When using the traditional static analysis method to analyze the influence of strong motion on the variation of the attribute parameters of rocks in mountainous areas, the interaction between the bottom and top of the rock fragment is neglected, which leads to inaccurate analysis results of rock density and other attribute parameters. Therefore, in this study, an influence analysis method is proposed to analyze the influence of strong motion on the attribute parameters variation of rocks in mountainous areas. With the proposed method, the degree to which the rock was subjected to strong motion can be effectively shown through the elevation control effect. Indoor and outdoor measurements of the original and fragmented rock densities are carried out, and the unloading and pressure between gravels are added to the measurement results. Then the variation in the results of various parameters such as density, porosity, natural water absorption rate, permeability coefficient, and softening coefficient of rock are obtained with the wax-coated method, and then, they can be effectively analyzed. The experimental results that show the proposed method is highly accurate for analyzing the attribute parameters variation of rocks in mountainous areas subjected to strong motion.