| dc.contributor.author | Baranowska-Janota, Maria | pl_PL |
| dc.date.accessioned | 2018-12-19T12:16:42Z | |
| dc.date.available | 2018-12-19T12:16:42Z | |
| dc.date.issued | 1971 | |
| dc.identifier.citation | Rocznik Naukowo-Dydaktyczny. 1971, Z. 40, Prace Geograficzne 5, s. [115]-120 | pl_PL |
| dc.identifier.uri | http://hdl.handle.net/11716/3862 | |
| dc.description.abstract | Detritic Sarmatian measures are strongly differentiated in both vertical and horizontal directions as regards
lithology and compactness, which as a result brought about selective rock weathering. Three principal types of
weathering can be distinguished.
Further, several types of cryoturbative structures, connected with certain types of rock waste, have been observed
in Sarmatian measures.
Generally it can be stated that Sarmatian measures are resistant to large perviousness weathering; this is why the
observed cryoturbative structures are not a common phenomenon among them. | en_EN |
| dc.language.iso | pl | pl_PL |
| dc.title | Wietrzenie i zaburzenia mrozowe w stropie detrytycznych utworów sarmackich na Płaskowyżu Szanieckim i Pogórzu Szydłowskim | pl_PL |
| dc.title.alternative | Weathering and frost disturbances in the ceiling of detritic sarmatian measures in the Szaniec Table-land and Szydlow Plateau | en_EN |
| dc.type | Article | pl_PL |
