As Yellow River leaves the desert region in Inner Mongolia 内蒙古, it enters the loess plateau of soil deposits which are easily erodible. Over 90% of Yellow River's sediment enters the river from tributaries in the middle reaches. These two pictures show the passage of the river between Shanxi province 山西省 (to the right of the river) and Shaanxi province 陕西省 (to the left of the picture).

黄河 进入 晋陕边界, 黄河 90% 的 沙量 来自 这里

Picture source: 黄河水利委员会 编:《黄河风》, 黄河水利出版社, 1996.