Paleogeograficzne tło rozwoju doliny w Załęczańskim Łuku Warty (Wyżyna Wieluńska)

Abstract

The author describes the relief and geological structure of the Warta valley in its river gap across the Wieluń Upland, being 43 km long. There is underlined an interesting geological history of this area reflected in the fluvia land karst relief and in a complicated system of under ground and surface water circulation (for summary see page 176-178).