Huangguoshu in which city and county in Guizhou

Huangguoshu Waterfall is in Zhenning Buyi Miao Autonomous County, Anshun City, Guizhou Province.

Huangguoshu Falls, Huangguoshu Falls. Anciently known as the White Water River Falls, also known as the "Huangguoshu" waterfalls or "Huangguoshu" waterfalls, the folk of Guizhou since ancient times has been rumored to be the myth of Huangguoshu Falls, Huangguoshu Waterfalls, the name comes from the myth of the knots in the story "" tree. Huangguoshu Waterfall is named after the tree that bears the " yellow fruit" in this mythological story.

Located in Anshun City, Guizhou Province, China, Zhenning Buyi Miao Autonomous County, belonging to the Pearl River system, the mainstem of the Xijiang River tributary of the Nanpanjiang River tributary of the Beipanjiang River tributary of the Taipan River tributary of the Kobu River downstream of the whitewater section of the water system, for the Huangguoshu Waterfalls in the largest waterfalls, is one of the world's famous waterfalls. Known for the water force is huge. The height of the waterfall is 77.8 meters, of which the main waterfall is 67 meters high; waterfall width of 101 meters, of which the top of the main waterfall is 83.3 meters wide. Huangguoshu waterfall is a karst landscape in the erosion of the rift point type waterfall.

Geological formation

Huangguoshu Waterfalls cause to go back to more than 200 million years ago in the Triassic, when the Huangguoshu area deposited a set of huge thick carbonate rocks. Huangguoshu waterfalls developed in a set of "middle Triassic in the middle of the Guanling two thick layer with a small amount of thin layer of cloudy tuff", the location in the east wing of the Wengzhai small dorsal slopes. Huangguoshu Waterfall formation period of the Baishui River, is a development between 100,000-500,000 years ago.

Quaternary period, late Pleistocene period by the "broad valley" to "canyon period" in the evolution of the ground river, and later due to the "Himalayan movement" period of the earth's crust many times intermittent Later, due to the "Himalayan Movement" period of crustal uplift, caused by the decline in the erosion datum of the river, resulting in the river erosion, dissolution and other downcutting effect to strengthen the formation of the "rift point" (riverbed due to the uplift of the earth's crust, the decline in the erosion datum, and tectonics, lithology, and other factors and the occurrence of a large turning point), this rift point at the rift, the cavern, the river is very well developed.

White water river first formed a karst erosion rift point type of falling water hole type waterfall, later with the river erosion, dissolution, side erosion effect in the crust intermittent uplift and the late Pleistocene warm and humid climate, hydrodynamics gradually increased under the influence of factors such as the roof of the falling water hole gradually collapsed, huangguoshu waterfalls finally presented, there have been 50,000 years of history.

Refer to Baidu Encyclopedia-Huangguoshu Waterfalls for the above