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the Obręczówka and the Przepaść river valleys located in the north fragment of the Sandomierz Upland (Kondracki 2001) belong to those areas where numerous archeological excavations have been carried out for a long time (Podkowińska 1961; żaki 1972; bąbel 1975; Kowalski 1975; Uzarowiczowa 1975; Uzarowicz -Chmielewska 1979; bąbel 1998; balcer 2002; Orzechowski 2007; Jedynak, Kaptur 2008; Kaptur 2010; Przeździecki et al. 2011; Orzechowski 2013; Kaptur 2014) (Fig. 1). the settlement development within the border between the Sandomierz Upland and the iłża Foreland, lasting, with breaks, from the Paleolithic period, resulted in the cultural diversification of archeological sites. Within the above-mentioned river catchment areas, settlement development was connected mainly with easy access to water, fertile soils derived from loess (in the case of the Przepaść river – chernozems), geology of the region (flint outcrops) and configuration of the land (defensive function of sites). Department of General Geology and Geotourism, Faculty of Geology, Geophysics and environment Protection, aGh University of Science and technology 30-059 Kraków, al. Mickiewicza 30, Poland; egalka@agh.edu.pl

annales universitatis mariae curie-skłodowska. sectio b, geographia, geologia, mineralogia et petrographia

The Main Phases of Settlement Development in the North Fragment of the Sandomierz Upland and their Sedimentological and Palynological Record in the Sediments of the Bottom of the Obręczówka River Valley