Which waterfall in my country is called the Yellow River
Where the river is curved, the radius of gyration of the water on the concave bank side is larger than that on the convex bank side. Over time, the concave bank plain will suffer from water and soil erosion and become smaller and smaller. Due to uneven water flow, most of the sediment in the water is deposited on the convex bank side. The land is fertile and the plain area is getting larger and larger. The ancestors considered choosing "Rui" in terms of residential safety and farming experience, aiming to make this terrain conducive to transportation, farming, fishing and hunting.
Feng Shui says that this kind of terrain is the best in form. If the convex bank triangle happens to be located in the south of the mountains and the north of the water, then this kind of terrain is the ultimate form of "form victory".
By the Ming and Qing Dynasties, this terrain had lingered in the subconscious of the Chinese nation. The topography of Tiananmen Square and Jinshui River can be seen as the craftsmen’s pursuit of “Rui”. The experience of our ancestors has become part of Feng Shui.
However, what I have to say here is that Feng Shui physiognomy and the art of "aligning yin and yang" have been infected by the theory of gods and ghosts in the Song, Yuan, Ming and Qing Dynasties, so that many people Not knowing what is going on, blindly superstitious. The experience of our ancestors was derived from their reverence for nature. If you cannot view it correctly and blindly believe in the theory of gods and ghosts, it will not only be useless for life, but also tarnish the traditional culture of the Chinese nation.
History and Humanities:
The Loess Plateau, Qinjin Gorge, Hukou Waterfall, Shili Longcao and Mengmen Mountain are all products of nature and important natural historical relics. . On the high terraces of the Yellow River, a 2-meter-thick gravel layer is accumulated on the rock surface 100 meters above the river bed. Together, they form the first-level high terraces of the Yellow River. This accumulation terrace is the product of the early development of the Yellow River and is a remnant of the Yellow River bed at that time. This high terrace also exists in some sections of the Qinjin Gorge, and it is of great significance as well as the characteristics of crustal movement at that time.
The origin of the two-toed beast fossils is 3 kilometers downstream of Hukou Waterfall. The two-toed beast fossils are found in an area of about 40 square meters. Didactylus was an animal that lived millions of years ago. The discovery of this paleontological fossil location is of great significance to the study of the paleogeographic environment of the Hukou area.