Issyk-Kölner Dom area

Mar 05, 12 Issyk-Kölner Dom area

The region is located in the east. parts of Kyrgyzstan. Was established November 21, 1939. Disbanded January 27, 1939, then December 11, 1970 was re-established. October 5, 1988, and the Issyk-Kelskaya Naryn region were combined, and December 14, 1990 they were again transformed into a separate area. Regional center – city of Karakol. The region consists of five districts of the (Ak-Suusky, Jeti-Ogyuzsky, Ton, Tyup, Issyk-Kelsky), three cities (Balykchy, Karakol, Cholpon-Ata), 5 townships (Ak-Bulak, Jyrgalan, kazhy -Say, Ortho-Tokoi, Pier – Przhevalsk), 58 Ail okmetyu, and 181 villages. From the north and north-east region is bordered by Kazakhstan, east and south-east – with China, from the west and south-west of Naryn region, north-west – with the Chu region.

The area of ​​43.1 km2 (21.6% of the plane schadi republic). The population of 413.1 thousand people. (Census 1999), which represents 8.6% of the population.

Nature. The territory is mainly composed of two parts. This Issyk-Kelskaya valley and the Issyk-Kelsky Sirt, surrounded by mountains to the north Teskey Ala-Too mountains to the south separated Kakshaal-Too.

The relief of the whole complex. Issyk-ling Kelskaya to Kungeyskimi surrounded on the north and south mountain ranges Teskeyskimi Ala-Too. At the east. and the west. the ends of the valley ridges Kuhn gay and Teskey Ala-Too, surrounding it with two one hundred Ron, come close to each other about once so distinctive mountain nuyu closed basin. Issyk-Kelskaya Valley associated with the Chu Valley through Boom Gorge, located in the west. In scale, it ranks second in the Central Asian Village le Ferghana Valley. The central part is occupied by Lake Lena to the Issyk-Cal with the adjoining lowland areas schimi. The narrow coastal strip around the lake are covered with soft, convenient for beach sand. Sometimes there are also rocky, covered with rubble, as well as bolotis tye beach. In the south, Teskey Ala-Tooskih mountain races put Sirt, which is a separate nye plains with more severe climatic conditions in E, as these plateau-like sites are well above sea level. Two mountain ranges in the territory of the region, on the east. end close to each other and merged to form the peak of Khan Tenir (Moose Too). This is the highest in Tenir Tooskih mountains Pobeda Peak (7439 m above sea level).

The mineral resources in the area are gold (Kum-Terek deposit is located but the Ak-Shyyrakskoy Hill), coal (Zhergalan, Segettyu), tin (in the valley. Sary-Jaz), complex metals (base metals Zhergalanskaya group), tungsten, copper , bismuth ore, cement raw materials, lime deposits, (Kyurmentyu), but pesoch-gravimnye deposits that are suitable for the production properties of glass, etc. On the basis of a set GOVERNMENTAL Thermal and mineral sources that have curative properties of constructed and continue to operate spas, resort Jeti-Ogyuz, Zhergalan, Ak-Suu, Cholpon-Ata, Blue Issyk-Kul ',' mark ',' Kirghiz beach, etc. In the area there are many sources of therapeutic mud – in Pokrovka Tamga, Zhergalane, Kyurmentyu, Cholpon-Ata, Chok-Tal, et al Ulakole

The climate is directly linked to high-altitude location of the surrounding mountains. The surrounding mountain ranges share Well do not let the cold air mass, which makes frost free all year round mountain lake valley provides extra cushioning, cool air, differing from the atmospheric climate of the valley feru other valleys in the mountains Tenir Too. The average July temperature is close to 18'S. Winters are mild on the southern. and sat. shores of the lake average January temperature is about ra -2