@misc{Kroh_Paweł._Autor_Recent_2021,
 author={Kroh, Paweł. Autor and Pawlik, Łukasz. Autor},
 volume={94},
 number={1},
 copyright={Creative Commons Attribution BY 4.0 license},
 address={Warszawa},
 journal={Geographia Polonica},
 howpublished={online},
 year={2021},
 publisher={IGiPZ PAN},
 language={eng},
 abstract={The increase of geomorphological research during the last decades in the Gorce Mts. caused the need for state-of-art review papers. The Gorce Mountains were formed as an isolated massif with Mt Turbacz (1310 m a.s.l.) as the highest summit. River channels are remodeled by sudden and high-level floods with the critical impact of log jams. The main processes influencing hillslope relief were landsliding, run-off, and tree uprooting. The review suggests the following issues await for studies: a long-term landscape evolution, monitoring of morphogenetic processes, and origin of landslides with their contribution to denudation rates. Also, current biomorphodynamics (uprooting process) has not been sufficiently studied.},
 type={Text},
 title={Recent advances on geomorphology of the Gorce Mountains, the Outer Western Carpathians – state-of-the-art and future perspectives},
 URL={http://www.rcin.org.pl/igipz/Content/179943/PDF/WA51_210776_r2021-t94-no1_G-Polonica-Kroh.pdf},
 keywords={geomorphology, relief, landslides, hillslope processes, fluvial processes, human impact, biomorphodynamics},
}