摘要：The investigated area is located along the Noteć Middle Valley and is situated on the border of several physical-geographical and geomorphologic units. There are according to Krygowski (2000): the Noteć Middle Valley, the GwdaValley, the Wałcz Lake District, the Kraina Lake District, the Chodzież Lake District. Varied geological structure and therelief of the area. The expression of dynamic activity of the last Scandinavian ice sheet are impressive ladforms like end morainehills of the Chodzież subphase, the Wyrzysk oscillation, glacial gully, outwash levels.
