Results of a case study on the Warta River were presented which demonstrate climatically controlled valley floor evolution. The change in channel pattern meant also a change in valley floor development. Very flat and broad sandy-gravely bottoms formed by braided rivers were cut by better organised meandering rivers. The key profile at Żabinko shows sediments at the braided channel and organic deposits 14C dated. The dates point to bölling interstadial age. A clear differentiation in outflow direction has been fund in the vertical pattern of sedimentation from the western to northern sector. This analysis show that the bifurcation of waters ended at level of the bifurcation (III) terrace.
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