Abstract
Abstract Landslides predisposed by the anisotropy of flysch bedrock are typical features of mass movements affecting the Outer Western Carpathians. A dendrogeomorphic investigation involving an extensive dendrometric (n = 1680) survey and tree-ring analysis of 176 Norway spruce trees (Picea abies (L.) Karst.) was used to reconstruct the spatial and temporal activity of the Mazak landslide, situated in the highest part of the Czech Outer Western Carpathians. As revealed by geomorphic analysis and electrical resistivity tomography, the landslide is a translational medium-depth ( 200–300 mm per 10 days).
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