Abstract

The georelief segments in the upper part of the drainage basin of the Suchý potok (Dry Creek) are defined on the basis of field mapping (map of land-use and present-day geomorphic processes and computation of the potential water soil erosion). Each segment is characterized by the use of the georelief (I-IV), dominant geomorphic process (1-11) and the value of the potential water soil erosion (A-C). Individual georelief segments are evaluated from the point of view of their economic use.

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