Where is Huangguoshu Waterfall, where is Huangguoshu Waterfall?

In Anshun City, Guizhou Province, Ningbuyi and Miao Autonomous County.

Huangguoshu Waterfall is located in Ningbuyi and Miao Autonomous County, Anshun City, Guizhou Province, China. Huangguoshu Waterfall was called Baishuihe Waterfall in ancient times, also known as "Huanggeshu" Waterfall or "Huanggeshu" Waterfall, Guizhou folk Hengrukuan has spread the mythical story of Huangguoshu Waterfall since ancient times, and the name of Huangguoshu Waterfall comes from the tree that bears "Huangguo" in this mythical story.

The height of Huangguoshu Waterfall is meters, of which the main waterfall is 67 meters high, the waterfall is 101 meters wide, and the top of the main waterfall is wide by meters.

The fame of Huangguoshu Waterfall began with the traveler Xu Xiake in the Ming Dynasty, and it has become a well-known scenic spot after the travel and dissemination of celebrities over the generations.

Huangguoshu Waterfall is located in the low-lying area of western Guizhou, the altitude is low, there is no frost all year round, the average annual temperature is 14 left oak banquet right, there is no severe cold in winter, there is no scorching heat in summer, it is a cold and summer resort.

Huangguoshu Waterfall, also known as Huangjushu Waterfall, is located in Ningbuyi and Miao Autonomous County, Anshun City, Guizhou Province, China, and is the largest first-class waterfall in the Huangguoshu Waterfall Group and one of the world's famous waterfalls.

The Baishui River at the time of the formation of Huangguoshu Waterfall was an above-ground river that developed between 100,000 and 500,000 years ago.

Later, with the erosion, dissolution and lateral erosion of the river, the intermittent uplift of the earth's crust, and the warm and humid climate in the late Pleistocene, the hydrodynamic force gradually increased under the influence of factors such as the gradual collapse of the sinkhole, and the Huangguoshu Waterfall finally appeared, which has a history of 50,000 years.

Zhenning County, Anshun City, Guizhou.

Huangguoshu Waterfall, that is, Huangguoshu Waterfall. In ancient times, it was called Baishuihe Waterfall, also known as "Huanggeshu" Waterfall or "Huanggeshu" Waterfall, Guizhou folk have spread the mythical story of Huangguoshu Waterfall since ancient times, and the name of Huangguoshu Waterfall comes from the tree that bears "Huangguo" in this mythical story.

Located in Ningbuyi and Miao Autonomous County, Anshun City, Guizhou Province, China, it belongs to the Baishui River section of the lower reaches of the Kebu River, a tributary of the Nanpan River, a tributary of the Beipan River, a tributary of the Beipan River, of the Pearl River system, and is the largest first-class waterfall in the Huangguoshu Waterfall Group and one of the world's famous waterfalls. It is known for its vast water potential. The height of the waterfall is meters, of which the main waterfall is 67 meters high; The waterfall is 101 meters wide, of which the main waterfall is 101 meters wide.

Huangguoshu Waterfall is an erosion crack waterfall in karst landform.

The geological formation of the Huangguoshu Waterfall

The origin of the Huangguoshu Waterfall can be traced back to the Middle Triassic period more than 200 million years ago, when a set of huge carbonate rocks were deposited in the Huangguoshu area. Huangguoshu Waterfall is developed in a set of "medium and thick layers interbedded with a small amount of thin-bedded cloud limestone in the second member of the Middle Triassic Middle Tongguanling", which is located on the east flank of the small anticline of Wengzhai.

The Baishui River in the formation period of Huangguoshu Waterfall is an above-ground river that developed between 100,000 and 500,000 years ago, and evolved from the "wide valley period" to the "canyon period" in the middle and late Pleistocene of the Quaternary period.

The fissures, karst caves, and dark rivers at this rift point are very well developed. Later, with the intermittent uplift of the earth's crust and the gradual increase of hydrodynamic forces in the late Pleistocene in the intermittent uplift of the earth's crust and the temperature and humidity in the late Pleistocene, the roof of the sinkhole gradually collapsed, and the Huangguoshu Waterfall finally appeared, which has a history of 50,000 years.