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Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)

Quaternary of the Morava and Dyje Rivers confluence area

 

Pavel Havlíček, Zdeněk Novák

Geoscience Research Reports 33, 2000 (GRR for 1999), pages 187–189

Full text (PDF, 0.13 MB)

 

Abstract

The aeolian sands overlying the Upper Pleistocene fluvial gravel in the valley flows both Morava and Dyje Rivers are typical of their confluence area. The characteristic dunes are dated to Late Glacial and on their surface the existence of the Mesolithic to Slavonic settlements was evidenced.