Geomorphology of the Sowie Mountains (Sudetes, SW Poland) – Landform patterns and anthropogenic impact

Author:

Migoń Piotr1ORCID,Latocha-Wites Agnieszka1ORCID,Jancewicz Kacper1ORCID

Affiliation:

1. Institute of Geography and Regional Development University of Wrocław

Abstract

The Sowie Mountains in the central part of the Sudetes range are an under-researched area in terms of geomorphology, despite their potential representativeness for a large number of terrains within the Bohemian Massif, built of metamorphic bedrock. Apart from providing an overview of past work, the paper summarizes the main topographic features of the massif using visualizations of the digital terrain model, and outlines the wide range of anthropogenic impacts on relief. Characteristic landforms of the Sowie Mountains include faultgenerated lithology-controlled escarpments, ridge-and-valley topography near the escarpments, water-divide flats, gneissic tors, agrarian terraces and various landforms related to former mining and military use.

Publisher

Institute of Geography and Spatial Organization, Polish Academy of Sciences

Subject

General Earth and Planetary Sciences,Geography, Planning and Development,Urban Studies,Cultural Studies

Reference76 articles.

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2. Aleksandrowski, P., & Mazur, S. (2002). Collage tectonics in the northeasternmost part of the Variscan belt: The Sudetes, Bohemian Massif. Geological Society Special Publication, London, 201, 237-277. https://doi.org/10.1144/GSL.SP.2002.201.01.12

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4. Aramowicz, S., Anczkiewicz, A. A., & Mazur, S. (2006). Fission-track dating of apatite from the Góry Sowie Massif, Polish Sudetes, NE Bohemian Massif: implications for post-Variscan denudation and uplift. Neues Jahrbuch für Mineralogie, Abhandlungen, 182(3), 221-229.

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