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Yandang Mountains

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Yandang Mountains

Yandang Mountains or Yandangshan (simplified Chinese: 雁荡山; traditional Chinese: 雁蕩山; pinyin: Yàndàng Shān; lit. 'Wild Goose Pond Mountain(s)') refers, in the broad sense, to a coastal mountain range in southeastern Zhejiang province in eastern China, covering much of the prefecture-level city of Wenzhou (from Pingyang County in the south to Yueqing County in the northeast) and extending to the county-level city of Wenling in Taizhou prefecture. The mountain range is divided in two by the Oujiang River, the two parts being the North Yandang and South Yandang. More narrowly, Yandangshan is also used to refer to Mount Yandang, a specific part of the North Yandang around an ancient caldera near a small town of the same name (雁荡; Yàndàng Zhèn). The highest peaks of North Yandang are located here, and this is also the main tourist spot. In this article, name "Yandang Mountains" is used to refer the mountain range and "Mt. Yandang" to refer to the caldera.

The main peak of North Yandang, Baigangjian (; Bǎigǎng Jiān; 'Hundred-Peak Point'), rises 1,150 m (3,770 ft) above sea level There is a radar station on the peak, which is closed to the public.

In 2004, Yandangshan became National Geological Park and in the beginning of 2005, a member of Global Geoparks Network, with total area of 450 km2 (170 sq mi). The Yandangshan National Forest Park has an area of 841 hectares (2,080 acres), covering Mt. Yandang.

Mt. Yandang is known for its natural environment, arising from its vertical rock faces and pinnacles, mountain slopes with forests and bamboo groves, streams, waterfalls and caves. The area also hosts several temples and shrines, many of them with a long history; characteristic of the temples is that many of them are built inside caves or in mouths of caves.[citation needed]

Yandang Mountains were formed through volcanic activity during the Cretaceous period c. 100-120 million years (Ma) ago. Similar igneous rocks are widespread in SE China, forming a ~400 km (250 mi) wide and ~2,000 km (1,200 mi) long belt of volcanic-intrusive complexes.

Yandangshan caldera is a round volcanicintrusive complex with a diameter of 13 square kilometers (5.0 sq mi), of which the north-east part was destroyed by a later regional fault. Yandangshan volcano erupted in four episodes. The mountain consists of various igneous rocks: ignimbrite, rhyolite, syenite and tuff. The mountain shows often conspicuous layering corresponding to the four different episodes of eruptions, giving rise to terrace-like structures where flatter, forested areas are separated by vertical cliffs.

Mt. Yandang is mostly covered by deciduous and evergreen forests, mixed with some Cunninghamia. Drier ridges can be dominated by small pine trees. There are also some bamboo grooves. Lower slopes and valleys are used for agricultural purposes, for example for growing tea, or as fruit gardens. Herbs and mushrooms collected from the mountain are sold locally.

A number of plant and animal species have been named after Mt. Yandang. A species of sedge, Carex yandangshanica, has been described from Mt. Yandang and two other mountainous locations in Zhejiang. Mt. Yandang has also given its name to Cyclosorus yandangensis, a marsh fern, and Arachniodes yandangshanensis, a holly fern. Among animal species, a mite Eustigmaeus yandangensis has been named after Mt. Yandang, but this has been challenged.

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