glacio-isostatic uplift of Ireland during the late Quaternary. The combination of geomorphic signs of the glacio-isostatic uplift and climate changes has produced the development of six accumulation river terraces.	cs
dc.language.iso	cs
dc.language.iso	en
dc.title	Vývoj údolí řeky Boyne (Irsko)	cs
dc.type	Příspěvek v časopisu	cs
dc.description.startPage	1
dc.description.endPage	11
dcterms.isPartOf.name	Informace České geografické společnosti	cs
dcterms.isPartOf.journalYear	2019
dcterms.isPartOf.journalVolume	38
dcterms.isPartOf.journalIssue	1
dcterms.isPartOf.issn	1213-1075
dc.identifier.lisID	000229841