Zhangjiajie

Zhangjiajie (simplified Chinese: 张家界; traditional Chinese: 張家界; pinyin: Zhāngjiājiè) is a prefecture-level city in the northwestern part of Hunan province, People's Republic of China. It comprises the district of Yongding and counties of Cili and Sangzhi. Within it is located Wulingyuan Scenic Area which was designated a UNESCO World Heritage Site in 1992 as well as an AAAAA scenic area by the China National Tourism Administration.

History

The city itself was previously named Dayong (大庸), and has a recorded history dating back to 221 BC. Humans lived here along both banks of the Lishui River (the mother river in Zhangjiajie), now within the boundaries of Zhanagjiajie City, very early during the Stone Age. Human settlement in this region dates back 100,000 years, rivaling such famous sites as Xi’an, Beijing and others. In 1986, the Academy of Chinese Social Science discovered Stone Age relics in Cili County, unearthing 108 articles of stoneware; mostly tapered-form, hacked-tamped and plate-shaped works. According to archaeological experts’ textual research, all of these wares were produced about 100,000 years ago. Shortly thereafter, in 1988, the Archaeological Institute of Hunan Province found other relics in Sangzhi County, including three pieces of stoneware which were estimated to have been fashioned over 100,000 years ago.

National Forest

National Forest may refer to:

See also

Forest Park

Forest Park may refer to:

Towns and villages

Parks

Neighborhoods

Public schools

National park

A national park is a park in use for conservation purposes. Often it is a reserve of natural, semi-natural, or developed land that a sovereign state declares or owns. Although individual nations designate their own national parks differently, there is a common idea: the conservation of 'wild nature' for posterity and as a symbol of national pride. An international organization, the International Union for Conservation of Nature (IUCN), and its World Commission on Protected Areas, has defined "National Park" as its Category II type of protected areas.

While this type of national park had been proposed previously, the United States established the first "public park or pleasuring-ground for the benefit and enjoyment of the people", Yellowstone National Park, in 1872. Although Yellowstone was not officially termed a "national park" in its establishing law, it was always termed such in practice and is widely held to be the first and oldest national park in the world. The first area to use "national park" in its creation legislation was the US's Mackinac Island, in 1875. Australia's Royal National Park, established in 1879, was the world's third official national park. In 1895 ownership of Mackinac Island was transferred to the State of Michigan as a state park and national park status was consequently lost. As a result, Australia's Royal National Park is by some considerations the second oldest national park now in existence.

Zhangjiajie National Forest Park

The Zhangjiajie National Forest Park (Chinese: 湖南张家界国家森林公园; pinyin: Húnán Zhāngjiājiè Guójiā Sēnlín Gōngyuán; literally: "Hunan Zhangjiajie National Forest Park") is a unique national forest park located in Zhangjiajie City in northern Hunan Province in the People's Republic of China. It is one of several national parks within the Wulingyuan Scenic Area.

History

In 1982 it was recognized as China's first national forest park with an area of 4,810 ha (11,900 acres). Zhangjiajie National Forest Park is part of a much larger 397.5 km² (153.5 sq mi) Wulingyuan Scenic Area. In 1992, Wulingyuan was officially recognized as a UNESCO World Heritage Site. It was then approved by the Ministry of Land and Resources as Zhangjiajie Sandstone Peak Forest National Geopark (3,600 square kilometres (1,400 sq mi)) in 2001. In 2004, Zhangjiajie Geopark was listed as a UNESCO Global Geopark.

The most notable geographic features of the park are the pillar-like formations that are seen throughout the park. Although resembling karst terrain, this area is not underlain by limestones and is not the product of chemical dissolution, which is characteristic of limestone karst. They are the result of many years of physical, rather than chemical, erosion. Much of the weathering which forms these pillars are the result of expanding ice in the winter and the plants which grow on them. The weather is moist year round, and as a result, the foliage is very dense. The weathered material is carried away primarily by streams. These formations are a distinct hallmark of Chinese landscape, and can be found in many ancient Chinese paintings.