How long is the Tien Shan mountain range and what is the elevation of the Tien Shan?

Tianshan is one of the world's seven major mountain systems, located in the hinterland of the Eurasian continent, spanning China, Kazakhstan, Kyrgyzstan and Uzbekistan from east to west, with a total length of about 2,500 kilometers, is the world's largest independent zonal mountain system, and is also the world's farthest mountain system from the ocean and the largest mountain system in the world's arid regions. The Tianshan Mountains run east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about 1.3 of the entire area of Xinjiang. The entire Tianshan mountain system is composed of three mountain ranges, which are called the Northern Tianshan, Middle Tianshan and Southern Tianshan respectively from north to south.

The Tianshan Mountains are composed of three parts: mountains, intermountain basins and piedmont plains.

The Tianshan Mountains are one of the world's seven major mountain systems, located in the hinterland of the Eurasian continent, the largest land on the earth, and the Tianshan Mountains span China, Kazakhstan, Kyrgyzstan and Uzbekistan from east to west, with a total length of 2,500 kilometers, an average width of 250,350 kilometers from north to south, and more than 800 kilometers at its widest point. The Tien Shan Mountains are the largest independent zonal mountain system in the world; The Tien Shan Mountains are also the world's farthest mountain system from the ocean and the largest mountain system in the world's arid regions.

The Tianshan Mountains run east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about 1.3 of the entire area of Xinjiang. The Tianshan Mountains in China divide Xinjiang into two parts: the Tarim Basin to the south; To the north is the Junggar Basin.

Tomur Peak is the highest peak of the Tien Shan mountain range, with an altitude of meters. The Syr Darya, Chu and Ili rivers all originate in the Tien Shan.

Mountain composition. The Tianshan mountain system consists of three mountain ranges, which are called the Northern Tianshan, Middle Tianshan and Southern Tianshan respectively from north to south. The Tianshan Mountains are composed of three parts: mountains, intermountain basins and piedmont plains.

At 12:10 on June 21, 2013, there were four districts in China: Tomur Peak, Karajun-Kurdenin, Bayinbrook and Bogda in the Tianshan Mountains"Xinjiang Tianshan"The name was successfully applied for World Natural Heritage and became the 44th World Heritage Site in China.

The Tien Shan Mountains are a large mountain range in central Asia that traverses the central part of China's Xinjiang region and juts into Kazakhstan at its western end. It is about 2,500 kilometers long, 250-300 kilometers wide, and has an average altitude of about 5,000 meters. The highest peak, Tomur Peak, is 6,995 meters above sea level, and Bogda is 5,445 meters above sea level.

These peaks are all within the territory of China, and the peaks are covered with snow. Three major rivers in Xinjiang--- the Syr Darya, Chu and Ili rivers, all originate in this mountain. The snow on the snowy peaks of the Tianshan Mountains --- Bogda peaks does not melt all year round, and people call it "the sea of snow".

On the mountainside of Bogda, there is a lake called "Tianchi", which is 1,900 meters above sea level and about 90 meters deep. The water in the pool is made of melting snow and ice, and it is clear and transparent, like a large mirror. The white snow-capped peaks and the emerald green spruce trees reflect in the lake, forming a beautiful picture and making it a famous tourist attraction in Xinjiang.

The Tianshan Mountains divide Xinjiang into two parts: the Tarim Basin to the south; To the north is the Junggar Basin. Although the two basins are twin "brothers", their natural characteristics are very different.

Surrounded by high mountains, the Tarim Basin has a particularly dry climate, mostly desert areas, and only on the green of the marginal areas can you grow grains, cotton, melons and fruits. The mountains on the northwest edge of the Jungga Basin are not very mountainous, and there are many gaps, and the air currents of the Atlantic Ocean and the Arctic Ocean can enter, so the climate is relatively humid, except for some oases in the basin where you can grow spring wheat, cotton, melons and fruits, etc., the pastures here are excellent, and the animal husbandry is developed. The famous Karamay oil field is also located in this basin.

The elevation of the Tien Shan Mountains is meters, and the Tien Shan Mountains are located in the hinterland of the Eurasian continent, flat.

The average altitude of Bai is about 4,000 meters, from the Gobi Xingxing Gorge in Hami in Xinjiang, to the Gobi in Hami, China, to the Kizilkum Desert in Uzbekistan in the west, extending from east to west, across China, Kazakhstan, Kyrgyzstan and Uzbekistan 4 countries, stretching for about 1,760 kilometers in Xinjiang, China.

The Tianshan Mountains run east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about 1.3 of the entire area of Xinjiang. The Tianshan Mountains in China divide Xinjiang into two parts: the Tarim Basin to the south and the Junggar Basin to the north.

Tomur Peak is the highest peak of the Tien Shan mountain range, with an altitude of meters. The Syr Darya, Chu and Ili rivers all originate in the Tien Shan.

The average altitude of the Tien Shan Mountains is about 4,000 meters. Located in the hinterland of Eurasia, it is one of the seven major mountain systems in the world, with a total length of about 2,500 kilometers.

The Tianshan Mountains in China.

Xinjiang is roughly divided into two parts: the Tarim Basin to the south.

