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Geological maps, with the exception of the newest ones, present this part of the Třebíč Massif in the studied area incorrectly as a part of the Moldanubicum. Conspicuous Neogene tectonic forms (e. g. fault-line valleys, fault-angle valleys) were discovered in the SE marginal part of the massif. Relations between the Tertiary and the older (mainly Variscan) tectonics were studied. Regularity of spatial distribution of the most frequent durbachite forms, as low exfoliation domes, was founded.

Contribution to the geomorphology of the southernmost part of the Třebíč Massif