Gobi jerboa the Great Lakes Depression, Valley of the Lakes, Northern Gobi, Dzungarian, Gobi Desert, Trans Altai Gobi Desert and Alashani Gobi Desert (Sokolov et al. 1998). Approximately 21% of the Gobi jerboa’s range in Mongolia is in protected areas (Clark et al. 2006). The Gobi jerboa is found in desert and steppe habitats, which are particularly well vegetated. Saltwort, ephedra, and desert bushes characterize these landscapes in China (Smith and Xie 2008). The gobi jerboa are nocturnal rodents which live alone, and spend most of the daylight hours in unplugged burrows that are relatively simple, and can extend up to 60
Gobi Desert is a rain shadow desert, formed by the Tibetan Plateau blocking precipitation from the Indian Ocean reaching the Gobi territory. The Gobi measures over from southwest to northeast and from north to south. The desert is widest in the west, along the line joining the Lake Bosten and the Lop Nor (87°–89° east). It occupies an arc of land in area as of 2007; it is the fifth-largest desert in the world and Asia's second largest. Much of the Gobi is not sandy but has exposed bare rock. In its broadest definition, the Gobi includes the long stretch of desert