Paluszkiewicz, Renata2016-11-212016-11-212011Quaestiones Geographicae vol. 30 (3), 2011, pp. 71-81978-83-62662-62-30137-477Xhttp://hdl.handle.net/10593/15639The article presents the morphological-lithological development and operation of dry erosional-denudational valleys located on morainic uplands in the Drawsko Lakeland. A detailed research was carried out on the morainic upland of the Buślarka and Piaski Pomorskie area. A geodetic study made it possible to identify over ten NW-SE and N-S oriented erosional-denudational valleys, clearly marked in the relief. They are small landforms: their length does not exceed 100 m, and the depth of incision reaches 4 m. Their exact morphometric description with the help of GIS methods and a detailed study of lithofacies characteristics of their deposits provided an insight into their operation. They follow a Late Glacial pattern in which Late Vistulian erosion only rejuvenated the already existing older forms.enginfo:eu-repo/semantics/openAccesserosional-denudational valleysupland scarpsmorphometric featuresDrawsko LakelandWest PomeraniaErosional-denudational valleys and their significance for the reconstruction of the Late Glacial environmental conditions (the Drawsko Lakeland, NW Poland)Artykuł