Following the ’8.8’ earthquake, many geological hazards, including landslides and collapses, are dispersed around the Jiuzhai gully. Susceptibility evaluation has been demonstrated to assist in reducing the chance of hazards and social and financial losses when developing mitigation plans for geological hazards, which are essential for risk management and hazard prevention. After the earthquake, as vegetation continues to recover, the temperature and precipitation fluctuate periodically, leading to regular changes in the amount and scale of geological hazards. We generated the geological hazards susceptibility mapping of Jiuzhai gully after the earthquake based on the variation trend slope of precipitation and vegetation, CIM-ANN, and CIM-LR ensemble models. The results of this research were validated using the area under the curve (AUC) and proportion. The study showed that, when comparing the CIM-LR and CIM-ANN, the AUC is 0.94 and 0.937, the accumulative cover area proportion of the geological hazards of MS, HS, and EHS is 40.86% and 55.79%, and the accumulative cover area proportion of the watershed is 55.79% and 37.24%, respectively. The geological hazards susceptibility obtained using the variation trend slope model has high applicability and AUC values that are relatively high compared to previous studies on the susceptibility in Jiuzhai gully. These results can be effectively used to assess the susceptibility of geological hazards in Jiuzhai Gully. Lastly, we anticipate that the susceptibility mapping produced can effectively protect people’s lives and property by serving as a reference and source of guidance for dynamic geological hazards assessment in high-seismic-intensity mountainous locations.