Government stocks are zero in all categories. These districts are respectively, near Lake Balkhash (in south-eastern Kazakhstan), in northern Kazakhstan. Usage Statistics for www.livingstonco.ky.gov Summary Period: March 2018 - Referrer Generated 01-Apr-2018 01:23 EDT.

Contents • • • • • • • • • • • • • • • History and naming [ ] The present name of the lake originates from the word 'balkas' of, and which means 'tussocks in a swamp'. From as early as up until the 8th century, the Balkhash was known to the as 布谷/布库/布苏 'Pu-Ku/Bu-Ku'. Drajvera na yarkostj ekrana samsung s3. From the 8th century on, the land to the south of the lake, between it and the mountains, was known in as Jetisu 'Seven Rivers' ( in ). It was a land where the nomadic and of the mingled cultures with the settled peoples of Central Asia. During China's (1644–1911), the lake formed the northwestern-most boundary of the Empire.

In 1864, the lake and its neighboring area were ceded to under the. With the dissolution of the in 1991, the lake became part of. Garmin mobile xt windows ce 6 download full. The origin of the lake [ ]. The numbers mark the largest peninsulas, island and bays: • Saryesik peninsula, separating the lake into two parts, and Uzynaral Strait • Baygabyl Peninsula • Balai Peninsula • Shaukar Peninsula • Kentubek Peninsula • and Ortaaral Islands • • Shempek Bay • Saryshagan Bay The lake includes several small basins. In the western part, there are two depressions 7–11 meters deep. One of them extends from the western coast (near Tasaral Island) to Cape Korzhyntubek, whereas the second lies south from the Gulf Bertys, which is the deepest part of western Balkhash. The average depth of the eastern basin is 16 m and the maximum depth of the eastern part (and of the lake) is 26 m.

The average depth of the lake is 5.8 m, and the total volume of water is about 112 km 3. The western and northern shores of the lake are high (20–30 m) and rocky; they are composed of such rocks as,,, and and keep traces of ancient terraces.

The southern shores near the Gulf Karashagan and Ili River are low (1–2 m) and sandy. They are often flooded and therefore contain numerous water pools. Occasional hills are present with the height of 5–10 m.

The is very curvy and dissected by numerous bays and coves. The large bays of the western part are: Saryshagan, Kashkanteniz, Karakamys, Shempek (the southern pole of the lake), and Balakashkan Ahmetsu, and those in the eastern part are: Guzkol, Balyktykol, Kukuna, Karashigan. The eastern part also includes peninsulas Baygabyl, Balay, Shaukar, Kentubek and Korzhintobe. The lake contains 43 islands with a total area of 66 km 2; however, new islands are being formed due to the lowering of water level, and the area of the existing ones is increasing. The islands of the western part include and (the largest), as well as Ortaaral, Ayakaral and Olzhabekaral. The eastern islands include Ozynaral, Ultarakty,.