Taimu Mountain

Taimu mountain is located in Fuding City on the border of Fujian and Zhejiang. It is 118 kilometers north to Wenzhou and 200 kilometers south to Fuzhou. Tongsan Expressway and Wenfu Railway pass through it, with convenient transportation. It stands on the coast of the East China Sea, with mountains and seas depending on each other. It is known as "Grand View of mountains and seas" and "fairyland city on the sea". The scenic area covers an area of 24.6 square kilometers. It is famous for its precipitous mountains, grotesque rocks, secluded caves and clouds.

Taimu Mountain

This entry is compiled and applied by "popular science China" Science Encyclopedia

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Taimu mountain is located in the northeast of Fujian Province. In a narrow sense, Taimu mountain refers to the mountainous area of Qinyu town in the south of Fuding City, with Fuding peak as the center. It is also the core area of Taimu mountain scenic spot. It is 45 kilometers south of Fuding City, about 120 degrees east longitude and 27 degrees north latitude. It stands on the coast of the East China Sea, facing the sea on three sides and mountains on one side. The main peak is 917.3 meters above sea level. In a broad sense, Taimu mountain refers to a series of mountains, or Taimu mountains, which are distributed between the east of Jiaoxi and the East China Sea in the northeast of Ningde City.

It is said that in the Yao Dynasty, the old mother planted blue (bluegrass, whose juice is blue, which is used to dye cloth) in the mountains. When she met the Taoist priest, she emerged as an immortal, so she was named "Tai Mu" and later changed to "Tai Lao". It is said that the immortals of the East China Sea gather here all the year round, so it has a good reputation as the "fairy capital on the sea". Wuyi, Tailao and Yandang constitute the three famous mountains in Fujian and Vietnam.

Taimu mountain is the watershed between Jiaoxi, Fuding and Xiapu. The mountain is mainly composed of Mesozoic volcanic rocks and granites. The mineral resources in the mountain are mainly lead, zinc, silver, cadmium, alunite, quartzite, kaolin, basalt, etc. The forest coverage rate is over 46%.

Taimu mountain scenic spot, located in Fuding City, the northeast end of Taimu mountain, is a national scenic spot. At the same time, Taimu mountain is the only peak forest landform developed on the terrain of granite hills in China, and the only peak forest landform on the crystal cave granite belt in China. It was listed in the World Geopark in 2010.

In order to pay homage to the medical workers and other special dedication occupations who are struggling in the front line of fighting against the epidemic situation, the scenic spot will be open to the national medical workers and others free of charge from the date of resumption of operation to December 31, 2020.

Location context

Taimu mountain (vein) is located in the east of Ningde City, between 119 ° 40 ′～ 120 ° 25 ′ E and 26 ° 42 ′～ 27 ° 25 ′ n. South Yandang Mountain in the north, Sansha Bay in the south, Jiufeng mountains across the river in the West and the seashore in the East. Winding in Fuding, Zherong, Xiapu, Fuan county (city) territory. Generally, the altitude is 400-700 meters. Dongshanding, the highest peak, is 1479 meters above sea level. Located in the east of Zherong county. The main peak covers Dingfeng, 917 meters above sea level, and is located in the south of Fuding City. It is the watershed between Jiaoxi (Changxi) and Fuding and Xiapu. The mountain is mainly composed of Mesozoic volcanic rocks and granites. The mineral resources in the mountain are mainly lead, zinc, silver, cadmium, alunite, quartzite, kaolin, basalt, etc. The forest coverage rate is over 46%. Fenshuiguan and dieshiguan are the key passes between Fujian and Zhejiang, and Taimu mountain is a famous scenic spot in the whole province.

Main peaks

Dongshan, also known as Yuhu mountain and Dongshi mountain, is located in the east of Zherong county and belongs to the middle part of Taimu mountain range. Dongshan, the main peak, is 1479 meters above sea level, the highest peak in Zherong county. The mountain slopes from northwest to Southeast. It is the birthplace and watershed of Xiyang River, Longxi River and Chixi river. Geologically, it belongs to Mesozoic volcanic rock and granite structure. Mu Haijian, also known as wanghaifeng. At the junction of Xiapu and Zherong counties, it belongs to the middle part of Taimu mountains. Because of the high mountains, you can see the sunrise in the East China Sea, so it's named. The main peak is 1192.4 meters above sea level. The mountains incline from northwest to Southeast and reach the seaside. It is the birthplace of Luohan River, Zhexi River, Qidu River and Xiyang river. Geologically, it belongs to Mesozoic volcanic rock and granite structure. There is a stone pond at the top of the peak that never dries up. Xiapu mountain, in the southwest of Xiapu, belongs to the southern part of Taimu mountain. Yantian port in the west, Dongwuyang in the East, Xiapu in the south. Because there are four islets in the river, green, black, dark and yellow, and the sun reflects the river like rosy clouds. The mountain is on it, so it is named. The main peak of xiapujian, 776.8 meters above sea level, is one of the famous coastal mountains in Sansha Bay. Hongshan, also known as gehongshan. In the south of Xiapu County, it is said that Ge Hong was once an immortal here, so he was named. The main peak is 605.2m above sea level. You can see the scene of Wentai from a distance. There are stone caves on the mountain. There are stone screens, stone tables, chess games, and six character characters in the cave, which people can't recognize. Shanbei ancient county village is governed by Maju County of Jinwen.

