Relief of the Aran elovac municipality area

Relief of the Aran elovac municipality area was formed under the power of exogen and endogen forces. However, since the endogen shapes were largely reformed on the surface, the paper paid special attention to exogen - morphosculptural processes. Therefore, the relief types are defined according to processes that played the dominant role in exogen forming of the geological basis. Geomorphologic evolution of the relief has been tracked from the Middle Miocene until these days. The forming of shapes and the entire relief is explained by geomorphologic processes. The development and the intensity of the processes depended on geological built, climate neotectonic movements and other. In the course of the morphologic evolution of the relief, the geomorphologic process have, under the effect of climate changes and neotectonic movements, mutually exchanging and restoring multiply.