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The research carried out in the years 1995–98 in the area of the Złocieniec proglacial lake inclined its authors to take a broader view of the operation of proglacial basins in the Drawsko Lakeland (Paluszkiewicz 2004). Glaciolacustrine deposits in the studied lakeland area were discovered by Maksiak and Mróz in 1978. Until that time, the varved deposits at Złocieniec had not been subjected to lithological analysis. The more detailed studies conducted by the present authors in the years 2006–2007 at both Złocieniec and Wierzchowo sites with the help of geo-engineering methods allowed them to show that the two sites with varved clays in this region should be treated as separate sedimentary basins. The basins differ in thickness of varved deposits, in size, and processes responsible for the formation of the rhythmically stratified series. keywards: proglacial lake, varved clays, glaciolacustrine deposits, Drawsko Lakeland, Pomerania Ryszard Paluszkiewicz, Renata Paluszkiewicz, Adam Mickiewicz University, Instytute of Geoecology and Geoinformation, Dzięgielowa 27, 61-680 Poznań, Poland; e-mail: paluch66@amu.edu.pl, reniach@amu.edu.pl ented series of boreholes, both archival and the researcher’s own, it was found that between the glaciolacustrine clays of the Złocieniec area and those of Wierzchowo there was a transition zone where glaciolacustrine deposits passed into fluvioglacial ones represented by sands (Fig. 1). The research made possible to state that the area of clays around the town of Wierzchowo could be a separate proglacial basin. In the years 2006–2007 a research was made under grant no. 0562/PO4/2005/29 concerning LITHOFACIES-GENETIC CHARACTERISTICS OF SEDIMENTARY bASINS IN THE FORELAND OF THE POMERANIAN STAGE IN THE DRAwSKO LAKELAND... 62 ryszard PaluszkiewiCz, renata PaluszkiewiCz a possible use of the static cone penetration test (CPTU) to analyse the stratigraphy of Cainozoic deposits (Wierzbicki et al. 2007). The study area included also the Złocieniec and Wierzchowo proglacial lakes (the Drawsko Lakeland). That allowed the researchers to make a detailed characterisation of the deposits filling the Wierzchowo (Wierzbicki et al. 2011) and the Złocieniec basins (Paluszkiewicz et al. 2007). The aim of this paper is to present the lithogenetic dissimilarity of the Złocieniec and Wierzchowo proglacial lakes, and thus to show that they should be considered as separate sedimentary basins.

Lithofacies-genetic characteristics of sedimentary basins in the foreland of the Pomeranian Stage in the Drawsko Lakeland (northern Poland)