TY - GEN N1 - 24 cm N2 - 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. L1 - http://www.rcin.org.pl/igipz/Content/179943/PDF/WA51_210776_r2021-t94-no1_G-Polonica-Kroh.pdf M3 - Text J2 - Geographia Polonica Vol. 94 No. 1 (2021) PY - 2021 IS - 1 EP - 67 KW - geomorphology KW - relief KW - landslides KW - hillslope processes KW - fluvial processes KW - human impact KW - biomorphodynamics A1 - Kroh, Paweł. Autor A1 - Pawlik, Łukasz. Autor PB - IGiPZ PAN VL - 94 CY - Warszawa SP - 47 T1 - Recent advances on geomorphology of the Gorce Mountains, the Outer Western Carpathians – state-of-the-art and future perspectives UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/179943 ER -