Szukana fraza: [Abstract = "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."]

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