A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)

In the southern part of the O´swi˛ecim Basin, in the Ko´nczyce Wielkie gravel-pit, we can find outcrops of Quaternary deposits with varied geological histories. The lower fluvial sequence is covered with glacigenic sediments. The glacigenic deposits occurring below the Brunhes-Matuyama boundary and...

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Main Authors: Foltyn, Eugeniusz, Foltyn, Edelgarda M, Jochemczyk, Leonard, Nawrocki, Jerzy, Nita, Malgorzata, Waga, Jan Maciej, Wójcik, Antoni
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
8
902
Online Access:https://kramerius.lib.cas.cz/view/uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc
id ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc
record_format openpolar
spelling ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc 2024-03-17T08:58:27+00:00 A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland) Staropaleolitické osídlení na lokalitě Kończyce Wielkie IV, Těšínsko, Polsko Foltyn, Eugeniusz Foltyn, Edelgarda M Jochemczyk, Leonard Nawrocki, Jerzy Nita, Malgorzata Waga, Jan Maciej Wójcik, Antoni https://kramerius.lib.cas.cz/view/uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc unknown https://kramerius.lib.cas.cz/view/uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc policy:public archeologie archaeology Lower Palaeolithic pebble-flake-microlithic inventory extraglacial deposits pre-Cromerian below Brunhes-Matuyama boundary 8 902 model:article ftczechacademysc 2024-02-19T22:57:32Z In the southern part of the O´swi˛ecim Basin, in the Ko´nczyce Wielkie gravel-pit, we can find outcrops of Quaternary deposits with varied geological histories. The lower fluvial sequence is covered with glacigenic sediments. The glacigenic deposits occurring below the Brunhes-Matuyama boundary and interglacial sediments are older than the Cromerian Complex. This ice-sheet advance, in its maximum extent in southern Poland, is correlated with the Günz, i.e. pre-Cromerian glaciation in Western Europe. Cultural material was located within fluvial sands with fine-grained gravels, below a layer of diamikton – interpreted as till – and underneath the boulder pavement – an equivalent of diamikton. Raw materials inventory include local flint and hornstone, foreign flint, hornstone, quartzite, opalite, gneiss granite. Among the artifacts are macrolithic and microlithic cores, flakes and tools. The pebbles, flakes and microlithic-flakes were base for making the tools. Eugeniusz Foltyn . [et al.]. Obsahuje seznam literatury Article in Journal/Newspaper Ice Sheet Czech Academy of Sciences: dKNAV Boulder Pavement ENVELOPE(161.756,161.756,-77.523,-77.523) Flint ENVELOPE(-65.417,-65.417,-67.333,-67.333)
institution Open Polar
collection Czech Academy of Sciences: dKNAV
op_collection_id ftczechacademysc
language unknown
topic archeologie
archaeology
Lower Palaeolithic
pebble-flake-microlithic inventory
extraglacial deposits
pre-Cromerian
below Brunhes-Matuyama boundary
8
902
spellingShingle archeologie
archaeology
Lower Palaeolithic
pebble-flake-microlithic inventory
extraglacial deposits
pre-Cromerian
below Brunhes-Matuyama boundary
8
902
Foltyn, Eugeniusz
Foltyn, Edelgarda M
Jochemczyk, Leonard
Nawrocki, Jerzy
Nita, Malgorzata
Waga, Jan Maciej
Wójcik, Antoni
A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
topic_facet archeologie
archaeology
Lower Palaeolithic
pebble-flake-microlithic inventory
extraglacial deposits
pre-Cromerian
below Brunhes-Matuyama boundary
8
902
description In the southern part of the O´swi˛ecim Basin, in the Ko´nczyce Wielkie gravel-pit, we can find outcrops of Quaternary deposits with varied geological histories. The lower fluvial sequence is covered with glacigenic sediments. The glacigenic deposits occurring below the Brunhes-Matuyama boundary and interglacial sediments are older than the Cromerian Complex. This ice-sheet advance, in its maximum extent in southern Poland, is correlated with the Günz, i.e. pre-Cromerian glaciation in Western Europe. Cultural material was located within fluvial sands with fine-grained gravels, below a layer of diamikton – interpreted as till – and underneath the boulder pavement – an equivalent of diamikton. Raw materials inventory include local flint and hornstone, foreign flint, hornstone, quartzite, opalite, gneiss granite. Among the artifacts are macrolithic and microlithic cores, flakes and tools. The pebbles, flakes and microlithic-flakes were base for making the tools. Eugeniusz Foltyn . [et al.]. Obsahuje seznam literatury
format Article in Journal/Newspaper
author Foltyn, Eugeniusz
Foltyn, Edelgarda M
Jochemczyk, Leonard
Nawrocki, Jerzy
Nita, Malgorzata
Waga, Jan Maciej
Wójcik, Antoni
author_facet Foltyn, Eugeniusz
Foltyn, Edelgarda M
Jochemczyk, Leonard
Nawrocki, Jerzy
Nita, Malgorzata
Waga, Jan Maciej
Wójcik, Antoni
author_sort Foltyn, Eugeniusz
title A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
title_short A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
title_full A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
title_fullStr A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
title_full_unstemmed A Lower Palaeolithic settlement at Kończyce Wielkie site 4, Cieszyn Silesian (Poland)
title_sort lower palaeolithic settlement at kończyce wielkie site 4, cieszyn silesian (poland)
url https://kramerius.lib.cas.cz/view/uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc
long_lat ENVELOPE(161.756,161.756,-77.523,-77.523)
ENVELOPE(-65.417,-65.417,-67.333,-67.333)
geographic Boulder Pavement
Flint
geographic_facet Boulder Pavement
Flint
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://kramerius.lib.cas.cz/view/uuid:ba0fbcd6-17e0-4560-b886-ca37f70e14cc
op_rights policy:public
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