EN
Investigations carried out in the Vistula River valley in the vicinity of Magnuszew (middle course) have shown the complexity of distribution of flood facies deposits. The type of lithological profile as well as sorption properties depends on site location in distinguished morphogenetic zones of floodplain: (1) terrace zone of meandering Vistula reworked by contemporary flows, (2) erosion troughs, (3) alluvial fans (crevasses), (4) contemporary terrace.