This thesis studies and presents the geomorphological setting of the Pleistocene river terrace Udin boršt, located in the northwestern part of the Ljubljana basin. In order to achieve said purpose the following aims were set: examining pertinent literature and cartographic material, delineating the studied area, conducting a morphographic analysis and synthesizing the findings. The formation of the relief was influenced by different geological bases and their intertwining, as well as an autogenous water inflow. Karst landforms along with fluvial landforms developed on the permeable carbonate conglomerate, fluvial landforms developed on the impermeable clay, contact karst landforms developed on the contact of karstic and non-karstic rock, while fluviokarst formed on a thick layer of regolith. The main result of the thesis is a morphographic map, which shows the identified landforms of the studied area.
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