Aydingkol Lake |
Travel in Xinjiang | |||
It has a long history going back about 250 million years. The raising of the Himalayas about 200 millions years ago created the lake. Ten thousand years ago it was a freshwater lake and was 1,000 times larger than its current size. Natural forces affected its elevation and once it became land locked so mineral deposits began to accumulate. During the winter of 1948, the lake basin was once filled with freshwater, which primarily originated from melted snow water from the mountains, as well as supplementary groundwater; owing to the lesser use of water to irrigate cultivated land during the winter, the water level was higher. During the summertime, the water level declined as a result of increased use of irrigation water for Aydingkol Lake conprises three parts. The outer area is salt flats, and due to severe evaporation, the ground is rock hard. The middle area is a salt marsh full of silts. The inner area consists of brackish water and crystal salt. In ancient times, Ayding Lake was known as Jueluowan (jiào luò huàn 觉洛浣). The Uyghur derived name Aydingköl means "moon lake" because of the reflective nature of the salt crystals. Now the lake is a salt puddle. The lake is highly mineralized and contains rock salt, Glauber's salt, glauberite, gypsum, etc. The reserves of salt and Glauber's salt exceed 300 million tons, an important source of raw materials to chemical industries. There is now a chemical plant on the lake front. Due to the high concentrations of salt in the lakebed, neither fish nor bird will be found around the area of the lake.
Admission Fee : CNY 10
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