Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej
Direction of ice advance during the Middle Polish glaciation in the northern part of the Polish JuraAn attempt is here made to interpret the ice advance of the Middle Polish glaciation in the northern part of the Polish Jura (Cracow-Częstochowa Highland). The writers investigations are based on stat...
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Faculty of Geology University of Warsaw
1967
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Online Access: | https://gq.pgi.gov.pl/agp/article/view/11467 |
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ftjgq:oai:geojournals.pgi.gov.pl:article/11467 2024-09-15T18:12:27+00:00 Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej Rózycki, Stefan Lamparski, Zbigniew 1967-09-15 application/pdf https://gq.pgi.gov.pl/agp/article/view/11467 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/11467/9954 https://gq.pgi.gov.pl/agp/article/view/11467 Acta Geologica Polonica; Vol. 17 No. 3 (1967); 369-392 Acta Geologica Polonica; Tom 17 Nr 3 (1967); 369-392 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1967 ftjgq 2024-07-30T03:29:09Z Direction of ice advance during the Middle Polish glaciation in the northern part of the Polish JuraAn attempt is here made to interpret the ice advance of the Middle Polish glaciation in the northern part of the Polish Jura (Cracow-Częstochowa Highland). The writers investigations are based on statistics concerning the percent content of local material in the 1-5 cm. fraction of moraine gravels, as determined by Z. Lamparski (1965) who showed the many-directional ice transport during the advance of the Middle Polish glaciation. The Jura ridge divided the margin of the glacier into two major lobes (the Silesian lobe and the Widawka lobe). These gradually advanced over the barrier of limestone outcrops both from the NE (the lobes of Widawka and of Koniecpol) and from the W (the Silesian lobe). The transgression of the ice sheet advancing generally from the NE to the SW and S was not completed before the final phase preceding the maximum ice transgresion in that glaciation. In addition to the distribution of local erratic boulders, the directions of ice movement are also marked by exaration forms and by glacitectonic disturbances. Article in Journal/Newspaper Ice Sheet Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
English |
description |
Direction of ice advance during the Middle Polish glaciation in the northern part of the Polish JuraAn attempt is here made to interpret the ice advance of the Middle Polish glaciation in the northern part of the Polish Jura (Cracow-Częstochowa Highland). The writers investigations are based on statistics concerning the percent content of local material in the 1-5 cm. fraction of moraine gravels, as determined by Z. Lamparski (1965) who showed the many-directional ice transport during the advance of the Middle Polish glaciation. The Jura ridge divided the margin of the glacier into two major lobes (the Silesian lobe and the Widawka lobe). These gradually advanced over the barrier of limestone outcrops both from the NE (the lobes of Widawka and of Koniecpol) and from the W (the Silesian lobe). The transgression of the ice sheet advancing generally from the NE to the SW and S was not completed before the final phase preceding the maximum ice transgresion in that glaciation. In addition to the distribution of local erratic boulders, the directions of ice movement are also marked by exaration forms and by glacitectonic disturbances. |
format |
Article in Journal/Newspaper |
author |
Rózycki, Stefan Lamparski, Zbigniew |
spellingShingle |
Rózycki, Stefan Lamparski, Zbigniew Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
author_facet |
Rózycki, Stefan Lamparski, Zbigniew |
author_sort |
Rózycki, Stefan |
title |
Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
title_short |
Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
title_full |
Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
title_fullStr |
Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
title_full_unstemmed |
Kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części Jury Polskiej |
title_sort |
kierunki ruchu lodu w czasie transgresji zlodowacenia środkowopolskiego w północnej części jury polskiej |
publisher |
Faculty of Geology University of Warsaw |
publishDate |
1967 |
url |
https://gq.pgi.gov.pl/agp/article/view/11467 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Acta Geologica Polonica; Vol. 17 No. 3 (1967); 369-392 Acta Geologica Polonica; Tom 17 Nr 3 (1967); 369-392 |
op_relation |
https://gq.pgi.gov.pl/agp/article/view/11467/9954 https://gq.pgi.gov.pl/agp/article/view/11467 |
_version_ |
1810450027153195008 |