Balkhash, Lake

or Lake Balqash

Lake, eastern Kazakhstan.

It is about 375 mi (600 km) long, with a maximum depth of roughly 85 ft (25 m). Its chief feeder is the Ili River, which enters at the southeast in a wide delta. Harsh climate affects its size greatly; its area has varied from about 6,000 sq mi (15,500 sq km) to 7,300 sq mi (19,000 sq km), depending on seasonal precipitation. It is frozen from November to March. Since the mid 20th century, damming and industrial pollution have caused severe ecological damage.

* * *

▪ lake, Kazakstan

Kazak  Balqash 

 lake, situated in east-central Kazakhstan. The lake lies in the vast Balqash-Alaköl basin at 1,122 feet (342 m) above sea level and is situated 600 miles (966 km) east of the Aral Sea. It is 376 miles (605 km) long from west to east. Its area varies within significant limits, depending on the water balance. In years in which there is an abundance of water (as at the beginning of the 20th century and in the decade 1958–69), the lake's area reaches 6,900–7,300 square miles (18,000–19,000 square km). In drought-afflicted periods, however (as at the end of the 19th century and in the 1930s and '40s), the area of the lake decreases to 6,000–6,300 square miles (15,500–16,300 square km). Such changes in area are accompanied by changes in the water level of about 10 feet (3 m). Jutting far out into the lake is the Sarymsek Peninsula, which divides Balkhash into two separate hydrologic parts: a western part, wide and shallow, and an eastern part, narrow and relatively deep. Accordingly, the width of the lake changes from 46 to 17 miles (74 to 27 km) in the western part and 6 to 12 miles (10 to 19 km) in the eastern part. The depth of the western part does not exceed 36 feet (11 m), whereas the eastern part reaches 85 feet (26 m). The two parts of the lake are united by a narrow strait, the Uzynaral, with a depth of about 21 feet (6 m).

      The large Ile River (Ili River), flowing in from the south, spills into the western part of the lake, and it contributed 80–90 percent of the total influx into the lake until a hydroelectric project reduced the volume of the river's inflow late in the 20th century. Only such small rivers as the Qaratal, Aqsū, Ayaguz, and Lepsi feed the eastern part of the lake. With almost equal areas in both parts of the lake, this situation creates a continuous flow of water from the western to the eastern section. The water of the western part was almost fresh and suitable for industrial use and consumption, but that of the eastern part has long been salty.

      The north banks of the lake are high and rocky, with clear-cut traces of ancient terraces. The south banks are low and sandy, and wide belts of them are covered with thickets of reeds and numerous small lakes. These low-lying banks are periodically flooded by the waters of the lake.

      Harsh climatic conditions prevail, and the warm summers and cold winters significantly affect the whole regime of the lake. The average annual water temperature in the western part of the lake is 50° F (10° C); in the eastern part it is 48° F (9° C). Average precipitation is approximately 17 inches (430 mm). The lake remains frozen from the end of November to the beginning of April.

      Carbonates predominate in the ground deposits of the lake. The fauna of the lake was formerly rich but declined from the 1970s owing to the lake's deteriorating water quality. Before these declines began, 20 species of fish inhabited the lake, of which six were peculiar to the lake itself. The remainder had been introduced to the lake and include the sazan, sturgeon, eastern bream, pike, and Aral barbel. The main food fish were the sazan, pike, and Balqash perch.

      The economic importance of Lake Balkhash had greatly increased during the first part of the 20th century. Most significant was the fishing and fish breeding begun in the 1930s. A regular shipping service with a large freight turnover also developed. Also of great economic significance to the region was the construction of the Balqash copper-refining plant, around which the large city of Balqash grew on the north shore of the lake. However, in 1970 the Qapshaghay hydroelectric-power station began operations on the Ile River. The diversion of water to fill the Qapshaghay reservoir and to provide for irrigation reduced the flow of the Ile River by two-thirds and caused a decline in the lake's water level. The surface of Lake Balkhash dropped 7 feet (2.2 m) between 1970 and 1987. The lake has become increasingly saline and has also suffered pollution from the leakage of fuel-storage depots and from copper mining and processing along its shores. Much of the catch from the fishing industry is now quarantined, and the forest and wetland habitats around the lake have shrunk. As of the early 1990s, no action had been taken to reverse the ecological damage done to the lake and its surroundings.

* * *