No one can tell why the strong wind and sand near the ancient city of Shule came into being.

Only thirty years ago, when sandstorms inundated the ancient city of Shule, there were periodic storms that never stopped.

If observed by meteorological satellite, the dynamic image will be formed.

You can see that within a hundred kilometers of the ancient city of Shule, from the southeast to the northwest, there is a continuous evil wind.

It is also this evil wind that makes the Taklimakan Desert expand northwest at a rate of 10 meters per year.

Perhaps tens of thousands of years later, the central region of the entire Asian...