2021
DOI: 10.7163/gpol.0193
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Recent advances on geomorphology of the Gorce Mountains, the Outer Western Carpathians – state-of-the-art and future perspectives

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 landscap… Show more

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Cited by 5 publications
(7 citation statements)
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“…The Gorce Mountains, containing forests and characterized by a high degree of biodiversity, are surrounded by dense built‐up areas (Chwistek, 2006; Kurzeja, 2006). Moreover, from a geomorphological point of view the Gorce Mountains are different from other Outer Carpathian mountain belts, due to the horn‐like structure of the mountain range (Kroh & Pawlik, 2021). The area is characterized by high anthropogenic impact: it is a popular tourist destination (Popko‐Tomasiewicz, 2006), but also subject to the increasing impact of motorized vehicles.…”
Section: Methodsmentioning
confidence: 99%
“…The Gorce Mountains, containing forests and characterized by a high degree of biodiversity, are surrounded by dense built‐up areas (Chwistek, 2006; Kurzeja, 2006). Moreover, from a geomorphological point of view the Gorce Mountains are different from other Outer Carpathian mountain belts, due to the horn‐like structure of the mountain range (Kroh & Pawlik, 2021). The area is characterized by high anthropogenic impact: it is a popular tourist destination (Popko‐Tomasiewicz, 2006), but also subject to the increasing impact of motorized vehicles.…”
Section: Methodsmentioning
confidence: 99%
“…Within this mountain group, the Gorce National Park was created in 1981. The park covers an area of 70.30 km 2 , which is 12.2% of the Gorce area (Kroh & Pawlik, 2021 ).
Fig.
…”
Section: Methodsmentioning
confidence: 99%
“…Thanks to the relief described above, the massif constitutes a clear and compact barrier to the west and north-west winds dominating in the region (IMGW, 2021). The building blocks of Gorce are the Carpathian flysch formed by rootles (detached from their substratum) nappes, consisting of series of alternating marine deposits of sandstones, shales, and claystones built of clay minerals, quartz, feldspar, muscovite, and similar minerals (Golonka et al, 2021;Kroh & Pawlik, 2021). Therefore, it is not a significant source of the tested heavy metals (Bońda & Brzeziński, 2017;Cieszkowski et al, 2017;Szczęch & Cieszkowski, 2021).…”
Section: Characterization Of the Gorce Mountainsmentioning
confidence: 99%
“…ample [44,45]. The use of geometric fields of equal area and shape enables full comparability of the presented phenomena at a given level of aggregation [46].…”
Section: Study Areamentioning
confidence: 99%
“…The first method makes it possible to obtain a complete picture of the distribution of the intensity of the analyzed phenomenon in space, while the second makes it possible to trace the process of the increase in the distance of buildings from city centers. Analyses conducted with the use of a grid of primary fields make it possible to divide the space into regular smaller polygons (grids), which is not possible with the use of an administrative or cadastral division, due to the different surface areas of the divisions; it is a method used by many researchers, for example [44,45]. The use of geometric fields of equal area and shape enables full comparability of the presented phenomena at a given level of aggregation [46].…”
Section: Introductionmentioning
confidence: 99%