Landscape, geology and hydrology
Jiuzhaigou's landscape is made up of high-altitude karsts shaped by glacial, hydrological and tectonic activity. It lies on major fault lines on the diverging belt between the Tibetan Plateau and the Yangtze Plate, and earthquakes have also shaped the landscape. The rock strata is mostly made up of carbonate rocks such dolomite and tufa, as well as some sandstone and shales.
The valley includes the catchment area of three gullies which due to their large size are often called valleys themselves, and is one of the sources of the Jialing River, part of the Yangtze River system. The area covering 720 km² 278 mi² of the Minshan mountains provides the catchment for the water system of Jiuzhaigou.
Jiuzhaigou's best-known feature is its dozens of blue, green and turquoise-colored lakes. Originating in glacial activity, they were dammed by rockfalls and other natural phenomena, then solidified by processes of carbonate deposition travertine. Jiuzhaigou's water has a high concentration of calcium carbonate, making it so clear that the bottom is often visible even at high depths. The lakes vary in color and aspect according to their depths, residues, and surroundings.
Understand
Jiuzhai Valley Jiuzhaigou is a major feature of the Sichuan Scenic Area, located 350 km north of Chengdu, the capital of Sichuan province. Jiuzhaigou is at the northeastern end of this scenic area in the Min Shan mountains. It is part of the Aba Tibetan and Qiang Autonomous Prefecture. The main scenic area stretches 80 km 50 mi long in the form of a letter Y comprising of three main valleys - Shuzheng, Rize and Zechawa covering 720 km² 278 mi² and offering stunning views of lakes, waterfalls, and mountains. The name means "Valley of Nine Villages", derived from the 9 ancient Tibetan villages that call it home. Its highest point is 4,700 m 15,420 ft above sea level, with the main sightseeing areas between 1,980 m and 3,100 m 6,500-10,170 ft.
Flora and fauna
The park is the natural habitat for two of Chinaâs most treasured endangered species â the Giant Panda and the Sichuan Golden Snub-Nosed Monkey éä¸ç´. However, due to the park's size and the number of tourists, the chances of seeing them are slim. About 20 pandas reportedly live within the boundaries of the park. There is probably higher chance of seeing them in Zaru Valley, the valley dedicated to eco-tourism as of July 2009. In the main valleys you are more likely to see other creatures including birds 140 species have been recorded here, insects and fish.
Despite all the lakes in the park, Jiuzhaigou is amazingly free of mosquitoes.
Nearly 300 km² 115 mi² of the core scenic area is covered by virgin mixed forests. The flora changes greatly with altitude. In the lower regions of the valley, grasses and reeds abound. These are quickly replaced by bamboo forests which in turn give way to deciduous trees and conifers at the upper end of the valley. Beyond them the rocky slopes and snow-capped peaks of the Min Shan range dominate the view.
History
The remote region was inhabited by various Tibetan and Qiang peoples for centuries, but was not officially discovered by the government until 1972. Extensive logging took place until 1979, when the Chinese government banned such activities. The area was made into a national park in 1982. An Administration Bureau was established and the site officially opened to tourism in 1984. Layout of facilities and regulations were completed in 1987. The site was inscribed by UNESCO as a World Heritage Site in 1992 and a World Biosphere Reserve in 1997.
In 2007, over 2.5 million people visited Jiuzhaigou. The site averages 7,000 visits per day, with a publicly reported cap of 12,000 however this is never enforced. The desire to balance environmental protection and mass tourism has become an increasingly acute challenge for park management. Exploitation of natural resources for financial gain in the form of mass tourism is the utmost priority.