Yakou pass

Fenshuiguan and dieshiguan are the key passes between Fujian and Zhejiang,

geographical environment

Geology and geomorphology

Taimu mountain is located in the continental margin of the southeast of Eurasia and the southeast edge of Eurasia plate. It is connected with the Pacific plate by island arc and trench in the East and formed in the long-term relative action of the two plates. In stratigraphic division, the South China stratigraphic area is divided into southeast coastal stratigraphic division, the Northeast belongs to Wenzhou stratigraphic District, and the rest belongs to Qingtian Zhangzhou stratigraphic district.

According to the geological structure, Taimu mountain is located in the Neocathaysian structural belt near the Pacific Ocean on the continental margin of East Asia and in the north of Yanshan volcanic fault zone in East Fujian. The geological structure is formed by multiple tectonic movements. The basic framework of the structural line is NNE and NE strike, which is mainly characterized by the intrusion and eruption of magmatic rocks in different periods (Times) along the structural line, as well as the NNE and NE trending major faults and the topography, topography and water system characteristics controlled by them.

It is located in the volcanic belt along the southeast coast of China. According to the lithologic genetic conditions, the rocks in this area can be divided into magmatic rocks, sedimentary rocks (including pyroclastic sedimentary rocks and normal sedimentary rocks) and metamorphic rocks. According to the lithologic composition and grain size, the rocks in the whole area can be roughly divided into seven types: acidic rocks (about 90.1% of the land area), neutral rocks (6.0%), basic rocks (0.15%), argillaceous rocks (1.7%), sandy rocks (1.3%), purple rocks (0.7%) and carbonaceous acid rocks (0.05%).

In geomorphology, most of Taimu mountain belongs to tectonic erosion and denudation Hilly Basin valley terrain. Generally, the altitude is less than 500 meters, the relative height is 200-400 meters, and the slope is 10-30 degrees. It is characterized by overlapping peaks and hills, broken surface, crisscross rivers, scattered basins and valleys among mountains. At the same time, on the basis of the early geological structure, due to the strong erosion of flowing water, the landform of hills, valleys and basins mainly composed of high hills were formed. Only in coastal areas, isolated low mountains were occasionally seen. Fuan basin was formed between Taimu mountain and Jiufeng Mountain.

hydrology

It is the watershed between Jiaoxi (Changxi) and Fuding and Xiapu. The West foot is mainly the tributary of Jiaoxi River on the east bank, and the east foot is mainly the river flowing into the sea alone.

Donglu River

Chixi is located in the southwest of Fuding. Its main tributaries are sangyuan River, Ziping River and chaxikou. Originated in zhayang, Zherong County, the first Jianshan mountain flows through Shishan, sangyuan and Chixi, and then flows into Yacheng in Xiapu and into the sea, with a drainage area of 287.2 square kilometers. The main stream is 37.6 km long with an average annual runoff of 346 million cubic meters.

Shuibeixi, originated in Zhejiang Province, flows through Fuding county and joins shachenggang. The drainage area is 341 square kilometers, and the main stream is 43.4 kilometers long, with a gradient of 7.69 ‰.

Qidu River, which originates from Fuding County, has a main stream of 58 km long and a drainage area of 334 square kilometers. The average annual runoff is 418 million cubic meters, and the average annual flow is 13.24 cubic meters per second. The river gradient is 16.2%.

Beixi, the largest river in Xiapu County. It originates from Baiyang Township and flows from chongru to Yantian to the sea from north to south. The main stream is 45 km long with a drainage area of 285.2 square km. The river gradient is 16.4 ‰. The average annual runoff is 314 million cubic meters and the average annual flow is 9.5 cubic meters per second.

Luohan River, originated from toubotou village, Baiyang Township, Xiapu County, flows from northwest to Southeast. Its main tributary is Tongyou River, which joins with the main stream under wukengyan and flows through Jiangbian, Qiaotou and Hougang to the sea. The main stream has a total length of 38 km and a total drainage area of 206.4 square kilometers. The average annual runoff is 227 million cubic meters, the average annual runoff is 7.8 cubic meters per second, and the river slope is 22.8 ‰.

Baibu River, originated from the southern foot of Wangfu mountain in Guanyang, Fuding, flows through wengxi, Yeju, tiyang and Bailin, and joins shachenggang. Its drainage area is 122 square kilometers, and its main stream is 26.1 kilometers long.

Xilu River

Xitouxi is located in Guanyang, northwest of Fuding county. The main tributaries are Xitou River and Xiyang river. It originates from zhayang in Zherong county and flows through Fuding, Guanyang, Guanghua, qiantou and Chulou to Jiaoxi. The drainage area is 125.2 square kilometers, the main stream is 29.5 kilometers long, and the average annual runoff is 146 million cubic meters.

Xiyang stream, also known as Liuqiao stream, originates from qinglangang (yuanyangtou village, Dongyuan township) in Fuxi Township, Zherong county. It flows southward in twists and turns until Xiping village of Zhaizhong Township meets with Xixi stream. It leaves at jiaxikou near chongjiuwan village and Xiapu village. Then it flows southward through Fuan Xibing and flows into Saijiang River downstream of Jiaoxi stream. In the county

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