Abstract: The study conducted the research on glacier relics and the sediments of glaciers, loess, stream using geochronology, which confirmed the corresponding relationship between the sediments of quaternary glacier, loess, stream and Marine Isotope Stages (MIS) in Pagoda Valley of Mengshan. And on this basis, it was the first time to study the relativity between all kinds of stratum sediments and Marine Isotope Stages(MIS) in Mengshan, and the intrinsic relationship between the sediments of glacier, loess, stream and environmental evolution was established. Comparing these sediments and Marine Isotope Stages(MIS) especially in Holocene and late Pleistocene found that it is a strong relationship between these Quaternary sediments and Marine Isotope Stages(MIS) and confirmed the fact that the existence of Quaternary glacial through the sedimentary sequence and environment evolution in Mengshan and eastern China.