1. Developed in mountain building movement
Danxia landform is a red-layer landform characterized by steep cliffs, in which "red layer" refers to red gravel.
2. Erosion over the years
The stone pillars and walls formed by the orogenic movement gradually disappear under erosion over the years, and gradually become hills with gentle slopes. The sandstone is called kamishiki, and the red walls are called red walls.
When you come to one of the viewpoints, you can enjoy the mountains in a sea of seven colors.
Since you are in the middle of it, you can see it more closely, but it is only a small corner of the picture of the mountains.
If you are standing on the top of the mountain, you may be able to feel their wonder of them.
Overlooking the mountains, the peaks in front of you look like the uneven paint blocks on an oil painting. It's amazing! Here you can feel the masculine beauty and pure natural beauty of the wilderness, the unadorned flair, and the unconcealed exuberance.
Danxia landform main distribution area
Danxia landform is a rare natural geological treasure on earth, which is mainly distributed in China, the western region of the United States, Central Europe, and Australia. Among them, China has the most distribution, the widest range, and the most magnificent scenery.
Among the many Danxia landform, the Colorado Grand Canyon in the United States is the most representative.
It is located in the northwestern part of Arizona and the southwestern part of the Colorado Plateau.
The Grand Canyon is full of red rocks from the bottom of the valley to the top of the canyon, with rock formations from the Cambrian to the Cenozoic period.
They are of various colors and extremely magnificent.
In Australia, the Danzig landscapes are found in the Olga Mountains, where the rocks are mainly Cambrian marine red sandstones with conglomerates and near-vertical rock layers.
In Germany, the Danxia landform is located in the southern Bohemian Plateau and is a Cretaceous red sandstone with horizontal production and vertical joint development.
There are rock peaks, rock pillars, and rock needles developed on the red-layered tectonic platform, and there are also natural bridges and sunburst landforms.
