Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000053" target="_blank" >RIV/00025798:_____/03:00000053 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/03:00000435
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Geomorphological aspects of glaciation in the Oldřichov Highland, Northern Bohemia, Czechia
Original language 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. These sediments are a relic of a glaciofluvial terrace which accumulated in front of a small lobe ofan 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 ~400-500 m to the south of the col. The maximum thickness of the lacierwas also determined. Clast petrology varies up-section in the glaciofluvial sediments with the predominance of local and near rocks together with quartz clasts of mainly near origin. Lower amount of nordic material was influenced by the local
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Project
<a href="/en/project/SB%2F630%2F1%2F98" target="_blank" >SB/630/1/98: Basic and special geological mappingof the Czech Republic at 1:25000 scale</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2003
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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