Chaka Salt Lake is located at No. 9, Salt Lake Road, Chaka Town, Ulan County, Haixi Mongolian Tibetan Prefecture, Qinghai Province. "Chaka" is a Tibetan language, which means salt pond, and "Dabxun Nur" in Mongolian language, which is the sea of green salt.
Chaka Salt Lake has an average altitude of 3059 meters, a lake area of 154 square kilometers, and a scenic area of 30 square kilometers. This is an important stop of the ancient Silk Road, and the intersection of National Highway 109 and National Highway 315. It is 298km east of Xining, the provincial capital, and 200km west of Delingha. It is known as the east gate of the Qaidam Basin.
The Chaka Salt Lake is surrounded by snow mountains. The calm lake is like a mirror, reflecting the beautiful and intoxicating sky scenery. It is known as "the mirror of the sky in China". Being in the world of salt, walking on the lake is like walking on clouds. The water reflects the sky and the sky touches the earth. Walking between lakes is like swimming in a painting.
Chaka Salt Lake has beautiful scenery all the year round. In spring, white clouds hanging low in the sky fall on the lake water. It is unclear whether the salt is whiter or the clouds are whiter; In summer, the rippling lake water is as green as emerald, refreshing people's hearts; The dry lake in autumn is clean and ice, flat and boundless; The desolation in winter is more challenging.
Chaka Salt Lake is also famous for its abundant green salt, becoming the first green edible salt production base in China. In recent years, it has enjoyed a high reputation in the international and domestic tourism circles and the scenery tour of the Qinghai Tibet Plateau due to its production and tourism. The number of tourists has increased year by year. It has been rated as one of the "55 places to go in one's life" by the National Tourism Geography magazine, and has become another beautiful golden card of the beautiful Qinghai.
| Chinese name | Chaka Salt Lake |
| Foreign name | CakaSaltLake |
| geographical position | South of Wulanchaka Town, Haixi Prefecture, Qinghai Province |
| Climate type | Plateau continental climate |
| Lake area | 105 square kilometers |
| Lake elevation | 3059m |
| Official telephone | 0977-8246999，0977-8240129 |
| Opening Hours | 6:00-22:00 all year round |
Panorama VR
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Chaka Salt Lake Formation and evolution
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake Watershed characteristics
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake Water system composition
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake hydrographic features
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake socioeconomic
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake Tourism information
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake Related events
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
Chaka Salt Lake album
Chaka Salt Lake Causes
Due to plate movement, the junction area between the Eurasian plate and the Indian Ocean plate, which was originally covered by sea water, gradually rose into the Qinghai Tibet Plateau. During the formation of the Qinghai Tibet Plateau, part of the seawater accumulated in low-lying areas and formed many salt lakes and ponds, including Chaka Salt Lake.
Chaka Salt Lake Circumstances change
About 100000 to 130000 years ago, Chaka Salt Lake was an outflow lake, flowing eastward into the Gonghe Basin and the Yellow River. Later, tectonic uplift occurred, making Chaka Salt Lake an inland lake. During the late glacial period, Chaka Salt Lake was a freshwater lake. Since the Holocene, the Chaka Salt Lake began to shrink, and salt deposits appeared. Even in the climate suitable period of the middle Holocene, the Chaka Salt Lake still showed a further shrinking state. In the late Holocene, the shrinkage and salinization of salt lakes were further intensified. The effect of temperature plays a vital role in the formation and evolution of Chaka Salt Lake. Compared with the late glacial period, the increase of Holocene temperature caused the evaporation of the salt lake to increase much more than the precipitation.
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