Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland
The article is an attempt to find relations between geology and the dynamics of the Mesozoic surface of the Łódź Synclinorium, the Radomsko Elevation and the Bełchatów Graben and the present relief on the border of the Polish Lowlands and Uplands in its central part. Fossil relief has been compared...
Published in: | Geology, Geophysics & Environment |
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Language: | English |
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AGH University of Science and Technology
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Online Access: | https://journals.agh.edu.pl/geol/article/view/3002 https://doi.org/10.7494/geol.2019.45.1.57 |
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ftaghuniojs:oai:ojs.journals.agh.edu.pl:article/3002 2023-05-15T16:40:49+02:00 Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland Szmidt, Aleksander Wachecka-Kotkowska, Lucyna 2019-04-25 application/pdf https://journals.agh.edu.pl/geol/article/view/3002 https://doi.org/10.7494/geol.2019.45.1.57 eng eng AGH University of Science and Technology https://journals.agh.edu.pl/geol/article/view/3002/2207 https://journals.agh.edu.pl/geol/article/view/3002 doi:10.7494/geol.2019.45.1.57 Copyright (c) 2019 Geology, Geophysics and Environment Geology, Geophysics and Environment; Vol. 45 No. 1 (2019); 57 2353-0790 2299-8004 Paleozoic platform sub-Quaternary surface relief inheritance contemporary relief central Poland info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftaghuniojs https://doi.org/10.7494/geol.2019.45.1.57 2021-06-15T07:35:29Z The article is an attempt to find relations between geology and the dynamics of the Mesozoic surface of the Łódź Synclinorium, the Radomsko Elevation and the Bełchatów Graben and the present relief on the border of the Polish Lowlands and Uplands in its central part. Fossil relief has been compared with the present one as related to the extent of the recession phases of the Saalian (Wartanian) ice-sheet. A significant convergence has been found between the Mesozoic surface plain and the main morphologic elements. The role of elevations and fossil valleys has been stressed as stable forms in the pre-Pleistocene and contemporary landscape. Also stressed has been the meaning of grabens and elevations enforcing longer stoppages of the Wartanian stadial of the Middle Polish Glaciations. Article in Journal/Newspaper Ice Sheet AGH (Akademia Górniczo-Hutnicza) University of Science and Technology: Journals Geology, Geophysics & Environment 45 1 57 |
institution |
Open Polar |
collection |
AGH (Akademia Górniczo-Hutnicza) University of Science and Technology: Journals |
op_collection_id |
ftaghuniojs |
language |
English |
topic |
Paleozoic platform sub-Quaternary surface relief inheritance contemporary relief central Poland |
spellingShingle |
Paleozoic platform sub-Quaternary surface relief inheritance contemporary relief central Poland Szmidt, Aleksander Wachecka-Kotkowska, Lucyna Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
topic_facet |
Paleozoic platform sub-Quaternary surface relief inheritance contemporary relief central Poland |
description |
The article is an attempt to find relations between geology and the dynamics of the Mesozoic surface of the Łódź Synclinorium, the Radomsko Elevation and the Bełchatów Graben and the present relief on the border of the Polish Lowlands and Uplands in its central part. Fossil relief has been compared with the present one as related to the extent of the recession phases of the Saalian (Wartanian) ice-sheet. A significant convergence has been found between the Mesozoic surface plain and the main morphologic elements. The role of elevations and fossil valleys has been stressed as stable forms in the pre-Pleistocene and contemporary landscape. Also stressed has been the meaning of grabens and elevations enforcing longer stoppages of the Wartanian stadial of the Middle Polish Glaciations. |
format |
Article in Journal/Newspaper |
author |
Szmidt, Aleksander Wachecka-Kotkowska, Lucyna |
author_facet |
Szmidt, Aleksander Wachecka-Kotkowska, Lucyna |
author_sort |
Szmidt, Aleksander |
title |
Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
title_short |
Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
title_full |
Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
title_fullStr |
Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
title_full_unstemmed |
Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland |
title_sort |
relations between present relief on the border of lowlands and highlands and geological structures of the paleozoic platform – a case study from central poland |
publisher |
AGH University of Science and Technology |
publishDate |
2019 |
url |
https://journals.agh.edu.pl/geol/article/view/3002 https://doi.org/10.7494/geol.2019.45.1.57 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geology, Geophysics and Environment; Vol. 45 No. 1 (2019); 57 2353-0790 2299-8004 |
op_relation |
https://journals.agh.edu.pl/geol/article/view/3002/2207 https://journals.agh.edu.pl/geol/article/view/3002 doi:10.7494/geol.2019.45.1.57 |
op_rights |
Copyright (c) 2019 Geology, Geophysics and Environment |
op_doi |
https://doi.org/10.7494/geol.2019.45.1.57 |
container_title |
Geology, Geophysics & Environment |
container_volume |
45 |
container_issue |
1 |
container_start_page |
57 |
_version_ |
1766031241459531776 |