Abstract
The flint mine in Bębło is situated in the Ojców Upland within the Olkusz Upland, above the Kluczwoda, Bolechówka and Bębłówka river valleys. Its vast mining field lies on a slope of a crest facing south-east, rising above a small valley, now dry but once crossed by a watercourse, to a height of approx. 30 metres. In the late 5th millennium BC, irregular flint concretions were extracted there through small shallow pits located one next to the other and reaching the bottom of karst karren. The nature, function and relative chronology of Site 4 in Bębło are crucial to the analysis of flint mining and reduction techniques in southern Poland in the middle phase of the Lengyel culture. They can also prove useful in tracing the relationship between the local technological changes and the influx of new ideas linked with the “second stage of the Neolithization in the Polish territories”.
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