Miljevci plateau is part of the North-Dalmatian karst plateau. It's situated between Krka river, Čikola river and mountain Promina with total area of the 264,89 km2. As a part of the geomorphological analysis, morphometric and morphogenetic characteristics were distinguished. Based on calculated values of the hypsometry, slope and vertical relief dissection it’s noticed that most prominent occurrence of karst plateau is linked with the areas ranging 200-300 meters of altitude (74,93%), slope inclination 0-5° (78,27%) and plain relief and weakly dissected plains (0-30 m/km2). Further more, dolines are considered as diagnostic forms of karst. The influence of morphometric parameters on the spatial distribution of the dolines are analysed as well. A total of 286 dolines has been identified in the researched area. According to the recent investigation of doline density on territory of Croatia, this area is classified in area with very low doline density since Miljevci plateau has just 1 doline/km2. A high degree of connection among dolines and prevailing geomorphometric categories is established. Moreover, speleological objects with simple morphology and small dimensions are most frequent. Considering a type of the speleological objects, pits prevail in this area. Most speleological object are found on the plateau (56%) in the same morphometric categories as dolines. 40% of the speleological object are found in canyon of the Čikola and Krka river where caves prevails unlike the pits which are more represented on the plateau. Beside morphometric features of the terrain this paper analyses structural-morphologic and exogeomorphologic characteristics. Along karst relief, fluvial, fluvio-karst, slope and anthropogenic morphogenetic types of the relief formation are determined too.