Search for: [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."]

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