The purpose of this thesis is geomorphological analysis of Dobrepolje and the Rašica river basin. Intermediate goals include reviewing and examining the literature, delimiting the area and geomorphological analysis, which will include morphographic, morphometric, and morphostructural analysis. The final goal of the assignment is defined as a morphogenetic interpretation based on the analytical part of the research and the selected literature. The objective of geomorphological analysis was achieved based on a combination of geomorphological analytical methods. The main result of the geomorphological analysis are morphography, morphometry, and morphostructure of the Dobrepolje and Rašica river basin. The main conclusion of the thesis is that the eastern part of the studied area is dominated by the karst genetic type of relief, while in the western part of the studied area a fluviokarst relief type is formed. Only a small part of the Rašica river basin is formed by fluvial relief type. From the hydrological point of view, Dobrepolje shows hydrological duality in its northern part. At normal water levels, it acts as a dry karst field without surface watercourses. Only at extreme high waters it acts as a border karst field.
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