To the north is the Junggar Basin.

Tomur Peak is the highest peak of the Tien Shan mountain range, with an altitude of meters. The Syr Darya, Fengyuzhou, Chu and Ili rivers all originate in the Tianshan Mountains. It is also the world's largest independent zonal mountain system, the world's farthest mountain system from the ocean, and the world's largest mountain system in arid regions.

Brief introduction. The Tianshan Mountains, also known as the Chinese Tianshan Mountains or the East Tianshan Mountains, were known as the White Mountains in ancient times, also known as the Snow Mountain, because of the snow in winter and summer, so they got their name. The Tianshan Mountains are the only large-scale mountain range in the world sandwiched by a huge desert, and have become a large-scale mountain ecosystem in the temperate arid region of the world due to its geographical location deep inland, temperate continental arid climate, landform pattern of mountain basins, numerous glaciers and rivers, wonderful natural scenery, special biota and chiral processes.

The most typical representatives.

The elevation of the Tien Shan Mountains is meters. Located in the hinterland of Eurasia, the Tianshan Mountains are one of the world's seven major mountain systems, with a total length of about 2,500 kilometers.

The highest peak of the Tomur Tien Shan mountain range, with an altitude of meters.

The Syr Darya, Chu and Ili rivers all originate in the Tien Shan. It is also the world's most independent zonal mountain system, the world's farthest mountain system from the ocean and the largest mountain system in the world's arid region.

A brief introduction to other aspects of the Tianshan Mountains. The climate of the Tianshan Mountains is clearly divided into two seasons in the year: cold and warm. The weather is mostly sunny in the cold season, with deep snow and fog and frost in the mountains, basins and valleys below 3,000 meters.

In the warm season (summer), there is a lot of rain and snow above 3,000 meters above sea level. The climate is cool below 3000 meters. In the Tianshan Mountains, especially in the western section of the Tianshan Mountains, obvious inversion stratification is often formed in winter.

The inversion occurs in October and disappears in April of the following year. The stratification in January was the largest, reaching about 3,000 meters.

The Tianshan Mountains in China are about 2,500 kilometers long.

Tianshan, one of the world's seven major mountain systems, is located in the hinterland of the Eurasian continent, spanning China, Kazakhstan, Kyrgyzstan and Uzbekistan from east to west, with a total length of about 2,500 kilometers, an average width of 250-350 kilometers from north to south, and a maximum width of more than 800 kilometers.

The Tianshan Mountains run east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about 1.3 of the entire area of Xinjiang. The Tianli Tanshan Mountains in China divide Xinjiang into two parts: the Tarim Basin to the south, and the Junggar Basin to the north.

Tomur Peak is the highest peak of the Tien Shan mountain range, with an altitude of meters. The Syr Darya, Chu and Ili rivers all originate in the Tien Shan. The Tianshan Mountains in China are composed of three parallel folded mountain ranges, high in the west and low in the east, and the mountains are broad.

The northern veins of the Tianshan Mountains include Alatau Mountain, Keguqin Mountain, Borokonu Mountain, Bogda Mountain, etc.; The central vein (trunk) of the Tianshan Mountains includes Mount Arakhar, Mount Nalati, Mount Erwengen, Mount Hora, etc.; The southern veins of the Tianshan Mountains include Kokshar Mountain, Harke Mountain, Tiersk Mountain, Karatek Mountain, etc.

Fill in the adjectives to modify the Tianshan, the majestic Tianshan.

The Tianshan Mountains are relatively young, formed about two to three million years ago. About 12 million to 2 million years ago. The geomorphological characteristics of the Orange Hail Mountains are the product of crustal changes in the late Cenozoic.

The geological evolution of the Fanshan Mountains in Tianyuanzhou can be divided into the late Carboniferous to the early Permian collisional-postcollisional tectonic magmatic activity stage, the early to middle Permian mantle source magmatic activity and crust-mantle interaction stage, and the intracontinental evolution stage since the late Permian.

East Tien Shan.

Tianshan Scenic Area is located on the north slope of the East Tianshan Mountains, starting from the cold gas ditch in the east, reaching the pine pond in the west, from the Tianshan Temple in the south, and connecting the Mingsha Mountain in the north, with a total area of 120 square kilometers, about 70 kilometers away from the city of Hami Ants, and there is a provincial highway (i.e. the Silk Road North New Road) to the road, and the traffic and communication are convenient. The Tianshan Mountains, a huge mountain range across Xinjiang, have a pleasant scenery.

The Tianshan Mountains stretch across central Xinjiang for about 1,500 kilometers from east to west. It divides Xinjiang into the Tarim Basin and the Junggar Basin, which is an important geographical boundary. The folds of the Hercynian movement were uplifted, and the Yanshan movement was eroded into a quasi-plain state in the later stage.

The Himalayan movement uplifted again, forming many bulky mountains and faulted basins. It consists of a series of parallel mountain ranges, divided into three zones: northern, central and southern. The Northern Tien Shan Mountains include the Alatau, Borikonu, Ilian Habilga and other mountain ranges, with a length of about 1,000 kilometers from east to west, a width of 35 to 50 kilometers, and an altitude of 4,000-5,000 meters.