How to get to the glacier?

Take a bus from Xining, the capital of Qinghai Province, to Maqin (Dawu), where Guoluo Prefecture is located. The whole journey is 638 kilometers and takes 2 days. But sometimes in winter, the traffic will stop temporarily because of the heavy snow closing the mountain. From Maqin to Xueshan Township, it is 55 kilometers north along Dongqinggou. Mountain torrents often occur in rainy season, which hinders traffic. Change horses or cattle from Xueshan Township, return to Kiriko Quhe River for more than 30 kilometers, and reach the mountaineering base camp at the end of Quhar Ma Xiao Glacier.

Another route into the mountains is from Xining to Qinghai Lake, and then take a bus to the hot springs. The road section is in good condition, with a total length of 460 kilometers. It's 360 kilometers from the hot spring to the base camp. It takes 9 days to climb the mountain officially when the weather is fine. Then go to Maqin, guide from the base camp and return to Xining. This route climbs the second peak of Mount Animaqing, with an altitude of 6268 meters. Its climbing route is shorter and the mountain shape of this peak is steeper.

2. Where to see glaciers

Glaciers can be seen in western Sichuan in July.

Western Sichuan is a part of the Qinghai-Tibet Plateau, which belongs to the plateau and mountainous climate. Some peaks are over 7 kilometers above sea level, such as Siguniang Mountain. Every time the altitude rises 1000m, the temperature drops by about 6. Therefore, the temperature in the mountains is 40% lower than that in the plains, basically below zero. So glaciers don't melt in summer and July, so you can see glaciers.

3. How to get out of the glacier holy land?

This means that the climate of the earth and the United States is extremely cold, and large areas at high latitudes are covered by continental glaciers. The last ice age was in the Pleistocene. According to the research results in Europe and North America, there are six glacial periods and five interglacial periods. According to the analysis of Japanese ice bucket topography (kar), it is found that there were two ice ages. The most important ice age is Carboniferous Permian, and the remains of glaciers remain in Gondwana. In addition to the above two ice ages, glacial remains of Precambrian, Mesozoic and Tertiary were also found in Europe and America, but they were not significant. During the ice age in geological history, glaciers slipped on the earth. This influence depicts vast land and forms many lakes and swamps. The last ice age occurred about 2 billion years ago. In southern Canada, there are a series of primitive glacial deposits on the ground, stretching 1000 miles from east to west. This earliest Canadian ice sheet is at least 1000 miles long, 1000 miles wide and thousands of feet thick. The latest evidence shows that ice has flowed to the northern United States, at least to Michigan. Scientists believe that glacial sediments found in South Africa, central India and western Australia belong to the same era as southern Canada. If so, the ice age 2 billion years ago must have been very extensive and lasted for millions of years. Since then, the earth has experienced several ice ages. In the recent 654.38+0 billion years, the earth has experienced at least six major ice ages, each with an interval of about 654.38+0.5 billion years and each lasting about 50 million years. As for why there is such a periodic ice age, it is a mystery in the history of the earth. Scientists have put forward many theories about this, from the change of ocean currents to the periodic change of sunspots. But no theory is tenable and convincing. Obviously, the ice age phenomenon is caused by many factors, but one thing seems certain, the earth is still in the ice age. The term ice age may be a bit vague. Usually, this term refers to the period when some parts of the earth were covered by glaciers for one or two million years. These times are usually marked by a series of glacial advances or interglacial periods (glaciers stop advancing, melting and retreating). However, the ice age, as geologists say, refers to the period of global cooling, which may have lasted for millions of years. The 50 million years mentioned above are considered as the ice age. Obviously, several ice ages may and do occur in one ice age. The recent ice age began about 65 million years ago, which seems to be related to the Cretaceous extinction. There is a lot of evidence that the earth collided with a huge comet or asteroid, and the debris of the latter flew into outer space. A large amount of smoke and dust from forest fires caused by collisions permeates the lower atmosphere, blocking sunlight, causing the earth's temperature to drop sharply and producing a large amount of acid rain. In this way, the only remaining dinosaurs became extinct, and three-quarters of the existing animal and plant species became extinct. This collision may have changed the earth's orbit, which is why the earth has kept this low temperature. There is no indication that the earth may return to the Mesozoic hot climate suitable for dinosaur growth. The beginning of the ice age was a slow process. About 65 million years ago, glaciers began to form in Antarctica, and the ice surface became smaller and smaller, gradually forming a thick uplift ice sheet. About 20 million years ago, ice covered the entire Antarctic continent, and this process continues. It was not until about120,000 years ago that glaciers began to spread and move, covering alaska range. During the ice age, the glaciers in Greenland were relatively young, because the continent was not covered by glaciers until about 3 million years ago. Time has entered a new ice age, which geologists call Pleistocene. About 2 million years ago, a large number of glaciers began to move forward, sometimes covering a quarter of the earth and thousands of feet thick. During the last freeze, the glacier melted at least four times, so it moved forward several times and retreated several times. Now people are beginning to find some evidence that glaciers are always fiercer in the next advance than the previous one.

