Lably
Skip to content

Mount Tai

Mountain in Shandong, China

  • 18 min read
  • 7 chapters
The sacred Mount Tai was the object of an imperial cult for nearly 2,000 years, and the artistic masterpieces found there are in perfect harmony with the natural landscape. It has always been a source
xiquinhosilva · CC BY 2.0

Related on Lably

Through UNESCO, Australia and Earthquake

Mount Tai is known as the eastern mountain of the Sacred Mountains of China. It is associated with sunrise, birth, and renewal, and is often regarded the foremost of the five. Mount Tai has been a place of worship for at least 3,000 years and served as one of the most important ceremonial centers of China during large portions of this period. Because of its sacred importance and dramatic landscape, it was made a UNESCO World Heritage Site in 1987. It meets 7 of the 10 evaluation standards for World Heritage sites, and is listed as a World Heritage site that meets the most of the standards, along with the Tasmanian Wilderness World Heritage Area in Australia.

An earthquake or thunderstorm occurred around Mount Tai in 1831 BC or 1652 BC, also known as the Mount Tai earthquake. This event was first recorded in the Bamboo Annals, and at present, it is recognized by most scholars as the first recorded earthquake in Chinese history.

Location

Mount Tai is located in western Shandong, just north of the city of Tai'an and to the south of the provincial capital Jinan. It extends from 150–1,545 meters (492–5,069 ft) above sea level and covers an area of 426 km2 (164 sq mi) at its base. The Jade Emperor Peak, which rises 1,532.7 meters (5,029 ft) above sea level, is located at 36° 16′N and 117° 6′E.

Geological origin speculation

Mount Tai was formed in the middle of the Cenozoic about 30 million years ago. The stratum of Mount Tai is ancient, mainly composed of several ancient rocks such as mixed rock, mixed granite and various gneiss. The government prevents exploration of the caves, for they are unassessed and potentially dangerous. The Luxi region (including Mount Tai) used to be a huge subsiding belt or sea canal. The orogeny made the rock layers on the subsidence zone folded and uplifted into ancient land, forming a huge mountain system, which has experienced 2 billion years of weathering and denudation, and the terrain has gradually become flat. About 600 million years ago, Mount Tai sank into the sea again. After more than 100 million years, the entire area rose to land again, and the ancient Mount Tai uplifted into a relatively low barren hill. In the late Mesozoic period about 100 million years ago, due to the extrusion and subduction of the Pacific plate to the Eurasian Plate, the Taishan stratum experienced extensive folds and fractures under the influence of the Yanshanian. During the crustal movement above, Mount Tai was rapidly uplifted. In the mid-Cenozoic period about 30 million years ago, the outline of Mount Tai as it is known today was formed.

Climatic vegetation

Due to its height, Mount Tai has a vertical climate gradient. The lower part of the mountain is a warm temperate zone and the top of the mountain is a medium temperate zone. The mountain is cloudy and foggy, with an average annual precipitation of 1132mm, while the surrounding area receives only 750mm. Taishan scattering coverage rate reaches 80%. On the foothills, deciduous forests, broad-leaved coniferous mixed forests, Coniferous forest, alpine shrubs and grass can be seen in sequence. The vertical boundaries of the forest belts are distinct and the vegetation landscapes are different. There are 989 species of seed plants in 144 families, including 433 species of woody plants in 72 families, 556 species of herbaceous plants in 72 families, and 462 species of medicinal plants in 111 families.

Sign in to keep reading

6 more chapters are free with a Lably account.

More in Physical geography