Tibet, in the evolution of the geological history, land and sea through repeated ups and downs, but also to bear the qualities of the Himalayan orogeny, Heng Kong to the sea, the constant uplift, the formation of the modern world's youngest plateau at 4,000 meters above sea level on average more than Is indeed a "roof of the world." Tibet scene in the high mountains due to strong Tectonic movement and more of the rock. Igneous, sedimentary, and metamorphic rocks all kinds, including the role of the force outside the camp, which rise amid the proliferation of cave Jian Fei, rock Zi, Zhuang Wei at high altitude posed a peculiar landscape.
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