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The Pleistocene soft rock pediments in the Central Moravian Carpathians developed due to different geomorphic processes. At a locality situated between Nesovice and Brankovice villages, it was mainly downwearing of the former river terrace and the underlying Lower Miocene strata due to development of a small flat, at present dry valleys (dells). At Slavkov u Brna (Austerlitz), in turn, the leading process affecting the same sediments as at the previous locality consisted in the recession of the northern valley side of the Litava River. The main reason for the development of the lower segment of the pediment at Slavkov u Brna in the contact zone with the Litava River terrace was surface runoff. The present appearance of the pediments at both localities is an effect of periglacial processes active in the Middle and mainly Late Pleistocene. Thus, the same landforms (pediments) developed in comparable geologic and climate conditions due to different processes caused by local geomorphic factors.

Two different modes of the origin of Pleistocene pediments: an example from the Central Moravian Carpathians, Czech Republic