Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48
Geologically, sites 18 and 48 at Wojnicz are located within sub-Carpathian depression, approximately 2 km from the geological boundary with the Carpathians, and more precisely with the Skolska unit (Stupnicka 1997; Paulo et al. 2000). Geological formations which build that region include Pleistocene...
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Krakowski Zespół do Badań Autostrad
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ftjagiellonuniir:oai:ruj.uj.edu.pl:item/39479 2023-05-15T16:41:22+02:00 Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 Macroscopic identification of rock raw materials from sites 18 and 48 at Wojnicz Wasilewski, Michał 2010 http://ruj.uj.edu.pl/xmlui/handle/item/39479 pol pol Krakowski Zespół do Badań Autostrad Wojnicz 18 i 48, powiat Tarnów : osady z epoki brązu, żelaza i średniowiecza, Chochorowski, Jan, s. 325-328 978-83-916599-4-6 http://ruj.uj.edu.pl/xmlui/handle/item/39479 artykuł (rozdział w książce) 2010 ftjagiellonuniir 2019-08-30T06:09:41Z Geologically, sites 18 and 48 at Wojnicz are located within sub-Carpathian depression, approximately 2 km from the geological boundary with the Carpathians, and more precisely with the Skolska unit (Stupnicka 1997; Paulo et al. 2000). Geological formations which build that region include Pleistocene and Holocene sediments of glacifluvial, fluvial and eolian character, that is glacial gravels, sands, gravels of the Dunajec river and loesses. The Dunajec and Biała Rivers are primary sources of Carpathian gravels and sands. Identification of rock raw materials (Tables 1, 2, 3a*, 3b*, 4*) was limited to macroscopic studies and field surveys. The majority of raw materials occurs in direct vicinity of the site and is fully described in literature (e.g. Kamieński ed. 1975; Radwanek-Bąk, Bąk 1999). Conducted field survey allows concluding that a part of raw materials in the form of pebbles originates undoubtedly from the Dunajec gravels, another part comes from fluvioglacial formations mixed with sands and sandy soils from the Wojnicz region (Fig. 1), while the rest are flysh materials from the Wieliczka Foothils (Fig. 2). Analyzed assemblage encompassed approximately 3210 rock fragments, including sandstones 54.39%, quartzose sandstones/quartzites 26.62%, granites 11.50% and slates 3.80%. The remaining 4% consists of diabases, cherts, quartz pebbles, ochre, tripoli and loess. Rocks of the Scandinavian origin, which are exotic from the standpoint of geology, were brought to the analyzed area as a result of ice sheet activity. For prehistoric communities they were local materials. It can be generally declared that population inhabiting the present-day sites 48 and 18 at Wojnicz used almost exclusively locally or mezzo-locally acquired raw materials. Other/Unknown Material Ice Sheet Jagiellonian University Repository Ochre ENVELOPE(166.550,166.550,-78.233,-78.233) |
institution |
Open Polar |
collection |
Jagiellonian University Repository |
op_collection_id |
ftjagiellonuniir |
language |
Polish |
description |
Geologically, sites 18 and 48 at Wojnicz are located within sub-Carpathian depression, approximately 2 km from the geological boundary with the Carpathians, and more precisely with the Skolska unit (Stupnicka 1997; Paulo et al. 2000). Geological formations which build that region include Pleistocene and Holocene sediments of glacifluvial, fluvial and eolian character, that is glacial gravels, sands, gravels of the Dunajec river and loesses. The Dunajec and Biała Rivers are primary sources of Carpathian gravels and sands. Identification of rock raw materials (Tables 1, 2, 3a*, 3b*, 4*) was limited to macroscopic studies and field surveys. The majority of raw materials occurs in direct vicinity of the site and is fully described in literature (e.g. Kamieński ed. 1975; Radwanek-Bąk, Bąk 1999). Conducted field survey allows concluding that a part of raw materials in the form of pebbles originates undoubtedly from the Dunajec gravels, another part comes from fluvioglacial formations mixed with sands and sandy soils from the Wojnicz region (Fig. 1), while the rest are flysh materials from the Wieliczka Foothils (Fig. 2). Analyzed assemblage encompassed approximately 3210 rock fragments, including sandstones 54.39%, quartzose sandstones/quartzites 26.62%, granites 11.50% and slates 3.80%. The remaining 4% consists of diabases, cherts, quartz pebbles, ochre, tripoli and loess. Rocks of the Scandinavian origin, which are exotic from the standpoint of geology, were brought to the analyzed area as a result of ice sheet activity. For prehistoric communities they were local materials. It can be generally declared that population inhabiting the present-day sites 48 and 18 at Wojnicz used almost exclusively locally or mezzo-locally acquired raw materials. |
format |
Other/Unknown Material |
author |
Wasilewski, Michał |
spellingShingle |
Wasilewski, Michał Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
author_facet |
Wasilewski, Michał |
author_sort |
Wasilewski, Michał |
title |
Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
title_short |
Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
title_full |
Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
title_fullStr |
Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
title_full_unstemmed |
Makroskopowa identyfikacja surowców skalnych ze stanowisk Wojnicz 18 i 48 |
title_sort |
makroskopowa identyfikacja surowców skalnych ze stanowisk wojnicz 18 i 48 |
publisher |
Krakowski Zespół do Badań Autostrad |
publishDate |
2010 |
url |
http://ruj.uj.edu.pl/xmlui/handle/item/39479 |
long_lat |
ENVELOPE(166.550,166.550,-78.233,-78.233) |
geographic |
Ochre |
geographic_facet |
Ochre |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Wojnicz 18 i 48, powiat Tarnów : osady z epoki brązu, żelaza i średniowiecza, Chochorowski, Jan, s. 325-328 978-83-916599-4-6 http://ruj.uj.edu.pl/xmlui/handle/item/39479 |
_version_ |
1766031798382362624 |