Podrobnosti záznamu

    Recent landforms evolution in the Moravian-Silesian Carpathians (Czech Republic)
    Demek, J.
    Hradecký, J.
    Kirchner, Karel
    Létal, A.
    Pánek, T.
    Smolová, I.
Typ dokumentu
    část monografie (kapitola)
Zdrojový dokument - monografie
    Recent Landform Evolution : The Carpatho-Balkan-Dinaric Region
    S. 103-139
    Autoři celkem: 6
    Rozsah: 37 s. : E82009460
Předmětová kategorie
    recent landforms evolution
    topographic changes
    Western Carpathians
Klíčové slovo
Abstrakt (anglicky)
   Topographic changes in the Moravian-Silesian Carpathians have been due to variations of natural conditions (climatic changes, accelerated rates of exogenic geomorphic processes during the Little Ice Age), but mainly to the growing intensity of human activities. In this geomorphologically highly sensitive region, land-use changes exerted a great influence on the intensity and type of exogenic geomorphological processes in the last millennium. Their impact is studied on archive maps. The density of slope deformations (like deep-seated slope failures, lateral spreading, toppling, sackung, translational and rotational landslides, earthflows, debris flows and rockfalls) in the study area is the highest in the Czech Republic. Other geomorphic processes presented in this overview are erosion by water on the surface and underground (piping), wind erosion, and a range of anthropogenic processes (urbanization, mining, industry, water management, and transport).
    AV ČR Brno, Ústav geoniky
Kód přispěvatele
    AV ČR, ÚG
Zdrojový formát
Datum importu
    20. 3. 2014