How the Tien Shan Mountains were formed How the Tien Shan Mountains were formed

It has accumulated snow over many years.

Majesticof the Tien ShanSnowyof the Tien ShanMajesticof the Tien ShanBeautifulof the Tien ShanMagicalof the Tien ShanRelated Notes:Tianshan, one of the world's seven major mountain systems, is located in the hinterland of Eurasia, across 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 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.

the majestic Tien Shan; the vast Tianshan Mountains; the winding Tien Shan; the towering Tien Shan; Beautiful Tien Shan.

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 of Xinjiang's major rivers, the Syr Darya, Chu and Ili rivers, all originate in this mountain.

the majestic Tien Shan; the vast Tianshan Mountains; the winding Tien Shan; the towering Tien Shan; Beautiful Tien Shan. the magical Tien Shan; the Tian Shan that raised me; The Tianshan Mountains in the fairyland of earth.

The tall Tien Shan, the beautiful Tien Shan.

Beautiful Tien Shan.

Tall Tien Shan.

The vast Tien Shan Mountains are beautiful Tien Shan.

The Tianshan Mountains are one of the seven major mountain systems in the world, running east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about one-third of the area of Xinjiang. It is a relatively young mountain system, formed about two to three million years ago. The geomorphological features of the present mountain range are the product of crustal changes in the late Cenozoic.

The formation of the Tianshan Mountains is mainly due to the orogenic Zhaoliang movement, and since the Mesozoic and Cenozoic, under the influence of the long-range extrusion effect of the collision between the Indian plate and the Eurasian plate, intracontinental subduction has occurred. Under the action of tectonic loads, bending intracontinental subduction foreland basins were developed along the southern and northern frontlands of the Tianshan Mountains, which is the formation of the Tianshan Mountains.

The Tianshan Mountains are one of the world's seven major mountain congratulatory systems, running east-west, stretching for 1,700 kilometers in China, covering an area of more than 570,000 square kilometers, accounting for about one-third of the entire area of Xinjiang. It belongs to a relatively young mountain system, formed about two or three million years ago. The geomorphological features of the present mountain range are the product of crustal changes in the late Cenozoic.

The formation of the Tianshan Mountains is mainly due to the orogeny, and since the Mesozoic and Neo-Zen cavities, under the influence of the long-range extrusion effect of the collision between the Indian plate and the Eurasian plate, intracontinental subduction has occurred. Under the action of tectonic loads, an intracontinental subduction foreland basin was developed along the south and north of the Tianshan Mountains, which is the formation of the Tianshan Mountains.

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.