The biggest inland salt lake and inland saline lake
LI Mingsheng
In August 1994, on the second day after we reached Golmud, we visited theworld well-known Qarhan Salt Lake.
Along the road north away from the urban areas, we drove on a grayish black road with the smooth and straight surface, which was the rare “Wanzhang Salt Bridge” (a natural salt bridge about 60 kilometers long). This salt bridge looks like a road; however, it was made up by putting rock salts on the salt shell of the lake. Under the salt shell, it was a dry salt lake which was composed of salt bed and inter-crystal brine. This north-south orientated road was 60 kilometers long, paralleling Qingzang railway and crossing the biggest salt lake—“King of the Salt lake” —Qarhan Salt Lake. It is amazing that the road’s maintenance is very convenient. Only need topour bottles of brine on the damaged surface. Once dried up, the road surface is well repaired. Because of its exceptionally gifted characteristic, the “Wanzhang Salt Bridge” has become one of the scenic wonders in Golmud.
Photo Qarhan Salt Lake with abundant salt mine resources |
Return from Golmud to Xi'ning by train, we passed by the famous Qinghai Lake, which is the largest inland saline lake in China (over 4,573 square kilometers, total dissolved solids (TDS )of 15.5g/L). The Qinghai Lake seemed likevast expanse of sea. The water and sky put together and made people completely relaxed and happy.
In history, Qinghai Lake was named as West Sea, also called Xian shui. In Mongolian, it was called Kukunuoer; while in Tibetan, it was called Cuowenbu. Both of them Have the meaning of “blue lake”. With the circumference of 360 kilometer and the height of 3,194 meters, this lake was formed by tectonic movement occurred 40million years ago, Located in an intermountainous basin among the Qilian mountains. According to the research, Qinghai Lake was a freshwater lake, which was connected with the Yellow River Hundreds of thousand years ago. However, because of Climate changes and Tectonic mountains formed by crust faulting and uprising, Connection between yellow river and Qinghai lake was blocked. Meanwhile, Salt in lake is gradually accumulated, and then became a closed interior saline lake.
Photo Rape flower in the lakeside of Qinghai Lake |
The climate in the lake area is suitable for planting rape and highland Naked barley. Leaning against the train window, we could see many yellow rape flowers dotted on the green grassland, adding some coquettish and bright color to the Qinghai lake a little monotonous background, as if we had back to homeland of fish and rice of south of the Yangtze River.
Brief introduction to the author: Li Mingsen, a geographer, graduated from the Geology and Geography Department of Beijing University in 1963. As a researcher of the Commission for Integrated Survey of Natural Resources (one of the two mergers of the Institute of Geographic Sciences and Natural Resources Research in 1999), he has taken part in several scientific expeditions to Southwest China and the Qinghai-Tibet Plateau during the past 40 years. Since 1973, he has been to the Qinghai-Tibet Plateau more than 20 times, and left his footprints in the Himalayas, Yarlung Zangbo Grand Canyon, Qangtang no-human zone and Hengduan mountain region.