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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Uniwersytet im. Adama Mickiewicza w Poznaniu
2016
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Online Access: | https://doi.org/10.1515/quageo-2016-0002 https://bibliotekanauki.pl/articles/1052742.pdf https://bibliotekanauki.pl/articles/1052742 |
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fttriple:oai:gotriple.eu:ValoZO8clAXC-G5o2jLwO 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 2016-03-15 https://doi.org/10.1515/quageo-2016-0002 https://bibliotekanauki.pl/articles/1052742.pdf https://bibliotekanauki.pl/articles/1052742 en eng Uniwersytet im. Adama Mickiewicza w Poznaniu doi:10.1515/quageo-2016-0002 https://bibliotekanauki.pl/articles/1052742.pdf https://bibliotekanauki.pl/articles/1052742 lic_creative-commons Quaestiones Geographicae; 2016, 35, 1; 29-36 0137-477X 2081-6383 geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2016 fttriple https://doi.org/10.1515/quageo-2016-0002 2023-01-22T19:38:19Z 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 |
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language |
English |
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geo envir |
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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 |
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 |
Uniwersytet im. Adama Mickiewicza w Poznaniu |
publishDate |
2016 |
url |
https://doi.org/10.1515/quageo-2016-0002 https://bibliotekanauki.pl/articles/1052742.pdf https://bibliotekanauki.pl/articles/1052742 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Quaestiones Geographicae; 2016, 35, 1; 29-36 0137-477X 2081-6383 |
op_relation |
doi:10.1515/quageo-2016-0002 https://bibliotekanauki.pl/articles/1052742.pdf https://bibliotekanauki.pl/articles/1052742 |
op_rights |
lic_creative-commons |
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 |
_version_ |
1766030922236297216 |