The most intense one happened about 50,000 years ago and stopped at 1 0,000 years ago. Whenever there is an interglacial period, the climate in the United States will get warmer on average, much warmer than it is now. Usually the interglacial period lasts for thousands of years. Even at the peak of the last ice age, it stopped melting several times, and the temperature of the whole world was slowly rising and fluctuating. Scientists believe that the earth is still in the ice age, because the surface of110 Mars is still covered with hard ice. Greenland and Antarctica are covered with 5 million cubic miles of ice. Glaciers are more common in mountains and valleys around the world. But on the clear historical record, the earth experienced the interglacial period of 100 years. The tourist resort built in Switzerland at the beginning of this century once gave visitors an unobstructed view of the ice and snow scenery, but now, the world of ice and snow has long since disappeared! If this interglacial period continues, all the glaciers on the earth will melt, and the sea level will rise by 200~300 feet, flooding many big cities around the world. Only frogmen with diving equipment can go to new york and Boston. Perhaps this interglacial period is temporary, and the earth will become cold and frozen again in the next few thousand years. Huge icebergs will reappear, push around the world and devour all civilizations along the way. Perhaps the ice age is really coming to an end: all this can only be explained by time and submerged coastal cities.

4. Where is the glacier?

Glaciers are generally at least 2500 meters above sea level.

Glaciers mostly exist in the north and south poles and high altitude areas. For example, Hailuogou Glacier in Ganzi, Sichuan Province is a modern glacier with a low altitude, with an altitude of only 2,850 meters. Because of the low temperature, the snowfall greatly exceeds the snowmelt, and the snow is getting tighter and tighter. Snow that melts during the day will form ice crystals at night and become granular snow. Particles of snow are combined and compacted into ice, which is called glacier ice. When glacier ice accumulates to a certain thickness, it will begin to flow under the action of gravity, so it is called a glacier, that is, flowing ice.

5. How to get to the glacier?

Going up high, there is usually snow in the alpine terrain, and the snow is generally next to the alpine biota. If a large number of spruces suddenly appear, or if you walk around the plain, you may find snow fields! I hope you are in the world of Mincartfs!

Jogory Peak is located in the middle of Karakorum Mountain. The border between China and Pakistan. Mount Qomolangma is 86 1 1 m above sea level, which is the main peak of the Karakorum Mountains, second only to Mount Qomolangma (8844.43m above sea level). Qiaogeli Peak is located in Tashkurgan Tajik Autonomous County, Xinjiang Uygur Autonomous Region, and belongs to China. Jogory in Tajik means tall and majestic. But Tibetan also has a white goddess. The reason for this is that there are descendants of Tibetans on the south side of Chogory Peak. According to historical research, the south side of Chogory Peak is the nomadic and active area of Tajik herders. Because their language is similar to Tibetan, Qogir can also be considered as Tibetan. The glacier on the north side of the Jogory Peak is called the Jogory Glacier, and the topography of the Jogory Glacier is complex and changeable. Glacier surface is broken, and light and dark ice seams are staggered. The valley on the west side of the glacier is a steep rock wall, and there are often rolling stones, ice collapses and avalanches. On both sides of Mount Everest, there are 44 kilometers of Yinshugeti Glacier.

6. Where is the glacier?

Yibin is 639 kilometers away from the ancient glacier. It takes about 9.5 hours to take Yin Kun Expressway, Rongzun Expressway, Rongchang Expressway, National Highway 377 and National Highway 347.

7. How to get to the ancient glacier

World of Warcraft level 77 learned to fly out to make storm cliffs and ice cap glaciers.

1. Brush hemolysis furnace, 70 brush ecological boat, 77 fly out to do the task of storm cliff and ice cap glacier.

2. If it is a trumpet, you can skip the last part of the task.

3. The other 58-70 is still a melting pot. If you don't know much about it, just go up a few stairs at the door and go to the battlefield, so you won't be tired if you win.

After 4.70, I brushed the magic pivot and cleared a few dragons at will. The entrance is square, with four sides, one on each side and a room in the middle of the tail king. Besides, the right-hand side of the entrance can go in and hit a tree or something. This is much easier than an eco-boat. A has only 1 1w stingy experience.

8. How to get to the ice cap glacier?

Glacier Treaders are a group called Glacier Treaders Glory, which is divided into 10 and 25 people. This is what the world often says about ICC dragon's achievement. In fact, the copy of that team is called Icecrown Castle Plug, and the entrance to the battle with the Lich King is in the Arctic Icecrown Glacier.