After the analyses, diagnosed faults were mounted on the physical map, so some morphologic features related to
faults were shown very clearly on the edge of the depression area. The most important features of these are foothills
triangle surfaces, shifted valleys, alluvial fans on the edge of the western part of depression etc. In some areas,
alluvial fans can not be noticed easily because the edge of the western part of depression is covered with settlements.
However, they are noticed very clearly in some areas, for example, between Aktepe and Hassa towns. Parallel faults
and their shaping attract attention in this area.