TY - GEN A1 - Widera, Marek A1 - Chomiak, Lilianna A2 - Kuczyński, Tadeusz - red. PB - Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego N2 - The current research focuses on explaining the origin of end moraines running through the northernmost districts of the city of Poznań. The highest hills, that is, the Moraska Hill and the Dziewicza Hill, are a stagnation record of the Vistulian Glaciation of the Poznań Phase. These two hills represent terminal moraines of similar height and age, but the mechanism of their formation is diametrically opposed. N2 - The Dziewicza Hill is a typical accumulative end moraine, where Pleistocene deposits over 70 m thick are undisturbed. On the other hand, the Moraska Hill is a classic example of a push end moraine with a relatively thin cover of Pleistocene sediments and glaciotectonically elevated (up to 130 m a.s.l.) upper Neogene deposits. In the latter case, these strongly deformed sediments are the so-called "Poznań Clays" that underlie the Quaternary deposits in the vast area of the Polish Lowlands. L1 - http://zbc.uz.zgora.pl/repozytorium/Content/68184/ceer2019_3_widera_various.pdf L2 - http://zbc.uz.zgora.pl/repozytorium/Content/68184 KW - Pleistocene of central-western Poland KW - accumulative moraines KW - push end moraines KW - depositional processes KW - deformational processes KW - Scandinavian ice sheet KW - Plejstocen KW - Polska środkowo-zachodnia KW - moreny akumulacyjne KW - moreny pchające KW - procesy depozytowe KW - procesy deformacyjne KW - skandynawskie pokrywy lodowe KW - lodowiec skandynawski T1 - Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland UR - http://zbc.uz.zgora.pl/repozytorium/dlibra/docmetadata?id=68184 ER -