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The aim of this paper is to give information on the research of the present exogenic morphogenetic processes in the Ďumbier Tatra Mts which are part of the Low Tatra Mts. In the article the author presents a brief outline of the geomorphological conditions of the Ďumbier Tatra Mts, classification of processes taking part in a contemporary morphogenesis of the above mountains and an outline of their extension. In the conclusion, the author describes processes characteristic of the individual geoecological types of the area under invertigation.

The present-day exogenic morphogenetic processes in the Ďumbier Tatra Mts