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Tectonic denudation concept of Lublin Upland morphogenesis using the example of Giełczew Heights

Superson Józef, Reder Jan, Demczuk Piotr

Studia Geomorphologica Carpatho-Balcanica

2019/2020

Vol. 53/54

137--151

Land surface development at Giełczew Heights (central part of the Lublin Upland), especially denudational forms, has interested researchers since the 1950s due to its representativeness of the entire region. First, two planation levels and one valley level were separated. At a later stage of the study, more than three stacked levels were identified. Previous studies have proven that the denudational relief of Giełczew Heights is dependent on disjunctive tectonics. Numerous fault zones formed during the Paleogene and Neogene, which divided territories into several tectonic blocks of different rank, size and absolute height. Notably, this observation suggests a multitude of planation surfaces. Additionally, tectonic movements in the Early Pleistocene formed Giełczew Heights as an independent geomorphological region and strengthened the late Pliocene collocation of river valleys that has survived into the modern era.