Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland
Abstract The paper presents a research on a marginal zone near Knyszewicze in the southern part of Sokółka Hills (northeastern Poland). Terminal moraine hills are arranged amphitheatrically in a lobal pattern. Dynamics of the Knyszewicze frontal ice-sheet lobe during the Saale Glaciation and success...
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Walter de Gruyter GmbH
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crdegruyter:10.1515/squa-2015-0007 2023-05-15T16:37:26+02:00 Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland Rychel, Joanna Woronko, Barbara Karasiewicz, Mirosław T. Szymczuk, Paweł Morawski, Marcin 2015 http://dx.doi.org/10.1515/squa-2015-0007 http://content.sciendo.com/view/journals/squa/32/2/article-p79.xml unknown Walter de Gruyter GmbH http://creativecommons.org/licenses/by-nc-nd/3.0 CC-BY-NC-ND Studia Quaternaria volume 32, issue 2, page 79-90 ISSN 2300-0384 Earth-Surface Processes Geology journal-article 2015 crdegruyter https://doi.org/10.1515/squa-2015-0007 2022-04-14T05:07:19Z Abstract The paper presents a research on a marginal zone near Knyszewicze in the southern part of Sokółka Hills (northeastern Poland). Terminal moraine hills are arranged amphitheatrically in a lobal pattern. Dynamics of the Knyszewicze frontal ice-sheet lobe during the Saale Glaciation and successive stages of the marginal zone near the village of Knyszewicze were reconstructed based on sedimentary and geomorphological analysis, using a digital elevation model and morpholineaments. Three main phases of the Knyszewicze glacial-lobe activity were identified including accumulation of glaciofluvial deposits, advances of the ice margin and ice-lobe retreat. Moraine hills developed at a stable ice-lobe terminus, initially as short end-moraine fans with the following sequence of lithofacies Gh ⇒ SGh ⇒ Sh or Gm ⇒ Gh ⇒ Sh . Such a sequence indicates cyclic sheet-floods. During a small but dynamic advance of the ice sheet terminus, these deposits were moved forward and monoclinally folded, then furrowed with sloping faults due to horizontal pressure. Typical thrust-block push moraines developed in this way. Ice sheet advance took place when permafrost was present in the substratum and very high water pressure occurred at glacial terminus. Inside a lobal configuration of moraines, there is a rich inventory of glacial forms with a classic terminal depression in the central part. Based on this landform pattern, their shape, rhythm and glaciotectonic disturbances, the land relief may be referred to as a hill-hole pair. The structure of Horczaki Knoll, deposited on the sub-Quaternary tectonic structure, significantly contributed to a development of this marginal zone. Article in Journal/Newspaper Ice Ice Sheet permafrost De Gruyter (via Crossref) Studia Quaternaria 32 2 79 90 |
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De Gruyter (via Crossref) |
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unknown |
topic |
Earth-Surface Processes Geology |
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Earth-Surface Processes Geology Rychel, Joanna Woronko, Barbara Karasiewicz, Mirosław T. Szymczuk, Paweł Morawski, Marcin Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
topic_facet |
Earth-Surface Processes Geology |
description |
Abstract The paper presents a research on a marginal zone near Knyszewicze in the southern part of Sokółka Hills (northeastern Poland). Terminal moraine hills are arranged amphitheatrically in a lobal pattern. Dynamics of the Knyszewicze frontal ice-sheet lobe during the Saale Glaciation and successive stages of the marginal zone near the village of Knyszewicze were reconstructed based on sedimentary and geomorphological analysis, using a digital elevation model and morpholineaments. Three main phases of the Knyszewicze glacial-lobe activity were identified including accumulation of glaciofluvial deposits, advances of the ice margin and ice-lobe retreat. Moraine hills developed at a stable ice-lobe terminus, initially as short end-moraine fans with the following sequence of lithofacies Gh ⇒ SGh ⇒ Sh or Gm ⇒ Gh ⇒ Sh . Such a sequence indicates cyclic sheet-floods. During a small but dynamic advance of the ice sheet terminus, these deposits were moved forward and monoclinally folded, then furrowed with sloping faults due to horizontal pressure. Typical thrust-block push moraines developed in this way. Ice sheet advance took place when permafrost was present in the substratum and very high water pressure occurred at glacial terminus. Inside a lobal configuration of moraines, there is a rich inventory of glacial forms with a classic terminal depression in the central part. Based on this landform pattern, their shape, rhythm and glaciotectonic disturbances, the land relief may be referred to as a hill-hole pair. The structure of Horczaki Knoll, deposited on the sub-Quaternary tectonic structure, significantly contributed to a development of this marginal zone. |
format |
Article in Journal/Newspaper |
author |
Rychel, Joanna Woronko, Barbara Karasiewicz, Mirosław T. Szymczuk, Paweł Morawski, Marcin |
author_facet |
Rychel, Joanna Woronko, Barbara Karasiewicz, Mirosław T. Szymczuk, Paweł Morawski, Marcin |
author_sort |
Rychel, Joanna |
title |
Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
title_short |
Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
title_full |
Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
title_fullStr |
Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
title_full_unstemmed |
Ice-Sheet Dynamics Of Warta Glaciation (SAALE) In The Marginal Zone Of Knyszewicze Area, Northeastern Poland |
title_sort |
ice-sheet dynamics of warta glaciation (saale) in the marginal zone of knyszewicze area, northeastern poland |
publisher |
Walter de Gruyter GmbH |
publishDate |
2015 |
url |
http://dx.doi.org/10.1515/squa-2015-0007 http://content.sciendo.com/view/journals/squa/32/2/article-p79.xml |
genre |
Ice Ice Sheet permafrost |
genre_facet |
Ice Ice Sheet permafrost |
op_source |
Studia Quaternaria volume 32, issue 2, page 79-90 ISSN 2300-0384 |
op_rights |
http://creativecommons.org/licenses/by-nc-nd/3.0 |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1515/squa-2015-0007 |
container_title |
Studia Quaternaria |
container_volume |
32 |
container_issue |
2 |
container_start_page |
79 |
op_container_end_page |
90 |
_version_ |
1766027725849493504 |