Drive carefully, one lane, from Danba to Erwacao, and the only road along Mozigou goes directly to mosca. Seda route, back to Danba to Dawu, and then to Seda via Luhuo.
Located in the east of Ganzi Tibetan Autonomous Prefecture, Danba County is the east gate of Ganzi Prefecture, bordering Xiaojin County of Aba Prefecture in the east, kangding city, the state capital, in the south and southeast, daofu county in the west, and Jinchuan County of Aba Prefecture in the north and northeast.
Danba County is high in the west and low in the east, with an altitude of 1700-552 1 m. The county seat is located in Zhanggu Town on the Dadu River, with an altitude of 1800 meters, 37 kilometers away from Kangding, the state capital, and 368 kilometers away from Chengdu. According to the data of the seventh census, as of 0: 00 1 1 in June 2020, the permanent population of Danba County was 49,872.
Danba County covers an area of 5,649 square kilometers, and governs 14 townships, 1 town and 2 streets. As of 0: 00 June 2020 165438+ 10 October 1, the resident population of Danba County was 49,872. 2065438+On April 28th, 2009, the Sichuan Provincial People's Government decided that Danba County would withdraw from poverty-stricken counties.
Terrain:
Danba county is 86.9 kilometers wide from east to west and 105 ~ 7 kilometers long from north to south. It belongs to the high mountain area of Minshan Qionglai Mountain. Dadu River runs through the whole territory from north to south, cutting high mountains, and its three-dimensional landform is remarkable. It is a part of the alpine valley in western Sichuan.
The area is covered with high mountains and deep valleys. Danba County is high in the southwest and low in the southeast. The lowest elevation of the county is1700m, the highest elevation is 5820m, and the relative elevation difference is 4120m. Therefore, it has the climatic characteristics of "one mountain with four seasons and ten miles of different days".
Danba County is a mountainous and narrow valley landform. The overall geological structure of the territory is an anticline, which consists of a series of parallel linear folds. The folds are mainly composed of 1 1 folds in Chunniuchang anticline and Danba syncline, and secondary folds are superimposed on each fold.
Fault activity is relatively strong, mainly in NW direction, followed by NE direction, and generally smaller in North-South direction. The most influential Ke Yu-Danba fault runs through the whole territory of Danba. Mainly high mountains and deep valleys, the terrain is high in the west and low in the east, high in the north and low in the south, and the northwest is inclined to the southeast.
Reference to the above content: Baidu Encyclopedia-Danba County