The material basis of Danxia Mountain World Geopark is the red river-lake facies gravel formed in the late Cretaceous period about 7-90 million years ago. Around 65 million years ago, the area where the geopark was located was affected by the tectonic movement of the earth, resulting in many faults and joints, and also turned the entire Danxia basin into a denuded area. The Himalaya movement, which began about 23 million years ago, has caused the area to rise rapidly. In the long years, intermittent uplifting effect has caused the landform of the region to change earth. The earth's internal and external forces have worked together to shape the Danxia Mountain area into 680 mountain rocks scattered and scattered, and the image is thousands.