| Attributes | Values |
|---|
| rdf:type
| |
| Description
| - The Oldřichov Highland was glaciated during the Middle Pleistocene as evidenced by the proglacial sediments in the valley of the Jeřice River at Mníšek. The glaciofluvial terrace accumulated in front of a small lobe of an ice sheet. Ice sheet mass advanced from north against northern face of the Oldřichov Highland. The southerly advancing ice lobe pushed through Oldřichov Col (478 m) and terminated ~500 m to the south of the col. The maximum thickness of the glacier to the north of the col was 50-60 m. Clast petrology varies up-section with the predominance of local and near rocks together with quartz clasts of mainly near origin. Lower amount of nordic material (below 8 %) was influenced by the local relief. Nordic erratics show the predominance of central and southern Swedish and east Baltic crystalline rocks and Baltic flints. The maximum extent of the glaciation was reconstructed by numerous sedimentological and geomorphological methods with sufficient accuracy.
- The Oldřichov Highland was glaciated during the Middle Pleistocene as evidenced by the proglacial sediments in the valley of the Jeřice River at Mníšek. The glaciofluvial terrace accumulated in front of a small lobe of an ice sheet. Ice sheet mass advanced from north against northern face of the Oldřichov Highland. The southerly advancing ice lobe pushed through Oldřichov Col (478 m) and terminated ~500 m to the south of the col. The maximum thickness of the glacier to the north of the col was 50-60 m. Clast petrology varies up-section with the predominance of local and near rocks together with quartz clasts of mainly near origin. Lower amount of nordic material (below 8 %) was influenced by the local relief. Nordic erratics show the predominance of central and southern Swedish and east Baltic crystalline rocks and Baltic flints. The maximum extent of the glaciation was reconstructed by numerous sedimentological and geomorphological methods with sufficient accuracy. (en)
- The Oldřichov Highland was glaciated during the Middle Pleistocene as evidenced by the proglacial sediments in the valley of the Jeřice River at Mníšek. The glaciofluvial terrace accumulated in front of a small lobe of an ice sheet. Ice sheet mass advanced from north against northern face of the Oldřichov Highland. The southerly advancing ice lobe pushed through Oldřichov Col (478 m) and terminated ~500 m to the south of the col. The maximum thickness of the glacier to the north of the col was 50-60 m. Clast petrology varies up-section with the predominance of local and near rocks together with quartz clasts of mainly near origin. Lower amount of nordic material (below 8 %) was influenced by the local relief. Nordic erratics show the predominance of central and southern Swedish and east Baltic crystalline rocks and Baltic flints. The maximum extent of the glaciation was reconstructed by numerous sedimentological and geomorphological methods with sufficient accuracy. (cs)
|
| Title
| - Geomorfologické aspekty zalednění Oldřichovské vrchoviny, severní Čechy, Česko (cs)
- Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia
- Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia (en)
|
| skos:prefLabel
| - Geomorfologické aspekty zalednění Oldřichovské vrchoviny, severní Čechy, Česko (cs)
- Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia
- Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia (en)
|
| skos:notation
| - RIV/00025798:_____/03:00000435!RIV07-MZP-00025798
|
| http://linked.open.../vavai/riv/strany
| |
| http://linked.open...avai/riv/aktivita
| |
| http://linked.open...avai/riv/aktivity
| - P(SB/630/1/98), Z(MZP:N03/98:00)
|
| http://linked.open...iv/cisloPeriodika
| |
| http://linked.open...vai/riv/dodaniDat
| |
| http://linked.open...aciTvurceVysledku
| |
| http://linked.open.../riv/druhVysledku
| |
| http://linked.open...iv/duvernostUdaju
| |
| http://linked.open...titaPredkladatele
| |
| http://linked.open...dnocenehoVysledku
| |
| http://linked.open...ai/riv/idVysledku
| - RIV/00025798:_____/03:00000435
|
| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - Continental glaciation, middle Pleistocene, northern Bohemia, glaciofluvial sediments, sedimentary petrology, nordic indicators (en)
|
| http://linked.open.../riv/klicoveSlovo
| |
| http://linked.open...odStatuVydavatele
| |
| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/nazevZdroje
| - Acta Universitatis Carolinae ? Geographica
|
| http://linked.open...in/vavai/riv/obor
| |
| http://linked.open...ichTvurcuVysledku
| |
| http://linked.open...cetTvurcuVysledku
| |
| http://linked.open...vavai/riv/projekt
| |
| http://linked.open...UplatneniVysledku
| |
| http://linked.open...v/svazekPeriodika
| |
| http://linked.open...iv/tvurceVysledku
| |
| http://linked.open...n/vavai/riv/zamer
| |
| issn
| |
| number of pages
| |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)