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The article analyses the southern part of the expansion of the Bzura–Ner Spillway (Bzura–Ner 3UDGROLQD FDOOHGWKH.RáR%DVLQDVZHOODVQHLJKERXULQJDUHDVRIWKHàDVN8SODQG3ODLQDQGWKH Turek Upland Plain. The purpose of the study was to present the role of Pleistocene glaciations, HVSHFLDOO\WKH:DUWD*ODFLDWLRQDQGLQSDUWLFXODUWKHLUUROHLQWKHHYROXWLRQRIODQGUHOLHILQWKLV area. It was noted that morphological activity of continental glaciers depended on morphology, lithology and dynamics of the bedrock. Special attention was paid to effects characteristic of the transgression and disappearance of the Warta ice sheet. A survey of geological and geomorphologi-cal literature, analyses of archival data, mainly the accounts of geologigeomorphologi-cal drillings as well as results of geomorphological and palaeogeomorphological research constitute the basis for the presented data and views.
It was found that successive continental glaciers had reduced height differences of the Pleis-tocene bedrock without obliterating the main forms in the area. Despite the genetic diversity of forms, postglacial forms and sediments – which emerged during the glaciation of the Warta
(the last glaciation in this area) – play a predominant part in the described area. The features of JODFLDOWLOOVDQGÀXYLRJODFLDODQGOLPQRJODFLDOVHGLPHQWVZKLFKIRUP:DUWLDQPRXQGVKLOOVDQG ridges prove that at the end of the Warta glaciation, during deglaciation (in the Bzura sub-phase), WKHG\QDPLFVRIJODFLDOSURFHVVHVZDVLQWHQVL¿HG$FFXPXODWLRQRILFHLQWKHORZHUSDUWRIWKH FXUUHQW.RáR%DVLQZDVFRQGXFLYHWRLQFUHDVHGG\QDPLFVRIWKHLFHOREHWKURXJKRVFLOODWLRQV and, possibly, through glacial surges. However, activity of the ice sheet edge has been blurred as a result of areal deglaciation, which is documented by numerous kames – the most widespread convex glacial forms in the area.
