| dc.contributor.author | Cabaj, Wacław | pl_PL |
| dc.date.accessioned | 2020-04-02T13:17:46Z | |
| dc.date.available | 2020-04-02T13:17:46Z | |
| dc.date.issued | 1991 | |
| dc.identifier.citation | Rocznik Naukowo-Dydaktyczny. 1991, Z. 142, Prace Geograficzne 13, s. 73-90 | pl_PL |
| dc.identifier.uri | http://hdl.handle.net/11716/7085 | |
| dc.description.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. | en_EN |
| dc.language.iso | pl | pl_PL |
| dc.title | Geneza wyższych teras Pilicy w Niecce Nidziańskiej między Koniecpolem a Przedborzem | pl_PL |
| dc.title.alternative | Upper terraces of the Pilica in the Nida Basin between Koniecpol and Przedbórz | en_EN |
| dc.type | Article | pl_PL |
