The Xiaojiang mudslide is located in Dongchuan District, Kunming City, Yunnan Province, not in Qujing. The Xiaojiang is a tributary of the Jinsha River on its southern bank, with a total length of 138.2 kilometers, a river valley floor width of 15-50 meters, steep cliffs on both banks, and a relative elevation difference of 1000-2000 meters. The water flow has a drop of 909 meters. The mudslide phenomenon here is relatively prominent, and the reasons include the loose rock stratum structure on both sides of the river and sparse vegetation on both sides of the valley.
The Xiaojiang mudslide is located in Dongchuan District, Kunming City, Yunnan Province, not in Qujing. The Xiaojiang is a tributary of the Jinsha River on its southern bank, with a total length of 138.2 kilometers. The valley floor is 15-50 meters wide, with steep cliffs on both sides, a relative altitude difference of 1000-2000 meters, and a water drop of 909 meters. The mudslide phenomenon here is relatively prominent, with reasons including loose rock strata on both banks of the river, sparse vegetation on both sides of the valley, and so on.