Which area does Anji Sea in Xinjiang belong to?

Kuitun City (English name: Kuytun City) is a county-level city directly under the jurisdiction of People's Republic of China (PRC) and Ili Kazakh Autonomous Prefecture in Xinjiang Uygur Autonomous Region, hence the name Kuitun River. Located in the northwest of Xinjiang, the northern foot of Tianshan Mountain and the southwest edge of Junggar Basin. It is 253 kilometers away from Urumqi in the west, Karamay in the south, Shawan County in Tacheng area in the east and Wusu City in Tacheng area in the west. The railway in northern Xinjiang passes through the territory, and the 2 17 national highway and the 3 12 national highway meet here. Area 1 17 1 km2, population 3 1 ten thousand. There are Han, Kazak, Uygur, Hui and other ethnic groups. The terrain is high in the southwest and low in the northeast, mostly in the piedmont alluvial plain, with Kuitun River in the west and many passages in the urban area. It is a new industrial city with light industry as the main industry, and its industries include brewing, cigarette, knitting, wool spinning, cotton spinning, chemical industry, printing, paper making, plastics, food and so on.

Hongshan Grand Canyon is located in Anji Haihe River Basin in Tianshan Mountain area, with a length of about 20-30 kilometers and the deepest part of the canyon of about 300-400 meters. It is the location of Hongshan coal mine in the seventh agricultural division. The deepest, riskiest and strangest part of the canyon is the downward part from the old mine department of Hongshan Coal Mine, No.7 Agricultural Division. There are two routes from Kuitun No.7 Agricultural Division to Hongshan Grand Canyon. All the way from Kuitun, along the National Highway 3 12 to the east to the south of Hongshan Dapo, along the county road to Hongshan Coal Mine to the old mine department of Hongshan Coal Mine, about 50 kilometers. The other way is from Kuitun along the 2 17 national highway to Kazi in the south and then along the 10 1 national highway to the old mine department of Hongshan Coal Mine in the east. To truly appreciate the wonder, danger and beauty of Hongshan Grand Canyon, it is best to cross Hongshan Grand Canyon on foot.

The danger of Hongshan Grand Canyon lies in its depth, which is 300-400 meters deep. Dangerous and steep, straight and steep as a knife and axe; The danger is that the cliff is not a hard stone, but a combination of sand, and you can see large and small landslides anytime and anywhere.

The wonder of Hongshan Grand Canyon is that it is close to the mountains and water, and the mountains and rivers are connected, and the distant mountains and waters are integrated. Qi rushed out of Tianshan Mountain with the sky falling, roaring all the way; It's strange that at the widest part of the valley, there are thousands of meters long, and the narrow place can only accommodate two or three meters of waterways, with a line hanging in the sky. Strangely, it bends in the waterway, like a dragon in the world; The famous "Ma He Qi Yu" is produced here. Although priceless jade is available to people, colorful stones can be found everywhere.

location

Kuitun City is located at the northern foot of Tianshan Mountain, on the southwest edge of Junggar Basin, beside the Kuitun River, with 4419'-44 49' north latitude and 84 47'-8518' east longitude, bordering Shawan County in the east, Wusu City in the west, Dushanzi City in the south and Karamay City in the north. It is 253km from Urumqi, the capital of the autonomous region, 243km from Alashankou in the east, 270km from Bole, 450km from Yining, 530km from Karamay 150km from Altay, 380km from Tacheng in the northwest and 540km from Kuqa County, an important town in southern Xinjiang.

geology

Kuitun city is located in the north of Tianshan geosyncline tectonic belt and the south edge of Junggar basin in piedmont depression area, and its tectonic movement is strongly influenced by Variscan, Yanshan, Himalayan and even neotectonic movements. Stratigraphically, it belongs to Hualixi fold belt in North Tianshan Mountain, with complex geological structure and great changes in stratigraphic development.

topography

Kuitun city is located at the edge of the piedmont alluvial fan on the northern slope of Tianshan Mountain, with an altitude of 450 ~ 530 meters. There are no mountains and peaks in the territory. The terrain is high in the southwest and low in the northeast, and the terrain is inclined from southwest to northeast. It is about 50 kilometers south of Tianshan Mountain and 8 kilometers west of Kuitun River. The terrain is high in the southwest and low in the northeast, with the elevation from 6 10 m to 320 m in the north and south, from 6 10 m to 460 m in the east and west, and the vertical slope from the north and south to 10-30‰ in the ground and from 3-5‰ in the east and west.

climate

Kuitun is a continental arid climate with long sunshine hours, scarce precipitation and large evaporation. The annual average temperature is 6.5℃, 1 monthly average temperature-18℃, and the July average temperature is 25.7℃. The sunshine in this area is extremely rich, with an average annual sunshine hours of 2598. 1 hour and an average annual sunshine rate of 58%. Located in the hinterland of Eurasia, it has a continental climate in the north temperate zone. The upper air is influenced by both the westerly weather system and the subtropical weather system. In addition, the Tianshan Mountains, as a barrier to the underlying surface dominated by cold air and Gobi in the north, make it hot in summer and cold in winter, with four distinct seasons, less precipitation, large evaporation, large temperature difference between days (years) and rich light resources.

hydrology

Kuitun belongs to Kuitun River system, with four rivers. The Kuitun River originates from the Tianshan branch, connects with the Gashan Mountain in Khabir, flows through Dushanzi, Wusu, Kuitun and Jinghe River, and flows into Ebinur Lake, with a total length of 220 kilometers. There are mainly 18 tributaries in the upstream, with an average annual flow of 640 million cubic meters and an average annual flow of 20. 1 cubic meter/second. The flood season is from the beginning of June to the end of September, and the dry season is from June 10 to March of the following year. There is a great difference in river flow between winter and summer, which is a typical inland river in arid areas.