Lably
Skip to content

Issyk-Kul

Lake in northeastern Kyrgyzstan

  • 7 min read
  • 7 chapters
Бұл суретте Қырғыстандағы Иссык-көл көлі
Қайырқан Әсем · CC BY-SA 4.0

Related on Lably

Through Salinity, Ramsar Convention and Biodiversity

The lake is a Ramsar site of globally significant biodiversity and forms part of the Issyk-Kul Biosphere Reserve.

Geography

Issyk-Kul Lake is 182 kilometres (113 mi) long, up to 60 kilometres (37 mi) wide and its surface area is 6,236 square kilometres (2,408 sq mi). It is the second-largest mountain lake in the world behind Lake Titicaca in South America. It is at an altitude of 1,607 metres (5,272 ft) and reaches 668 metres (2,192 ft) in depth.

About 118 rivers and streams flow into the lake; the largest are the Jyrgalang and Tüp. It is fed by springs, including many hot springs, and snow melt. The lake has no current outlet, but some hydrologists hypothesize that the lake's water filters deep underground into the Chu River. The bottom of the lake contains the mineral monohydrocalcite, one of the few known lacustrine deposits.

The lake's southern shore is dominated by the Teskey Ala-Too Range of the Tian Shan mountains. The northern slopes of the range are long and send a considerable flow to Issyk-Kul. Numerous streams taking their rise at the slopes flow together into comparatively large rivers. They deeply dissect the range and flow in wide valleys. On exit from mountains the rivers form large alluvial cones. In the eastern part of Issyk-Kul they flow into the Jyrgalang river. The Kungey Alatau of the Tian Shan runs parallel to the north shore. The southern slopes of the Kungey Alatau are comparatively short and the rivers rising on them are relatively small and do not have a chance to flow together to form larger hydrographic systems. As a result, they separately empty either into Issyk-Kul or into the Tüp river flowing along the range.

The lake water's salinity is approx. 0.6% – compared to 3.5% salinity of typical seawater – and, although the lake level is still currently some 8 metres (26 ft) higher than in medieval times, its level now drops by approximately 5 centimetres (2.0 in) per year due to water diversion.

Administratively, the lake and the adjacent land are within the Issyk-Kul Region of Kyrgyzstan.

Sign in to keep reading

6 more chapters are free with a Lably account.

More in Physical geography