Xuefeng (also known as Xuefeng) is named after years of snow on the top of the mountain. Xuefeng Mountain is located in the central and western parts of Hunan, which is an important mountain range in Hunan. Xuefeng Mountain is located between Yuanjiang and Zishui in the west of Hunan, China, which is the watershed between Zijiang and Shui Yuan. It starts from the border between Hunan Province and Guangxi Zhuang Autonomous Region in the south and is connected with the 80-mile South Mountain. Stop at North Dongting Lake. To the west are the mountains of Xiangxi. To the east are hills in central Hunan. Northeast-southwest trend. Folding fault block mountain. The mountains in the south are steep, and the north is gradually reduced to hills after being cut by endowment water. It is 350 kilometers long. Subaoding, the main peak, is1934m above sea level, located between Yang Mo and Jiankou. The elevation of baimashan, the second peak, is 178 1 m. Vegetation is dominated by subtropical evergreen broad-leaved forest and various Chinese fir, with obvious vertical differentiation. There are mineral resources such as tin. Water resources are abundant. There are reservoirs such as Zhexi, Huangcai and Shuifu Temple in mountainous areas. Langshan Scenic Area is a newly developed tourist attraction and the fourth batch of national key scenic spots. The main battlefields of War of Resistance against Japanese Aggression's last battle in Xiangxi in the later period were Gaosha, Jiangkou, Qingyan and Tieshan in Dongkou County at the eastern foot of Xuefeng Mountain. China, a mountainous area in the west of Hunan Province. Located between Yuanjiang and Zishui. North-north-east-south-southwest, south from the junction of Hunan and Guangxi, connected with Nanling, north to the southwest of Dongting Lake. The southwest part of the mountain is steep, and the elevation of Subaoding, the main peak, is 1, 934 meters. The northeast section is reduced to 500 1 1,000m, and the middle section is only 300,400m above sea level near Yan Xi. The lower reaches of Zishui River cross Xuefeng Mountain at right angles here, forming a canyon between Xinhua and Yan Xi, and the Hunan-Guizhou Railway passes through here. There is a large hydropower project in western Zhejiang. Xuefeng Mountain is rich in Chinese fir resources, and Huitong County is an important Chinese fir forest area, which is famous for its fast growth, high quality and high yield. Phyllostachys pubescens and masson pine are also widely distributed. The southern part of the mountain is close to Nanling, where tropical plants such as Castanopsis fissa, Phoebe bournei and Schima superba grow. [Edit this paragraph] The landform is located in the western mountainous area of Hunan Province, China. It is the watershed of two different natural landscapes, and it is also the watershed of Yuanjiang and Zishui. North-north-east-south-southwest, south from the junction of Hunan and Guangxi, connected with Nanling, north to the southwest of Dongting Lake. The southwest section of the mountain is steep, and the elevation of the main peak, Subaoding, is 1, 934m. The northeast section is reduced to 500 1 1,000m, and the middle section is only 300,400m above sea level near Yan Xi. The lower reaches of Zishui River cross Xuefeng Mountain at right angles here, forming a canyon between Xinhua and Yan Xi, and the Hunan-Guizhou Railway passes through here. There is a large hydropower project in western Zhejiang. Xuefeng Mountain is rich in Chinese fir resources, and Huitong County is an important Chinese fir forest area, which is famous for its fast growth, high quality and high yield. Phyllostachys pubescens and masson pine are also widely distributed. The southern part of the mountain is close to Nanling, where tropical plants such as Castanopsis fissa, Phoebe bournei and Schima superba grow. Xuefeng Mountain belongs to the southwest section of the "primitive Jiangnan ancient land" and has an arc structure protruding from the northwest. A set of strata composed of shallow metamorphic slate, metamorphic sandstone and phyllite are widely distributed in the Lengjiaxi Group and Banxi Group of the Pre-Sinian system, and the metamorphic clastic rocks of the Sinian system are also well developed, which are exposed among the strata composed of slate, limestone and fine sandstone of the Early Paleozoic Cambrian-Silurian system. Due to the uplift of Caledonian movement, a series of north-northeast uplifts and depressions were formed. Under the strong influence of Yanshan movement, a series of NE-trending faults and folds were produced, which further laid the structural and geomorphological pattern of Xuefeng Mountain. Xuefeng Mountain is an ancient uplift mountain with positive structure. It starts from Da Nan Shan at the junction of Hunan and Guangxi in the south and ends in Dongting Lake area, stretching for more than 300 kilometers, with a span of 80 ~ 120 kilometers. There is a mountain ridge with a height of 1000 meters, the elevation of the middle ridge is 1200 ~ 1700 meters, and the elevation of the sub-peak of the main peak is 65433. Under the action of intermittent uplift and external force, the mountain presents multi-level peeling surfaces such as 900 ~ 1 100 meters, 650 ~ 800 meters, 450 ~ 550 meters and 240 ~ 350 meters. The cutting depth of the valley varies from150 ~ 750 m. With the development of the fault, the ridges and valleys fluctuate alternately. On both sides of the whole mountain, the terrain is steep on the east slope and gentle on the west slope. The tributaries of the Yuanjiang River, such as Wushui, Xu Shui and Yiwangxi, Zishui Xiyuan and its tributaries, Pingxi and Chenxi, all come from both sides of the mountain. Two main streams pass through the north-central Xuefeng Mountain, and the river turns in an "S" shape to form a canyon.