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 Slls in the West Sudetes as well as the adjacent fore-mountain area. The legacy of several periods of volcanic activity in the Paleozoic and Cenozoic is the most distinctive component of regional geoheritage and finds its geomorphic expression in the occurrence of hills and ridges built of more resis

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使成核

The Stołowe Mountains—A Unique Sandstone Tablelandve the surrounding terrains by some 450 m. Albeit quite small in terms of spatial extent, the mountain range showcases a number of interesting geomorphic features, including prominent mesas and plateaus, rock labyrinths, pedestal rocks, solitary boulders and sandstone canyons. Since the morphology o

agglomerate

Cultural Geomorphological Landscapes of the East Sudetescan be considered as representative for the Sudetes, which exemplify a mid-latitude, medium-altitude mountain range distinguished by a high degree of human impact on the geomorphological system due to a great variety of economic activities carried out in the past and now. Human impact on topography

hereditary

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The Tatra Mountains—Host of the Deepest Caves in the Carpathianshe Wielka Śnieżna Caves System. Cave evolution started at the end of the Miocene and is related to the Tatras’ asymmetrical uplift and, during the Pleistocene, to the existence of mountain glaciers. Karst in the Tatras is strongly controlled by fold-and-thrust setting, which influences both undergro

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等级的上升

Dunajec River Gorge Through the Pieniny Mountainsysis of the Digital Terrain Model (DTM), indicate that the Dunajec River Gorge in the Pieniny Mts. (called also the Pieniny Gorge) is regressive and structural. The Dunajec River, originally flowing along the northern margin of the Pieniny Mts., was intercepted due to river piracy by the Niedziczank