According to the typical cross section systemic investigated the geologic strata of the Late Quaternary Period in the Lushan mountainous region, that from the layer sequence sieved particulates (ø = 1~3mm) to the quartz grain carried observational research by the environment electronic microscope, there recognized many show the microstructure are the grain modality - transform structure - dynamical chemical effect etc., the usage the systemic process developing in the node event carried analytical of the environment respond on the section of layer type, adopt the comprehensive index sign token the earth surface layer process and environment respond scene, nail down dividing are four development stage of the ancient climate environment, the from below to upside on the difference for the glacier epoch environment – inter-glacier epoch environment - ice margin epoch environment – post-glacier epoch environment, they provided new foundation according to the evolvement process of Quaternary Period environment and global change for with the thorough research and science understanding in the Lushan area of China.