Erosional-denudational valleys and their significance for the reconstruction of the Late Glacial environmental conditions (The Drawsko Lakeland, NW Poland)
Paluszkiewicz Renata
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Paluszkiewicz Renata: Institute of Geoecology and Geoinformation, Department of Geoecology, Adam Mickiewicz University, Poznań, Poland
Quaestiones Geographicae, 2011, vol. 30, issue 3, 71-81
Abstract:
The 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.
Keywords: erosional-denudational valleys; upland scarps; morphometric features; Drawsko Lakeland; West Pomerania; erosional-denudational valleys; upland scarps; morphometric features; Drawsko Lakeland; West Pomerania (search for similar items in EconPapers)
Date: 2011
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Persistent link: https://EconPapers.repec.org/RePEc:vrs:quageo:v:30:y:2011:i:3:p:71-81:n:7
DOI: 10.2478/v10117-011-0028-7
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