Abstract
The distinctive sandy structure of Prokopiak’s Mount in Opatowice stands out from the surrounding black soils of the Kujawy Upland, and therefore attracted the interest among the Late Neolithic communities of the region. A program of comprehensive archaeological research was conducted here in 1985-1998, eleven sites were investigated and the materials obtained from five of them were published. These sites all produced rich flint assemblages.Three of these assemblages, being relatively homogeneous, (Opatowice 33, 36 and 42), were selected for research on the formation of local traditions of flint production in the Late Neolithic in Kujawy. The presented assemblages cover the entire chronological span from3650 BC to 2600 BC. And chronologically correspond to the classic Wiórek horizon (Opatowice 33), the Luboń-Radziejów horizon (Opatowice 42) and the classic GAC horizon (Opatowice 36).
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