Primary core of Germi has been developed on the relative flat topographic space, but due to the land limitations, these days, this town is frequently (over 70%) developing in the high steep slopes (8 to 30 degrees). Active faults of the region and the presence of unresisting superficial and deposits and geological formations have caused instability of the urban constructions formation especially in the east and north east of this small city. In addition, the subsidence phenomena and cracks in foundations, due to deposit silts with the high percentage of clay and with high shear steers, have seriously threatened urban constructions. The large land slide in the 1995 destroyed some about the 250 residuals, hospitals and schools in the eastern slope of the town in the Katol district which led to obligatory replacing of some residuals. According to the research findings, out of whole urban land use (449.4 ha), 145.5 of them (32.4%) is located in the unsuitable to completely high risk zones. Therefore, occurrence of any earthquake stronger than 5.5 with Richter Scale, landslides, subsidence phenomena, subsidence liquefactions, and environmental hazards of geomorphic phenomena, result in crakes, movement and instability of soil formation, and the destruction of the constructions in the slopes.