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ZNALEZISKO SIEKIER KRZEMIENNYCH Z KLEMENTOWIC (PŁASKOWYŻ NAŁĘCZOWSKI) – DYLEMAT Z AFILIACJĄ KULTUROWĄ

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Libera J., Mączyński P., Sałacińska B., Sałaciński S.
Archeologia Polski
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2019
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vol. 64
157-203
EN
The subject of the study is a collective find of three axes discovered in 1964 during excavation research at the multicultural site VII in Klementowice, Kurów commune, Puławy dis-trict, Lublin voivodeship, in the north-western part of the Nałęczów Plateau. Two artefacts (with quadrilateral section and bifacial) are made of banded flint and one (with quadrilateral section) – of Świeciechów flint. These raw materials come from deposits exploited in the Neolithic period in mines of the Świętokrzyski region of the prehistoric flint mining. Despite the existing doubts, these axes should be combined with the Funnel Beaker culture, its southeastern group.
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Etapy rozwoju osadnictwa zachodniej części Płaskowyżu Nałęczowskiego i ich zapis w osadach dna Doliny Bystrej

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Reder J., Superson J., Król T.
Annales Universitatis Paedagogicae Cracoviensis Studia Geographica
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2010
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vol. 1 Dynamika zmian środowiska geograficznego pod wpływem antropopresji
126-136
EN
The article analyzed the impact of old (prehistoric, medieval) and modern settlement on the nature of the Holocene alluvial sediments at the bottom of the Bystra valley. It was shown that the transition from peat to mineral deposits was the result of Neolithic farming. Nomadic culture of the late Neolithic and early Bronze Age have helped to stop the denudation slope sand increasing erosion in the bottom of the river valley. Restarting the denudation in the basin and the beginning of accumulation on the Bystra floodplain occurred only in the tenth century. Bystra river basin deforestation in modern times caused catastrophic linear erosion, denudation slopes and speed up the submission of anthropogenic alluvial soils.
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