The highest peak in the world? 5. The highest peak in the world?

Of course, we are Mount Everest in China, about 8848 meters.

Everest, Tibetan means "water of the Virgin". Mount Everest is located in Dingri County, on the border between China and Nepal in the middle of the Himalayas, with an altitude of meters, it is the world's highest peak, and the peak is covered with snow all year round. The entire Everest Nature Reserve is divided into three types: core protection area, buffer zone and development zone.

The terrain of the reserve is high in the north and low in the south, the terrain is complex and diverse, the average altitude is 4200 meters, but its lowest point is only 1433 meters, and the relative height difference is more than 7000 meters, forming a unique three-dimensional climate, which is manifested as "four seasons of snow at the top of the mountain, four seasons of spring at the bottom of the mountain, four seasons of spring at the bottom of the mountain, four seasons of a mountain, ten miles of different days".

Mount Everest, of course.

Mount Everest (Qomolangma), referred to as Mount Everest, also translated as Our Lady's Peak, Nepal is called Sagarmata Peak, also known as "Everest", located in the Himalayas on the border of the People's Republic of China and Nepal, with snow all year round. The height is meters, it is the world's highest peak, and one of the top ten most beautiful and shocking mountains in China.

The highest peak in the world is Mount Everest.

Mount Everest, referred to as Mount Everest, is the highest mountain in the world, the elevation of the snow surface is meters, is the main peak in the Himalayas, located on the border between the People's Republic of China and Nepal, is an arc-shaped mountain system similar to east-west, its northern slope is in the Qinghai-Tibet Plateau in China, and the southern slope is in Nepal.

About 65 million years ago, the Indian subcontinent rushed towards Eurasia and eventually collided with Eurasia, forming the rolling Himalayas.

Due to the collision and extrusion of the edge of the Eurasian plate and the Indian plate, the Himalayas have been violently uplifted, and it is estimated that the average rise is about 20-30 meters per 10,000 years, and until now, the Himalayas are still rising, rising 7 centimeters every 100 years.

Climatic characteristics of Mount Everest:

The climate of the Mount Everest region and its nearby peaks is complex and changeable, and even within a single day, it is often unpredictable. Generally speaking, the rainy season is from early June to mid-September, and the strong southeast monsoon causes frequent heavy rains, clouds and fog, and a harsh climate of ice and snow.

From mid-November to mid-February of the following year, due to the strong northwest cold snap, the minimum temperature can reach -50, and the average temperature is around -30. The maximum wind speed can reach 90 meters per second. From early March to the end of May, when the monsoon season transitions to the rainy season, and from early September to the end of October, when the rainy season transitions to the monsoon season, autumn, there is a possibility of better weather.

The above content reference: Encyclopedia - Mount Everest.

The highest peak in the world is Mount Everest.

Mount Everest, referred to as Mount Everest, is located in the Himalayas on the border between China and Nepal, and is covered with snow all year round. It is the highest peak in the world. Mount Everest is in the shape of a giant pyramid, majestic and majestic, with extremely steep terrain and complex environment.

Within 20 kilometers of its surroundings, there are peaks and peaks. There are more than 40 peaks above 7,000 meters above sea level, forming a magnificent scene of peaks coming and going, and the peaks surging.

Mount Everest is a meter above sea level, standing on the highest point of the vast Himalayas, covered in snow and ice all year round. Its pyramid-shaped peaks are clearly visible hundreds of kilometers away, giving it a sense of solemnity and sacredness. With its reputation as the top of the earth, Mount Everest has become the "temple" in the hearts of mountaineers from all over the world, which is the lifelong wish of every mountaineer.

The climate of Mount Everest and its nearby peaks is complex and unpredictable, even in a single day, not to mention the ups and downs throughout the year.

Formation and evolution of Mount Everest:

About 100 million years ago, in the ancient period of Huizhihan, there were only two supercontinents on the earth, the continent of Laoya in the northern hemisphere and the continent of Gondwana in the southern hemisphere, and between the two was the vast ancient Tethys ocean.

About 300 million years ago, with the movement of plates, the Laoya continent was divided into two, forming the North American continent and the Eurasian continent, and the Gondwana continent completely disintegrated, and the Qiangtang and Lhasa massifs gradually drifted, crossed the equator and finally joined the northern hemisphere, forming the core of the Qinghai-Tibet Plateau.

About 65 million years ago, the Indian subcontinent rushed towards the Eurasian continent and eventually collided with the Eurasian continent, constituting the most important orogeny on Earth in 500 million years. The Tibetan Plateau rises violently, forming the rolling Himalayas.

The highest mountain in the world is Mount Everest.

Mount Everest is the main peak of the Himalayas and the highest peak in the world. Located on the border between the People's Republic of China and Nepal, its northern slope is in the Tibetan Plateau of China, the southern slope is in Nepal, and the summit of Mount Everest is located in China.

In Tibetan, "Zhumu" means goddess, and "Langma" means the third. Because there are four other peaks in the vicinity of Mount Everest, Mount Everest is the third, so it is called Mount Everest.

Physical geography of Mount Everest:

Mount Everest is a giant pyramid-shaped, majestic and majestic, with extremely steep terrain and a very complex environment. Snow line height: 5800 6200 m on the northern slope and 5500 6100 m on the southern slope.

The northeastern, southeastern, and western ridges are sandwiched between three steep walls (northern, eastern, and southwestern), and between these ridges and cliffs, there are 548 continental glaciers.

The total area is square kilometers, with an average thickness of 7,260 meters. The recharge of glaciers is mainly formed by the deterioration of snow in the two major precipitation belts of the Indian Ocean monsoon belt. There are thousands of magnificent and rare ice towers on the glacier, as well as light and dark ice crevasses with ice cliffs and traps tens of meters high, as well as ice avalanches and avalanche areas full of dangers.