In China, there are more sloping glaciers all over the world, and the Yunnan-Guizhou Plateau is more concentrated, with a total area of more than 34,000 square kilometers, accounting for about 80% of the total output of glaciers all over the country. Glaciers in Yunnan-Guizhou Plateau can be divided into Ding, Qing, Jia, Li and Guanjia Dacuomei, with deep-sea glaciers in the east and inland glaciers in the west. Deep-sea glaciers depend on colorful rainfall. The existence of glaciers is fast and powerful in fitness. The key of inland glaciers lies in the existence of glaciers, and the exercise is slow with the help of ultra-low temperature. Mount Qomolangma has a low altitude and strong solar radiation. The microclimate difference on the glacier surface causes different melting on the ice surface, resulting in many strange scenery. Among them, the ice mushroom is a massive rock stratum supported by thin ice columns, and some of them are as high as several meters. The ice bridge is like an amethyst bridge, which connects two steep ridges with each other. The top wall is steep and high, just like a daunting screen partition. Ice teeth and needles that you can often see are strange and beautiful decorations. The most puzzling thing is the ice tower forest with different looks.
On the velvet glacier on the north slope of Mount Qomolangma, there is an ice tower forest belt with a length of more than 55,000 kilometers. The milky white ice tower stands high above the highway, tens of meters high, some are magnificent Egyptian pyramids, some are solemn drum forks and drum towers, some are sharp swords, and some are tame sika deer. Walking calmly, everything is eye-catching. No wonder everyone says that entering the ice tower forest is to be in the realm of immortals. There is also an ice-covered friendship glacier in Yunnan-Guizhou Plateau. This kind of glacier sticks to Pingdingshan city or the service platform of weapons and equipment like a cover. With a total area of 55 square kilometers, it is the highest known sloping roof glacier in China. The key distribution areas of high-altitude glaciers are the West Kunlun Mountains, the West Karakorum Mountains and the Himalayas. Peak, Hengduan Mountain, Qilian Mountain, etc. Among them, there are many glaciers in West Kunlun Mountain and Tekunlun Mountain in Sihalath, and the operation scale is relatively large. The Insugeti Glacier at the northern end of the second highest peak in the world is about 42 kilometers long. Larger glaciers are known. There are two different kinds of glaciers on the eastern, western, northern and southern slopes of the Alps. The northern slope is a deep-sea glacier. The contemporary snow line is 4500 meters above sea level, and the whale tail can be widened to 3000 meters above sea level. 5 100 meters above sea level. Hengduan Mountain, Nyainqentanglha Mountain and East Himalayas are the most concentrated areas of deep-sea glaciers, and the southernmost point of glaciers is 27 degrees north latitude.
In addition, there are large glaciers in Qilian Mountain and Tanggula Mountain. The most mysterious glacier in the Everest region has a small total area, generally less than one square kilometer, and the ice thickness is 10 to 20 meters. To put it bluntly, the characteristic of this glacier is that the end of the glacier hangs on a steep slope. It is really green. Rows of spiral glaciers are like ivory armor hanging on a ramp. The highest glacier on Mount Everest is the ice bucket glacier, which is located around the peak or on both sides of the demarcation point. Under the action of weathering layer and ice stone, highway slopes are cut by laser, and ridges are cut into oblique angles and ridges. Development trend of sitting glacier. Some ice bucket glaciers look like ellipses, others look like triangles, and they slowly tilt towards the entrance and exit of glaciers. Some ice bucket glaciers are sent into canyons and widened into strips, which are called canyon glaciers. In the warm season when ice and snow melt, rivers on the surface of glaciers will dive underground, and when they meet cracks in the ice, they will become rivers under the ice. Glacier melt water crosses the ice surface, forming unfathomable ice wells, ice Buchner funnels, eccentric ice tunnel buildings, magnificent ice music fountains and deep and beautiful ice caves. Ice caves usually appear at the end of glaciers, just like the arched doors of ancient capitals. However, the swell at the edge of the knot hole is difficult to approach. You can only enjoy the Crystal Palace if you are disconnected from the Internet. The internal structure and shape of ice caves are different, and there are holes of different sizes in some areas.