GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU
Glaciofluvial sediments at Kolnovice originated on an outwash plain running along the ice sheet front. Its material is variable from petrographical and provenance point of view, as it was deposited from various parts of a wide ice sheet front. This contrasts with petrologically monotonous deposits o...
Published in: | Geologické výzkumy na Moravě a ve Slezsku |
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ftmasarykunivojs:oai:ojs.journals.muni.cz:article/1631 2024-06-23T07:53:45+00:00 GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU Glaciofluvial outwash plain at Kolnovice compared with terminoglacial fans between Sokol Ridge and Zlaté Hory Highlands near the Jeseník town Hanáček, Martin 2012-11-15 application/pdf https://journals.muni.cz/gvms/article/view/1631 ces cze Masaryk University https://journals.muni.cz/gvms/article/view/1631/1267 https://journals.muni.cz/gvms/article/view/1631 Geologické výzkumy na Moravě a ve Slezsku; Vol 19 No 1-2 (2012) Geological Research in Moravia and Silesia; Vol. 19 No. 1-2 (2012) 2336-4378 1212-6209 Czech Silesia outwash–plain deposits terminoglacial fan deposits Pleistocene continental glaciation info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2012 ftmasarykunivojs 2024-06-04T04:20:50Z Glaciofluvial sediments at Kolnovice originated on an outwash plain running along the ice sheet front. Its material is variable from petrographical and provenance point of view, as it was deposited from various parts of a wide ice sheet front. This contrasts with petrologically monotonous deposits of terminoglacial fans in this area (Písečná and Javorná sites), which originate from one marginal lobe of the ice sheet. In addition, the material in terminoglacial fans comes from the direct surroundings of the sites having been transported only a short distance. Glaciofluvial sediments at Kolnovice originated on an outwash plain running along the ice sheet front. Its material is variable from petrographical and provenance point of view, as it was deposited from various parts of a wide ice sheet front. This contrasts with petrologically monotonous deposits of terminoglacial fans in this area (Písečná and Javorná sites), which originate from one marginal lobe of the ice sheet. In addition, the material in terminoglacial fans comes from the direct surroundings of the sites having been transported only a short distance. Article in Journal/Newspaper Ice Sheet Masaryk University Journals Geologické výzkumy na Moravě a ve Slezsku 19 1-2 |
institution |
Open Polar |
collection |
Masaryk University Journals |
op_collection_id |
ftmasarykunivojs |
language |
Czech |
topic |
Czech Silesia outwash–plain deposits terminoglacial fan deposits Pleistocene continental glaciation |
spellingShingle |
Czech Silesia outwash–plain deposits terminoglacial fan deposits Pleistocene continental glaciation Hanáček, Martin GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
topic_facet |
Czech Silesia outwash–plain deposits terminoglacial fan deposits Pleistocene continental glaciation |
description |
Glaciofluvial sediments at Kolnovice originated on an outwash plain running along the ice sheet front. Its material is variable from petrographical and provenance point of view, as it was deposited from various parts of a wide ice sheet front. This contrasts with petrologically monotonous deposits of terminoglacial fans in this area (Písečná and Javorná sites), which originate from one marginal lobe of the ice sheet. In addition, the material in terminoglacial fans comes from the direct surroundings of the sites having been transported only a short distance. Glaciofluvial sediments at Kolnovice originated on an outwash plain running along the ice sheet front. Its material is variable from petrographical and provenance point of view, as it was deposited from various parts of a wide ice sheet front. This contrasts with petrologically monotonous deposits of terminoglacial fans in this area (Písečná and Javorná sites), which originate from one marginal lobe of the ice sheet. In addition, the material in terminoglacial fans comes from the direct surroundings of the sites having been transported only a short distance. |
format |
Article in Journal/Newspaper |
author |
Hanáček, Martin |
author_facet |
Hanáček, Martin |
author_sort |
Hanáček, Martin |
title |
GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
title_short |
GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
title_full |
GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
title_fullStr |
GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
title_full_unstemmed |
GLACIFLUVIÁLNÍ VÝPLAVOVÁ PLOŠINA U KOLNOVIC A JEJÍ SROVNÁNÍ S TERMINOGLACIÁLNÍMI KUŽELY MEZI SOKOLSKÝM HŘBETEM A ZLATOHORSKOU VRCHOVINOU U JESENÍKU |
title_sort |
glacifluviální výplavová plošina u kolnovic a její srovnání s terminoglaciálními kužely mezi sokolským hřbetem a zlatohorskou vrchovinou u jeseníku |
publisher |
Masaryk University |
publishDate |
2012 |
url |
https://journals.muni.cz/gvms/article/view/1631 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geologické výzkumy na Moravě a ve Slezsku; Vol 19 No 1-2 (2012) Geological Research in Moravia and Silesia; Vol. 19 No. 1-2 (2012) 2336-4378 1212-6209 |
op_relation |
https://journals.muni.cz/gvms/article/view/1631/1267 https://journals.muni.cz/gvms/article/view/1631 |
container_title |
Geologické výzkumy na Moravě a ve Slezsku |
container_volume |
19 |
container_issue |
1-2 |
_version_ |
1802645548087377920 |