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In water bodies of the Upper Silesia and D?browa Basin region (Southern Poland), shore processes should be considered on a micro scale owing to the small area of these lentic water bodies, especially when compared to large bodies of water around the world. Intensive geomorphological changes manifest themselves as abrasional forms (e.g. cliffs, terraces), which are found in small numbers on the banks of reservoirs impounded by dams and are more numerous within flooded mineral workings. On the other hand, accumulati...