Abstract

Neolithic flint mines are well-studied in the Kraków-Częstochowa Upland. However their spatial structure and diachronic history is still poorly understood especially due to the poor preservation of the mine relief on the surface. The paper presents results of ALS data analyses conducted on the Dąbrówka-I site which is the first Prehistoric flint mine in the region that has been studied recently on the basis of the surface relief. LiDAR analyses combined with technological analyses of collected cores gave us grounds to identify two phases of flint mining at the site dated to Lengyel-Polgar cycle and Late Bronze Age-Early Iron Age. The obtained results show the extent to which a multiproxy non-destructive approach may give ground for in depth studies of flint mines.

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