Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland)
the aim of this article is the description of lithofacies characteristics of sediments forming the north-east part of the morainic upland edge zone in the vicinity of Piaski Pomorskie (west Pomerania). the paper undertake also an attempt to reconstruct paleogeographical conditions of the formation o...
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Adam Mickiewicz University Poznan
2016
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ftamickiewiczojs:oai:ojs.pressto.amu.edu.pl:article/7543 2023-07-30T04:04:12+02:00 Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) Paluszkiewicz, Ryszard Paluszkiewicz, Renata 2016-03-15 application/pdf http://pressto.amu.edu.pl/index.php/qg/article/view/7543 eng eng Adam Mickiewicz University Poznan http://pressto.amu.edu.pl/index.php/qg/article/view/7543/7570 http://pressto.amu.edu.pl/index.php/qg/article/view/7543 Quaestiones Geographicae; Vol. 35 No. 1 (2016); 29-36 Quaestiones Geographicae; Tom 35 Nr 1 (2016); 29-36 2081-6383 0137-477X morainic upland edge zone lithofacies analysis the Pomeranian Phase west Pomerania info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Recenzowany artykuł 2016 ftamickiewiczojs 2023-07-17T19:43:05Z the aim of this article is the description of lithofacies characteristics of sediments forming the north-east part of the morainic upland edge zone in the vicinity of Piaski Pomorskie (west Pomerania). the paper undertake also an attempt to reconstruct paleogeographical conditions of the formation of moranic uppland edge. The diversification of glaciofluvial and fluvial processes during the phase of stagnation and recession of uppervistulian ice-sheet in the vicinity of Piaski Pomorskie (western Pomerania) led to the formation of a morainic upland edge distinctly marked in morphology The edge zone separates the undulating moraine plateau from a lower situated Dębnica River Valley. This area is mostly formed by fine-grained sands with occasional layers of a coarser fraction of gravel and coarse- and medium-grained sands. The observed type of low-angle cross-stratification and trough cross-stratification indicates the dominance of diversified energy depositional environment with considerable power of water as transporting medium. the research area was formed at the front of the ice-sheet, which receded from the nearby reach of the Pomeranian Phase of the weichselian glaciation. Article in Journal/Newspaper Ice Sheet Adam Mickiewicz University in Poznań: PRESSto Quaestiones Geographicae 35 1 29 36 |
institution |
Open Polar |
collection |
Adam Mickiewicz University in Poznań: PRESSto |
op_collection_id |
ftamickiewiczojs |
language |
English |
topic |
morainic upland edge zone lithofacies analysis the Pomeranian Phase west Pomerania |
spellingShingle |
morainic upland edge zone lithofacies analysis the Pomeranian Phase west Pomerania Paluszkiewicz, Ryszard Paluszkiewicz, Renata Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
topic_facet |
morainic upland edge zone lithofacies analysis the Pomeranian Phase west Pomerania |
description |
the aim of this article is the description of lithofacies characteristics of sediments forming the north-east part of the morainic upland edge zone in the vicinity of Piaski Pomorskie (west Pomerania). the paper undertake also an attempt to reconstruct paleogeographical conditions of the formation of moranic uppland edge. The diversification of glaciofluvial and fluvial processes during the phase of stagnation and recession of uppervistulian ice-sheet in the vicinity of Piaski Pomorskie (western Pomerania) led to the formation of a morainic upland edge distinctly marked in morphology The edge zone separates the undulating moraine plateau from a lower situated Dębnica River Valley. This area is mostly formed by fine-grained sands with occasional layers of a coarser fraction of gravel and coarse- and medium-grained sands. The observed type of low-angle cross-stratification and trough cross-stratification indicates the dominance of diversified energy depositional environment with considerable power of water as transporting medium. the research area was formed at the front of the ice-sheet, which receded from the nearby reach of the Pomeranian Phase of the weichselian glaciation. |
format |
Article in Journal/Newspaper |
author |
Paluszkiewicz, Ryszard Paluszkiewicz, Renata |
author_facet |
Paluszkiewicz, Ryszard Paluszkiewicz, Renata |
author_sort |
Paluszkiewicz, Ryszard |
title |
Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
title_short |
Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
title_full |
Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
title_fullStr |
Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
title_full_unstemmed |
Analysis of Sediments in the North-East Morainic Upland Edge Zone in the Vicinity of Piaski Pomorskie (West Pomerania, NW Poland) |
title_sort |
analysis of sediments in the north-east morainic upland edge zone in the vicinity of piaski pomorskie (west pomerania, nw poland) |
publisher |
Adam Mickiewicz University Poznan |
publishDate |
2016 |
url |
http://pressto.amu.edu.pl/index.php/qg/article/view/7543 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Quaestiones Geographicae; Vol. 35 No. 1 (2016); 29-36 Quaestiones Geographicae; Tom 35 Nr 1 (2016); 29-36 2081-6383 0137-477X |
op_relation |
http://pressto.amu.edu.pl/index.php/qg/article/view/7543/7570 http://pressto.amu.edu.pl/index.php/qg/article/view/7543 |
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Quaestiones Geographicae |
container_volume |
35 |
container_issue |
1 |
container_start_page |
29 |
op_container_end_page |
36 |
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1772815445869461504 |