摘要：The geomorphology of the Dicle valley and Raman Mountain has developed under the control of the tectonic periods and fluvial periods which are belong to the Dicle River and its branches. The valley is very helpful in the enlightement of the geodynamic and geomorphological development period of the region. In the slope of the Raman anticlinal in the north of the valley structural shapes belonged to overthrused-faulted and folded struktur has been formed owing to the South Eastern joint. In this study, the geomorphological units and events which are highly affluent has been aimed to be determined and the occurence mechanisms to be explained in the Dicle River valley and Raman anticlinals.
