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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Published in:Journal of Quaternary Science
Main Author: Teodorski, Artur
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access: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
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spelling 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
institution Open Polar
collection Wiley Online Library
op_collection_id 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
container_title Journal of Quaternary Science
container_volume 38
container_issue 5
container_start_page 647
op_container_end_page 657
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