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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Language: | English |
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Online Access: | https://doi.org/10.1515/quageo-2016-0002 https://doaj.org/article/944d80464c9e46cfbaeb1ca3cd55f35d |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:944d80464c9e46cfbaeb1ca3cd55f35d 2023-05-15T16:40:31+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 2016-03-01 https://doi.org/10.1515/quageo-2016-0002 https://doaj.org/article/944d80464c9e46cfbaeb1ca3cd55f35d en eng Sciendo 2081-6383 doi:10.1515/quageo-2016-0002 https://doaj.org/article/944d80464c9e46cfbaeb1ca3cd55f35d undefined Quaestiones Geographicae, Vol 35, Iss 1, Pp 29-36 (2016) morainic upland edge zone lithofacies analysis the pomeranian phase west pomerania geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2016 fttriple https://doi.org/10.1515/quageo-2016-0002 2023-01-22T17:58:05Z 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 Unknown Quaestiones Geographicae 35 1 29 36 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
morainic upland edge zone lithofacies analysis the pomeranian phase west pomerania geo envir |
spellingShingle |
morainic upland edge zone lithofacies analysis the pomeranian phase west pomerania geo envir 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 geo envir |
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 |
Sciendo |
publishDate |
2016 |
url |
https://doi.org/10.1515/quageo-2016-0002 https://doaj.org/article/944d80464c9e46cfbaeb1ca3cd55f35d |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Quaestiones Geographicae, Vol 35, Iss 1, Pp 29-36 (2016) |
op_relation |
2081-6383 doi:10.1515/quageo-2016-0002 https://doaj.org/article/944d80464c9e46cfbaeb1ca3cd55f35d |
op_rights |
undefined |
op_doi |
https://doi.org/10.1515/quageo-2016-0002 |
container_title |
Quaestiones Geographicae |
container_volume |
35 |
container_issue |
1 |
container_start_page |
29 |
op_container_end_page |
36 |
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1766030920261828608 |