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Development of the Odra River floodplain in the Ostrava Basin
2001
Geografie-Sbornik CGS
Preserved Fulltext
14C dating on 8 samples of subfossil trunks ("black oaks") indicates the Holocene age of the upper parts of the valley bottom gravel of the Odra River in the Ostrava Basin. These strata west of the town of Bohumín were redeposited during hazard floods shortly after 760 ± 70 BP.
doi:10.37040/geografie2001106020094
fatcat:i5l2oe23nfdvhpy2h3wkcurfxa