The geological structures in the study area are dominated by faults. The rest diredtions of the faults are northeast soutwest (16 faults) and north south ( 14 faults). The remainder of raults are trending in northwest -southeast ( 3 Faults.) and west -east (3 faults) directions. Generally, the northeast- southwest and northeast -southwest and north south trending faults are dominated by sinitral faults and a few of them are reactivated as normal faults. Whereas the northwest- southeast and west- -east trending fouts are mainly dextral and or normal faults.