Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis
ABSTRACT North‐central Poland was originally shaped by the Płock lobe of the ice sheet formed during the Weichselian Glaciation. The majority of the studied area comprises the Dobrzyń Lakeland, where numerous terminal moraine hills preserve a record of recession of the ice sheet from the maximum ext...
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crwiley:10.1002/jqs.3510 2024-06-02T08:08:10+00:00 Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis Teodorski, Artur 2023 http://dx.doi.org/10.1002/jqs.3510 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3510 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3510 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 38, issue 5, page 647-657 ISSN 0267-8179 1099-1417 journal-article 2023 crwiley https://doi.org/10.1002/jqs.3510 2024-05-03T11:12:39Z ABSTRACT North‐central Poland was originally shaped by the Płock lobe of the ice sheet formed during the Weichselian Glaciation. The majority of the studied area comprises the Dobrzyń Lakeland, where numerous terminal moraine hills preserve a record of recession of the ice sheet from the maximum extent of the last glaciation (LGM). Analysis of a digital elevation model enabled the determination of a network of morpholineaments, referring to the formation of linear glacial forms. Recession of the ice sheet from the LGM extent in north‐central Poland was uneven and proceeded in stages. Ice‐sheet recession stages were interspersed with local or regional ice‐sheet advance stages. During these individual periods of ice‐sheet behaviour, ice‐sheet movement changed direction from WNW–ESE to NNW–SSE. Transgression of the ice sheet into the central part of the study area as well as the Kujawy–Dobrzyń subphase may be related to cooling of the climate during 18.5–17.7 ka before ad 2000. Article in Journal/Newspaper Ice Sheet Wiley Online Library Journal of Quaternary Science 38 5 647 657 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
ABSTRACT North‐central Poland was originally shaped by the Płock lobe of the ice sheet formed during the Weichselian Glaciation. The majority of the studied area comprises the Dobrzyń Lakeland, where numerous terminal moraine hills preserve a record of recession of the ice sheet from the maximum extent of the last glaciation (LGM). Analysis of a digital elevation model enabled the determination of a network of morpholineaments, referring to the formation of linear glacial forms. Recession of the ice sheet from the LGM extent in north‐central Poland was uneven and proceeded in stages. Ice‐sheet recession stages were interspersed with local or regional ice‐sheet advance stages. During these individual periods of ice‐sheet behaviour, ice‐sheet movement changed direction from WNW–ESE to NNW–SSE. Transgression of the ice sheet into the central part of the study area as well as the Kujawy–Dobrzyń subphase may be related to cooling of the climate during 18.5–17.7 ka before ad 2000. |
format |
Article in Journal/Newspaper |
author |
Teodorski, Artur |
spellingShingle |
Teodorski, Artur Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
author_facet |
Teodorski, Artur |
author_sort |
Teodorski, Artur |
title |
Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
title_short |
Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
title_full |
Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
title_fullStr |
Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
title_full_unstemmed |
Palaeogeographic reconstruction of the Late Weichselian ice sheet in north‐central Poland based on relief analysis |
title_sort |
palaeogeographic reconstruction of the late weichselian ice sheet in north‐central poland based on relief analysis |
publisher |
Wiley |
publishDate |
2023 |
url |
http://dx.doi.org/10.1002/jqs.3510 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3510 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3510 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Journal of Quaternary Science volume 38, issue 5, page 647-657 ISSN 0267-8179 1099-1417 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jqs.3510 |
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Journal of Quaternary Science |
container_volume |
38 |
container_issue |
5 |
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647 |
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657 |
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1800753350940033024 |