Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland)
The Biśnik Cave is located near the town of Pilica in the central part of the Smoleń-Niegowonice Range (Cracow-Częstochowa Upland). During archaeological excavations a section of clastic sediments above 7 m thick was exposed. Based on sedimentological, mineralogical and archaeological data, the lith...
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ftjgq:oai:geojournals.pgi.gov.pl:article/10067 2024-09-15T18:39:50+00:00 Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) Mirosław-Grabowska, Joanna 2003-09-01 application/pdf https://gq.pgi.gov.pl/agp/article/view/10067 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/10067/8597 https://gq.pgi.gov.pl/agp/article/view/10067 Acta Geologica Polonica; Vol. 52 No. 1 (2002): Climate Changes – The Karst Record; 97-110 Acta Geologica Polonica; Tom 52 Nr 1 (2002): Climate Changes – The Karst Record; 97-110 Cave sediments Cracow-Częstochowa Upland Quaternary info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2003 ftjgq 2024-07-30T03:29:09Z The Biśnik Cave is located near the town of Pilica in the central part of the Smoleń-Niegowonice Range (Cracow-Częstochowa Upland). During archaeological excavations a section of clastic sediments above 7 m thick was exposed. Based on sedimentological, mineralogical and archaeological data, the lithology and stratigraphy of the deposits were documented. Series I (layers 18-8) accumulated in a dry cave environment in the Tertiary (layer 18), during the Middle Polish Glaciation (layers 17-14), the Eemian Interglacial (layers 13-12) and in the older part of the Vistulian (layers 11-8). Series II (layers 7-5) reflects accumulation under fluvial conditions during the Middle Vistulian. Series III (layers 4-2) consists of aeolian deposits accumulated during the Upper Vistulian. The humus layers (layers 1b-1a) were formed during the Holocene. The composition of the rich palaeontological material was used for reconstruction of the natural environment and the climatic conditions during the accumulation of the sediments. The existence of forest is documented during the time of the accumulation of layers 15, 13, 12. The presence of aquatic species of fauna testifies to the existence of a small river in the neighbourhood of the cave (e.g. layers 11, 6-7). The high proportion of remains of steppe-tundra fauna indicates a periglacial environment (e.g. layers 14, 8, 2). The results of the investigations of the BiÊnik Cave sediments helped in reconstructing the evolution of the relief of the surrounding area. Article in Journal/Newspaper Tundra Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
English |
topic |
Cave sediments Cracow-Częstochowa Upland Quaternary |
spellingShingle |
Cave sediments Cracow-Częstochowa Upland Quaternary Mirosław-Grabowska, Joanna Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
topic_facet |
Cave sediments Cracow-Częstochowa Upland Quaternary |
description |
The Biśnik Cave is located near the town of Pilica in the central part of the Smoleń-Niegowonice Range (Cracow-Częstochowa Upland). During archaeological excavations a section of clastic sediments above 7 m thick was exposed. Based on sedimentological, mineralogical and archaeological data, the lithology and stratigraphy of the deposits were documented. Series I (layers 18-8) accumulated in a dry cave environment in the Tertiary (layer 18), during the Middle Polish Glaciation (layers 17-14), the Eemian Interglacial (layers 13-12) and in the older part of the Vistulian (layers 11-8). Series II (layers 7-5) reflects accumulation under fluvial conditions during the Middle Vistulian. Series III (layers 4-2) consists of aeolian deposits accumulated during the Upper Vistulian. The humus layers (layers 1b-1a) were formed during the Holocene. The composition of the rich palaeontological material was used for reconstruction of the natural environment and the climatic conditions during the accumulation of the sediments. The existence of forest is documented during the time of the accumulation of layers 15, 13, 12. The presence of aquatic species of fauna testifies to the existence of a small river in the neighbourhood of the cave (e.g. layers 11, 6-7). The high proportion of remains of steppe-tundra fauna indicates a periglacial environment (e.g. layers 14, 8, 2). The results of the investigations of the BiÊnik Cave sediments helped in reconstructing the evolution of the relief of the surrounding area. |
format |
Article in Journal/Newspaper |
author |
Mirosław-Grabowska, Joanna |
author_facet |
Mirosław-Grabowska, Joanna |
author_sort |
Mirosław-Grabowska, Joanna |
title |
Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
title_short |
Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
title_full |
Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
title_fullStr |
Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
title_full_unstemmed |
Geological value of Biśnik Cave sediments (Cracow-Częstochowa Upland) |
title_sort |
geological value of biśnik cave sediments (cracow-częstochowa upland) |
publisher |
Faculty of Geology University of Warsaw |
publishDate |
2003 |
url |
https://gq.pgi.gov.pl/agp/article/view/10067 |
genre |
Tundra |
genre_facet |
Tundra |
op_source |
Acta Geologica Polonica; Vol. 52 No. 1 (2002): Climate Changes – The Karst Record; 97-110 Acta Geologica Polonica; Tom 52 Nr 1 (2002): Climate Changes – The Karst Record; 97-110 |
op_relation |
https://gq.pgi.gov.pl/agp/article/view/10067/8597 https://gq.pgi.gov.pl/agp/article/view/10067 |
_version_ |
1810484182961356800 |