The origin of drumlins at Zbójno, Central Poland
Drumlins at Zbójno, Dobrzyń Lakeland, are located in a channel-like terminal basin, in the proximal part of the Chrostkowo end moraines. A fragment of the drumlin field was examined in detail. The drumlins are elongated ridges, parallel to one another and to the basin margins. Their orientation is p...
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ftlitinstagrecon:oai:elaba:5851441 2023-05-15T16:40:59+02:00 The origin of drumlins at Zbójno, Central Poland Drumblinų prie Zbójno (Vidurio Lenkija) kilmė Głębicki, Piotr Marks, Leszek 2009 http://lmavb.lvb.lt/LMAVB:ELABAPDB5851441&prefLang=en_US lit eng lit eng info:eu-repo/semantics/altIdentifier/doi/10.2478/v10056-009-0014-0 http://lmavb.lvb.lt/LMAVB:ELABAPDB5851441&prefLang=en_US Geologija, 2009, Vol. 51, no. 3/4 (67/68), p. 131-138 ISSN 1392-110X Drumlins Georadar Pleistocene Poland info:eu-repo/semantics/article 2009 ftlitinstagrecon https://doi.org/10.2478/v10056-009-0014-0 2021-12-02T00:15:40Z Drumlins at Zbójno, Dobrzyń Lakeland, are located in a channel-like terminal basin, in the proximal part of the Chrostkowo end moraines. A fragment of the drumlin field was examined in detail. The drumlins are elongated ridges, parallel to one another and to the basin margins. Their orientation is parallel to perpendicular with regard to the presumed regional direction of the ice sheet advance. The drumlins' geological structure is tripartite, including a lower till, a glaciofluvial core and a covering upper till. Georadar examination indicated the presence and extension of glaciotectonic deformations of the lower till. It is squeezed up to 3 m above its primary setting and forms protodrumlins that have not been, however, the bed bumps that stimulated a lee-side deposition. Protodrumlins are usually absent along a drumlin axis, but they occur also in pairs. They could both initiate but also terminate drumlin development when thawing appeared in the subglacial zone and the ice body was disintegrated into dead-ice blocks. Glaciofluvial cores are less deformed than the lower till: their sediments are stratified, but commonly uplifted towards a protodrumlin. Article in Journal/Newspaper Ice Sheet LAEI VL (Lithuanian Institute of Agrarian Economics Virtual Library) Geologija 51 3 131 138 |
institution |
Open Polar |
collection |
LAEI VL (Lithuanian Institute of Agrarian Economics Virtual Library) |
op_collection_id |
ftlitinstagrecon |
language |
Lithuanian English |
topic |
Drumlins Georadar Pleistocene Poland |
spellingShingle |
Drumlins Georadar Pleistocene Poland Głębicki, Piotr Marks, Leszek The origin of drumlins at Zbójno, Central Poland |
topic_facet |
Drumlins Georadar Pleistocene Poland |
description |
Drumlins at Zbójno, Dobrzyń Lakeland, are located in a channel-like terminal basin, in the proximal part of the Chrostkowo end moraines. A fragment of the drumlin field was examined in detail. The drumlins are elongated ridges, parallel to one another and to the basin margins. Their orientation is parallel to perpendicular with regard to the presumed regional direction of the ice sheet advance. The drumlins' geological structure is tripartite, including a lower till, a glaciofluvial core and a covering upper till. Georadar examination indicated the presence and extension of glaciotectonic deformations of the lower till. It is squeezed up to 3 m above its primary setting and forms protodrumlins that have not been, however, the bed bumps that stimulated a lee-side deposition. Protodrumlins are usually absent along a drumlin axis, but they occur also in pairs. They could both initiate but also terminate drumlin development when thawing appeared in the subglacial zone and the ice body was disintegrated into dead-ice blocks. Glaciofluvial cores are less deformed than the lower till: their sediments are stratified, but commonly uplifted towards a protodrumlin. |
format |
Article in Journal/Newspaper |
author |
Głębicki, Piotr Marks, Leszek |
author_facet |
Głębicki, Piotr Marks, Leszek |
author_sort |
Głębicki, Piotr |
title |
The origin of drumlins at Zbójno, Central Poland |
title_short |
The origin of drumlins at Zbójno, Central Poland |
title_full |
The origin of drumlins at Zbójno, Central Poland |
title_fullStr |
The origin of drumlins at Zbójno, Central Poland |
title_full_unstemmed |
The origin of drumlins at Zbójno, Central Poland |
title_sort |
origin of drumlins at zbójno, central poland |
publishDate |
2009 |
url |
http://lmavb.lvb.lt/LMAVB:ELABAPDB5851441&prefLang=en_US |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geologija, 2009, Vol. 51, no. 3/4 (67/68), p. 131-138 ISSN 1392-110X |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.2478/v10056-009-0014-0 http://lmavb.lvb.lt/LMAVB:ELABAPDB5851441&prefLang=en_US |
op_doi |
https://doi.org/10.2478/v10056-009-0014-0 |
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Geologija |
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51 |
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3 |
container_start_page |
131 |
op_container_end_page |
138 |
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1766031414291070976 |