Park form of Dawushan National Park

Wushan Mountain was formed at the end of the Pleistocene Ice Age about 10,000 years ago, with a history of millions of years. Glaciers have reduced the climate of the whole area. The cold climate makes plants such as evergreen trees in the north extend southward and reach the territory of Dawushan National Park.

Later, when the glaciers retreated northward, these forests disappeared. Some forests have been preserved because of the high coolness and humidity of Fog Mountain. There are signs everywhere in the park, advising visitors to see this "unchanging world".

There are 25 peaks 1.800 meters above Wushan Mountain, which blocks the southward movement of the great glacier, so you can find plants and animals in the north and south here.