Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland
tytuł dodatkowy: Prace z Inżynierii Lądowej i Środowiska The current research focuses on explaining the origin of end moraines running through the northernmost districts of the city of Poznań. The highest hills, that is, the Moraska Hill and the Dziewicza Hill, are a stagnation record of the Vistuli...
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Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego
2019
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ftunivzielonogor:oai:zbc.uz.zgora.pl:68184 2023-05-15T16:40:59+02:00 Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland Widera, Marek Chomiak, Lilianna Kuczyński, Tadeusz - red. 2019 application/pdf https://zbc.uz.zgora.pl/dlibra/docmetadata?showContent=true&id=68184 http://zbc.uz.zgora.pl/Content/68184/ceer2019_3_widera_various.pdf eng eng Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego oai:zbc.uz.zgora.pl:publication:75108 https://zbc.uz.zgora.pl/dlibra/docmetadata?showContent=true&id=68184 oai:zbc.uz.zgora.pl:68184 http://zbc.uz.zgora.pl/Content/68184/ceer2019_3_widera_various.pdf Biblioteka Uniwersytetu Zielonogórskiego Civil and Environmental Engineering Reports (CEER), no 29, vol. 3 Pleistocene of central-western Poland accumulative moraines push end moraines depositional processes deformational processes Scandinavian ice sheet Plejstocen Polska środkowo-zachodnia moreny akumulacyjne moreny pchające procesy depozytowe procesy deformacyjne skandynawskie pokrywy lodowe lodowiec skandynawski artykuł 2019 ftunivzielonogor 2022-12-27T00:09:33Z tytuł dodatkowy: Prace z Inżynierii Lądowej i Środowiska The current research focuses on explaining the origin of end moraines running through the northernmost districts of the city of Poznań. The highest hills, that is, the Moraska Hill and the Dziewicza Hill, are a stagnation record of the Vistulian Glaciation of the Poznań Phase. These two hills represent terminal moraines of similar height and age, but the mechanism of their formation is diametrically opposed. The Dziewicza Hill is a typical accumulative end moraine, where Pleistocene deposits over 70 m thick are undisturbed. On the other hand, the Moraska Hill is a classic example of a push end moraine with a relatively thin cover of Pleistocene sediments and glaciotectonically elevated (up to 130 m a.s.l.) upper Neogene deposits. In the latter case, these strongly deformed sediments are the so-called "Poznań Clays" that underlie the Quaternary deposits in the vast area of the Polish Lowlands. Article in Journal/Newspaper Ice Sheet Uniwersytet Zielonogórski: Zielonogórska Biblioteka Cyfrowa Polska ENVELOPE(27.500,27.500,67.100,67.100) |
institution |
Open Polar |
collection |
Uniwersytet Zielonogórski: Zielonogórska Biblioteka Cyfrowa |
op_collection_id |
ftunivzielonogor |
language |
English |
topic |
Pleistocene of central-western Poland accumulative moraines push end moraines depositional processes deformational processes Scandinavian ice sheet Plejstocen Polska środkowo-zachodnia moreny akumulacyjne moreny pchające procesy depozytowe procesy deformacyjne skandynawskie pokrywy lodowe lodowiec skandynawski |
spellingShingle |
Pleistocene of central-western Poland accumulative moraines push end moraines depositional processes deformational processes Scandinavian ice sheet Plejstocen Polska środkowo-zachodnia moreny akumulacyjne moreny pchające procesy depozytowe procesy deformacyjne skandynawskie pokrywy lodowe lodowiec skandynawski Widera, Marek Chomiak, Lilianna Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
topic_facet |
Pleistocene of central-western Poland accumulative moraines push end moraines depositional processes deformational processes Scandinavian ice sheet Plejstocen Polska środkowo-zachodnia moreny akumulacyjne moreny pchające procesy depozytowe procesy deformacyjne skandynawskie pokrywy lodowe lodowiec skandynawski |
description |
tytuł dodatkowy: Prace z Inżynierii Lądowej i Środowiska The current research focuses on explaining the origin of end moraines running through the northernmost districts of the city of Poznań. The highest hills, that is, the Moraska Hill and the Dziewicza Hill, are a stagnation record of the Vistulian Glaciation of the Poznań Phase. These two hills represent terminal moraines of similar height and age, but the mechanism of their formation is diametrically opposed. The Dziewicza Hill is a typical accumulative end moraine, where Pleistocene deposits over 70 m thick are undisturbed. On the other hand, the Moraska Hill is a classic example of a push end moraine with a relatively thin cover of Pleistocene sediments and glaciotectonically elevated (up to 130 m a.s.l.) upper Neogene deposits. In the latter case, these strongly deformed sediments are the so-called "Poznań Clays" that underlie the Quaternary deposits in the vast area of the Polish Lowlands. |
author2 |
Kuczyński, Tadeusz - red. |
format |
Article in Journal/Newspaper |
author |
Widera, Marek Chomiak, Lilianna |
author_facet |
Widera, Marek Chomiak, Lilianna |
author_sort |
Widera, Marek |
title |
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
title_short |
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
title_full |
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
title_fullStr |
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
title_full_unstemmed |
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland |
title_sort |
various genetic types of end moraines in the city of poznań and its close vicinity, central-western poland |
publisher |
Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego |
publishDate |
2019 |
url |
https://zbc.uz.zgora.pl/dlibra/docmetadata?showContent=true&id=68184 http://zbc.uz.zgora.pl/Content/68184/ceer2019_3_widera_various.pdf |
long_lat |
ENVELOPE(27.500,27.500,67.100,67.100) |
geographic |
Polska |
geographic_facet |
Polska |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Civil and Environmental Engineering Reports (CEER), no 29, vol. 3 |
op_relation |
oai:zbc.uz.zgora.pl:publication:75108 https://zbc.uz.zgora.pl/dlibra/docmetadata?showContent=true&id=68184 oai:zbc.uz.zgora.pl:68184 http://zbc.uz.zgora.pl/Content/68184/ceer2019_3_widera_various.pdf |
op_rights |
Biblioteka Uniwersytetu Zielonogórskiego |
_version_ |
1766031417586745344 |