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What are the characteristics of Wuyi Mountain? Draw them in the text with horizontal lines.
Wuyishan is characterized by its peculiar shape and steep mountain.

The specific introduction of Wuyi Mountain:

Wuyishan is located at the junction of Jiangxi Province and the northwest of Fujian Province, with a total area of 999.75 square kilometers, at the southeast foot of the northern section of Wuyishan. It is a famous scenic tourist area and summer resort in China. It is a typical Danxia landform and one of the first national key scenic spots. Wuyishan is a famous mountain of three religions.

Wuyishan has been the habitat of Liu Yu's Zen family since Qin and Han dynasties, leaving many temples, Taoist temples and the former site of Antang. Wuyishan was once a place where Confucian scholars preached Taoism and gave lectures.

199965438+February, Wuyi Mountain was listed as a dual heritage of world culture and nature by UNESCO in the World Heritage List (No.911) according to the criteria of world heritage selection (Ⅲ), (ⅶ) and (ⅹ).

Other introductions:

2065438+On July 9, 2007, Wuyishan Mountain in Jiangxi Province successfully applied for the World Heritage and was listed as a world cultural and natural heritage. Wuyishan will be open to medical workers (including Hong Kong, Macao and Taiwan) free of charge from the date of reopening to February 3, 20201. Wuyishan is mainly composed of pre-Sinian and Sinian metamorphic rock series, Mesozoic volcanic rocks, granite and clastic rocks.

In the late Mesozoic, a strong volcanic eruption occurred in Wuyishan, followed by a large-scale granite intrusion. It has been found that there are abundant volcanic institutions in this area, which is a typical structural feature of the Pacific Rim region in East Asia. The late Cretaceous red glutenite is the main body of Danxia landform.

Mesozoic crustal movement laid the basic skeleton of Wuyishan landform. The development of Wuyishan landform is also obvious. The peaks above 1500m in the west are basically composed of tuff lava and rhyolite.

In the eastern red sandstone shale area, there are often wider valleys and basins. Therefore, the rich landform types in Wuyishan are the result of comprehensive actions such as geological structure, flowing water erosion, weathering erosion and gravity collapse.