Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)

A new palaeogeographic reconstruction from the end of the Odranian Glaciation to the end of the Weichslian Glaciation (MIS 2) is based on research carried out at the Knyszewicze site, NE Poland, focusing on the dynamics of the Wartanian Glaciation (MIS 6) and showing the lobed nature of this ice she...

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Main Author: Rychel, Joanna
Format: Article in Journal/Newspaper
Language:English
Published: Polish Geological Institute-National Research Institute 2021
Subjects:
Online Access:https://gq.pgi.gov.pl/article/view/27239
id ftjgq:oai:geojournals.pgi.gov.pl:article/27239
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spelling ftjgq:oai:geojournals.pgi.gov.pl:article/27239 2024-09-15T18:12:26+00:00 Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland) Rychel, Joanna 2021-04-08 application/pdf https://gq.pgi.gov.pl/article/view/27239 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/27239/pdf https://gq.pgi.gov.pl/article/view/27239 Copyright (c) 2021 Geological Quarterly Geological Quarterly; Vol. 65 No. 1 (2021); 65: 12, doi:10.7306/gq.1585 Geological Quarterly; Tom 65 Nr 1 (2021); 65: 12, doi:10.7306/gq.1585 1641-7291 glacial lobe periglacial zone polygenetic relief info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftjgq https://doi.org/10.7306/gq.1585 2024-07-30T03:29:08Z A new palaeogeographic reconstruction from the end of the Odranian Glaciation to the end of the Weichslian Glaciation (MIS 2) is based on research carried out at the Knyszewicze site, NE Poland, focusing on the dynamics of the Wartanian Glaciation (MIS 6) and showing the lobed nature of this ice sheet. Reconstruction of deglaciation in the research area was supplemented by analysis of postglacial morpholineaments (MMA). Research carried out at the Jałówka site enabled reconstruction of the processes affecting lake processes during the Eemian (MIS 5e) Interglacial and transformation of this area during the Weichselian Glaciation. The results obtained indicated that the study area was not covered by Weichselian ice, the sediments formerly considered as glacial being slope-related and providing evidence of periglacial conditions. A new conceptual model for the evolution of this area is put forward, showing the polygenetic nature of the relief. The glacial landforms developed during the Warta Stadial and transformed during the Eemian Interglacial were further affected by periglacial processes, which significantly remodelled the relief. Article in Journal/Newspaper Ice Sheet Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
topic glacial lobe
periglacial zone
polygenetic relief
spellingShingle glacial lobe
periglacial zone
polygenetic relief
Rychel, Joanna
Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
topic_facet glacial lobe
periglacial zone
polygenetic relief
description A new palaeogeographic reconstruction from the end of the Odranian Glaciation to the end of the Weichslian Glaciation (MIS 2) is based on research carried out at the Knyszewicze site, NE Poland, focusing on the dynamics of the Wartanian Glaciation (MIS 6) and showing the lobed nature of this ice sheet. Reconstruction of deglaciation in the research area was supplemented by analysis of postglacial morpholineaments (MMA). Research carried out at the Jałówka site enabled reconstruction of the processes affecting lake processes during the Eemian (MIS 5e) Interglacial and transformation of this area during the Weichselian Glaciation. The results obtained indicated that the study area was not covered by Weichselian ice, the sediments formerly considered as glacial being slope-related and providing evidence of periglacial conditions. A new conceptual model for the evolution of this area is put forward, showing the polygenetic nature of the relief. The glacial landforms developed during the Warta Stadial and transformed during the Eemian Interglacial were further affected by periglacial processes, which significantly remodelled the relief.
format Article in Journal/Newspaper
author Rychel, Joanna
author_facet Rychel, Joanna
author_sort Rychel, Joanna
title Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
title_short Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
title_full Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
title_fullStr Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
title_full_unstemmed Palaeogeographic reconstruction of the North Podlasie region in the Sokółka area during the Late Pleistocene (NE Poland)
title_sort palaeogeographic reconstruction of the north podlasie region in the sokółka area during the late pleistocene (ne poland)
publisher Polish Geological Institute-National Research Institute
publishDate 2021
url https://gq.pgi.gov.pl/article/view/27239
genre Ice Sheet
genre_facet Ice Sheet
op_source Geological Quarterly; Vol. 65 No. 1 (2021); 65: 12, doi:10.7306/gq.1585
Geological Quarterly; Tom 65 Nr 1 (2021); 65: 12, doi:10.7306/gq.1585
1641-7291
op_relation https://gq.pgi.gov.pl/article/view/27239/pdf
https://gq.pgi.gov.pl/article/view/27239
op_rights Copyright (c) 2021 Geological Quarterly
op_doi https://doi.org/10.7306/gq.1585
_version_ 1810450010204012544