Abstract: The present paper discusses the features of mountain glacier sediment of Late Sinian in Beishan area that located in the west end of Inner Mongolia and northwest border of Gansu Province. The mountain glacier uplift belt, as an island-chain in Baihu-Mazongshan region, extends several handreds kilometers, its southern side is fault marine basin in Changheishan-Shuangyingshan-Wutongjing area, and the northern one is slope belt of sea basin, Pochengshan-Heidashan-Xichangjing, joint with the ocean area. The whole area appear'two depressions and one unlift"deposited basin framework. Tarim palacontinent, which located in the southern margin of the basin, was not covered with continental glacier by then. The central island chain uplift belt, consists of Middle Late Proterozoic Qingbaikou System, Jixian System and Changcheng System, was the source region of the palaeo-tillite. The authors found that the Xichangjing profile, as a representive one, is mostly developed. It shows that the Upper Sinian Xichangjing Group contains two sets i.e., the upper and the lower, of the paleoglacigenous rock, between them are the carbonate rock and terrigeneoussclastic sediments, which represent the warm climate condition at interglacial stage. It is suggested that there were two paleoglacial stage developed. In Beishan area, Xichangjing Group of Upper Sinian contacts with the underlying Dahuoluoshan Group, Qingbaikou Systam, and Pingtoushan Group, Jixian System with angular unconformity, and graduauly transited to the overlying Shuangyingshan formation of Cambrian System. The Pochengshan profile clearly indicated that the silicic rock of top of upper palaeo-tillite of Xichangjing Group showed gradual transitional contact with calcarenite containing Eoredlichia sp. fossil pieces, relevantly, the glacial pelitic conglomerate of transition bed from the upper glacigenous rock to Cambrian System contained sponge spicules and micropaleoflora fossils in Xichangjing region, some of which are correspond to that of upper Luoquan formation in Shaanxi and Henan Province. Therefore, it is proved that the upper glacigenous rock of Xichangjing Group belongs to Luoquan Ice Age, the paleoglaoigenous rocks under the interglacial deposits are the products of Nantuo Ice Age. In the area, tills from the mountain glacier were frequently carried away by ice rafting toward both side and droped in the distant places of the basins. As a result, the various environment marine deposit associations that containing tillites were formed.