With the continuous acceleration of urbanization, the impact of human activities on geological hazards has gradually increased, and people's lives and property safety have been threatened. Controlling geological hazards cannot delay. In this paper, nine factors such as slope gradient, relative elevation difference, slope direction, slope type, engineering geology groups, geomorphic type, rainfall, distance from rivers and distance from major traffic arteries are selected as evaluation indicators. The Information Value Model is used to evaluate the geological hazards susceptibility. The results show that: (1) This County can be divided into four types: extremely high susceptibility, high susceptibility, medium susceptibility and low susceptibility. Low susceptibility type is the largest, accounting for 64.64%, and extremely high susceptibility type is the smallest, accounting for 0.39%. (2) According to the verification, it can be seen that the density of geological hazards points in the extremely high areas and high areas is higher than that in medium susceptibility and low susceptibility areas, and the results are reasonable.

geological hazards  /  susceptibility evaluation  /  the Information Value model  /  the hinterland of the Loess Plateau