Geneza wyższych teras Pilicy w Niecce Nidziańskiej między Koniecpolem a Przedborzem

Abstract

The paper presents a geological structure of forms between Koniecpol and Przedbórz. These forms are thought to be the Pilica terraces. The deposits are different according to lithology and age. They were created mainly during the Middle Poland glaciation which covered this area. As these forms do not show any connections with longitudinal profiles of the river, therefore they were thought to be glacial, fluvioglacial and limmniglacial forms undercut by the Pilica. Part of the Pilica valley is a valley of marginal waters outflow during the Middle Poland glacier thawing.