What causes waterfalls to form? What is the role of Huangguoshu Waterfall in tourism and economic de

From ancient times to the present, there will be many literati and writers who express Huangguoshu Waterfall in their own words.

The magnificence can be felt from the verses of the surging Huangguoshu Waterfall. The main reason for the formation of the waterfall is the difference in terrain and the large flow of water, which is a spectacular sight. Huangguoshu Waterfall has a role in promoting tourism and local economic development, and can make the local cultural resources known to more people, so it can promote the rapid development of local tourism-related economy.

Huangguoshu Waterfall is also the largest waterfall in China, is a famous scenic spot in our country, you can feel a different scenery here, this place is located in Guizhou, and it is also a beautiful business card of the local area. It will be found that Huangguoshu Waterfall is only one of the branches of the waterfall group, the largest of them, and through scientific methods, the width of Huangguoshu Waterfall can be 101 meters and the height can be as high as meters, which is the largest waterfall in China and Asia, so this waterfall is very well-known in the world. Many people also don't understand why Huangguoshu Waterfall is called Huangguoshu Waterfall, because there is a tree that is widely distributed here, and there are some ancient legends and stories, and finally this place is called Huangguoshu.

The formation of Huangguoshu Waterfall is mainly related to the local climate and geological movements, and it is located in Anshun City, Guizhou Province.

And in the upper reaches of the Baishui River, in the Pearl River system.

Therefore, it evolved for a long time, and finally formed a waterfall with a relatively large drop. According to some related investigations, it will be found that this area was once also an underground river.

Therefore, these areas of Guizhou also belong to karst landforms.

Over the long years, there have been many movements of the earth's crust.

Every time the rock layer is moved, there is a break, and when the rock layer breaks, the drop becomes larger, and some surface runoff flows here. When the rock layer is constantly broken, the crevices are constantly widened, the water is constantly flowing, and when the rock is soaked with water, the surface water flows into this place, forming the entrance to the dark river, which expands through movement, and finally becomes a spectacular waterfall.

The difference in rock types creates a "wall" in the river channel. It can promote the development of local tourism, attract talents to the local area, improve the local economy and GDP, improve the local visibility, and play a certain role in promoting.

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. During the formation period of Huangguoshu Waterfall, the Baishui River was raised intermittently during the "Himalayan Movement", which caused the river erosion datum to decline, resulting in the strengthening of the erosion and dissolution of the river, and the formation of a "rift" there. For the sustainable hairpin of the tourism area, it is also the basis for the sustainable development of the entire regional economy, ensuring the principle of people-oriented, harmonious coexistence between man and nature, and thus enhancing the development of the regional economy.

Differences in rock types, with cliffs on both sides of the valley. It can promote local economic development, promote the development of local tourism, improve local visibility, promote the development of GDP, and can make the economy lively.

The reason for the formation of Huangguoshu Waterfall is that the cause of Huangguoshu Waterfall can be traced back to the Middle Triassic 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. Later, with the intermittent uplift of the earth's crust and the gradual increase of hydrodynamic forces 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.

It is naturally formed, but there is a long process.

The box-shaped canyon in front of Huangguoshu Waterfall was originally a water-falling cave, and later with the development of the cave, the erosion of the water flow caused the top of the cave to collapse, and the waterfall was formed. Therefore, it was the sinkhole that collapsed to form the Huangguoshu Waterfall. Since the formation process of a waterfall is closely related to the development process of the river where the waterfall is located, the formation process of the Huangguoshu Waterfall slide cloth must be considered in conjunction with the evolution and development history of the Baishui River.

The development process of Huangguoshu Waterfall can be roughly divided into seven stages: the former Dou Period, Zhedou Period, Laolongdong Period, Baishui River Period, Huangguoshu Subcurrent Period, Huangguoshu Waterfall Period and Modern Cutting Period. It was formed from the Tertiary Miocene epoch between 27 million and 10 million messengers, and has continued to the present day, undergoing a cyclical evolution process from the surface to the bottom and back to the surface.