The Cubolta catchment is located in the northern part of the Republic of Moldova, occupying a total area of940.1 km2. The geological conditions, relief, climate, hydrography, vegetation and especially the anthropogenic pressure that are encountered in this region have led to the development of geomorphological processes on large areas. The most important processes that contribute to the degradation of land within the catchment are specific to the entire hilly area between the Prut and Dniester and consist of surface erosion, gullies and landslides. To identify, map and analyze these processes, topographic maps at a scale of 1:25 000, geological maps at a scale of 1: 200 000 and orthophoto with a resolution of 0.5 m (2007 edition) were used, using MapInfo 9 and ArcGis 9.3, as well as field observations. The spatial distribution of geomorphological processes reveals their greater predominance in the upper course of the territory and shows a decrease towards the lower course. Predominant being on the right bank of the river.