Titlebook: Landscapes and Landforms of Poland; Piotr Migoń,Kacper Jancewicz Book 2024 The Editor(s) (if applicable) and The Author(s), under exclusiv

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Land of Extinct Volcanoes—Rock-Controlled Landforms, Postglacial Gorges, and Faulted Margin of the Snerated marginal escarpment of the Sudetes. The pending application for the status of a UNESCO Global Geopark reflects both the international dimension of regional geoheritage and the considerable involvement of local communities to promote tourism based on geoscience-related values.

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The Sto?owe Mountains—A Unique Sandstone Tableland of processes working at depth, which are thought to have primarily contributed to the non-catastrophic evolution of cliff lines and the development of ruiniform relief, has been recognized. The outstanding natural beauty of the area resulted in a long history of tourism development within the time

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Cultural Geomorphological Landscapes of the East Sudeteshe diversity of anthropic landforms of various age according to their origin related to various economic activities such as agriculture, forestry, settlement, mining, quarrying, industry, and water management. The section on indirect human impact includes a discussion on anthropogenic modification o

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Mount ?l??a—The Highest Inselberg in the Sudetic Foreland and Its Glacial-Periglacial Morphogenesiseet and the influence of the periglacial environment. During the maximum extent of the inland glaciation the hilltop of Mt. ?l??a remained as a nunatak, but glacial erosion occurred on the lower slopes. In the younger phase of the Saalian glaciation and during the Weichselian glaciation, the slopes

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Mt. Babia Góra—The Highest Flysch Ridge in the Western Carpathiansslope and the gentle southern slope (penestructural slope). The upper part of the northern slope, where gradients exceed 40° and locally reach 70°, features elements of glacial and nival relief, remodelled landslide forms, periglacial covers, as well as couloirs, torrential fans, and debris flows, w

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Tatra Mountains—The Only High-Mountain Landscape in Polandations which are only preserved locally in the High Tatra Mountains. The Tatra Mountains with patches of discontinuous permafrost and perennial firn-ice patches (glacieretes) are the only area with the present-day periglacial phenomena in Poland. Nevertheless, all rock glaciers are there relict, inh

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Hills, Gravelly Floodplains and Peat Bogs of the Podhale—A Unique Landscape Mosaic Between the Tatrasive, and now fragmented peatland on the basin floor. Finally, human impacts have led to the transformation of fluvial systems which now span an unusual range of river styles from island- and bar-braided morphologies functioning in relatively natural manner to regulated and incised, bedrock channels

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Dunajec River Gorge Through the Pieniny Mountainsotwall elevation phenomenon, had a significant impact on the formation of high walls of the gorge. The Dunajec River Gorge through the Pieniny Mts. is therefore not strictly antecedent, related to the elevation (.) of the mountain massif transversely cut by the river, but connected with the selectiv

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2213-2090 eographers and Quaternary geologists, but will be also of interest to anyone interested in natural landscapes and their conservation.978-3-031-45764-7978-3-031-45762-3Series ISSN 2213-2090 Series E-ISSN 2213-2104