The characteristics and causes of the landscape of the Aksu Wensu Grand Canyon.

The Wensu Grand Canyon is characterized by its ancient rock salt geological scenery, the unique Yadan geological scenery in western China, and China's unique giant karst geological secrets. Its formation is mainly caused by long-term terrain evolution.

Entering the scenic spot is like entering a beautiful and powerful natural gallery. The rock layers on the mountain wall in the canyon are clearly distributed, and the folds and curved lines formed by extrusion are very clear. The fractured rocks are sandwiched in the rock layer on the mountain wall. After hundreds of millions of years of wind and rain erosion, towering cliffs, strange peaks, and various shapes have been formed. It is a strange, rugged and strange landscape with strong colors, various shapes and colors.

To the northwest of the Grand Canyon, you can see the famous snow peak Tomur Peak, to the west you can reach Wensu Shenmu Garden, to the east it is adjacent to the famous Xiate Ancient Trail and Qiuci Cultural Tourism Area, and to the south it is adjacent to the Taklimakan Desert. The Wensu Grand Canyon tourist route is characterized by "one peak and one valley", and can also be expanded to "one desert and one river" to the south, forming a situation of simultaneous development of misaligned tourism products that complement each other.