Geografie 2000, 105, 347-360

https://doi.org/10.37040/geografie2000105040347

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

Martin Brzák

Katedra geografie, Přírodovědecká fakulta MU, Kotlářská 2, 611 37 Brno, Czechia

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.

Funding

Výsledky publikované v tomto článku byly získány během geomorfologického výzkumu okolí lokality miocénních sedimentů u Hostimi v rámci grantu GA ČR 205/98/P280.

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