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SEDIMENTÁRNĚ-GEOLOGICKÉ STUDIUM VYBRANÝCH KVARTÉRNÍCH SEDIMENTŮ V OKOLÍ BRNĚNSKÉ PŘEHRADY
Author(s) -
Marek Mikulík,
Slavomı́r Nehyba,
František Hubatka
Publication year - 2012
Publication title -
geologické výzkumy na moravě a ve slezsku v roce .../geologické výzkumy na moravě a ve slezsku v roce ...
Language(s) - English
Resource type - Journals
eISSN - 2336-4378
pISSN - 1212-6209
DOI - 10.5817/gvms2012-1-2-030
Subject(s) - geology , colluvium , loess , outcrop , facies , fluvial , quaternary , sedimentary rock , sediment , geomorphology , geochemistry , pleistocene , sedimentary structures , aeolian processes , paleontology , alluvium , structural basin
Outcrops of Quaternary deposits are lining banks of the Brno dam. One of them is situated on the left bank ~ 250 m NW of the Osada pier. The sedimentary profile of Pleistocene deposits is composed of fluvial deposits of the Paleo – Svratka River covered by colluvial and eolian (loess) deposits. Alternation of various facies and various grain-size fractions reveals alternation of more or less arid conditions and also evolution of the surrounding landscape.

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