Abstract
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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