Issyk-Kul
Issyk-Kul (Russian: Иссык-Куль) or Ysyk-Köl (Kyrgyz: Ысык-Көл [ɯsɯ́q kʰɵl]; lit. 'Hot Lake') is an endorheic saline lake in the western Tian Shan mountains in eastern Kyrgyzstan—just south of a dividing range separating Kyrgyzstan from Kazakhstan. It is the eighth-deepest lake in the world, the eleventh-largest lake in the world by volume, and the second-largest saline lake. It is located at an elevation of 1,607 metres (5,272 ft). Despite the elevation and low temperatures during winter, it rarely freezes due to its high salinity.
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 ruggedly beautiful 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 eastern part of Issyk-Kul they flow into 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. Therefore, 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 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 Issyk-Kul Region of Kyrgyzstan.
Tourism
During the Soviet era, the lake became a popular vacation resort, with numerous sanitoria, boarding houses and vacation homes along its northern shore, many concentrated in and around the town of Cholpon-Ata. These fell on hard times after the break-up of the USSR, but now hotel complexes are being refurbished and simple private bed-and-breakfast rentals are being established for a new generation of health and leisure visitors.
The city of Karakol (formerly Przhevalsk, after the Russian explorer Przhevalsky, who died there) is the administrative seat of Issyk-Kul Region of Kyrgyzstan. It is near the east tip of the lake and is a good base for excursions into the surrounding area. Its small old core contains an impressive wooden mosque, built without metal nails by the Dungan people and a wooden Orthodox church that was used as a stable during Soviet times.
History
Issyk-Kul Lake was a stopover on the Silk Road, a land route for travelers from the Far East to Europe. The great Chinese Buddhist scholar-monk Xuanzang passed by this lake and noted the details in the classic travelogue Great Tang Records on the Western Regions in the 7th century. The lake was once a part of the territory of Qing dynasty of China and was ceded to Russia – along with the surrounding territory – after the Treaty of Tarbagatai. In Manchu/Mongol records, the lake was known as Temurtu-Nor, or "Iron Lake".
Many historians believe that the lake was the point of origin for the Black Death that plagued Europe and Asia during the early and mid-14th century. In 2022, researchers reported on the analysis of preserved genetic material from seven individuals buried in two cemeteries near Issyk-Kul and determined that the Black Death was present there in 1338 or 1339. The plague first infected people in a small, nearby settlement of traders eight years before it devastated Eurasia, killing 60 percent of the population, having traveled along trade routes. The lake's status as a byway for travelers allowed the plague to spread across these continents via medieval merchants who unknowingly carried infested vermin along with them.
The lake level is some 8 metres (26 ft) higher than in medieval times. Divers have found the remains of submerged settlements in shallow areas around the lake.
Maksim Menshikov notes that Toru-Aygyr, a settlement near the northwest shore of the lake, was founded in the 13th century. Earthquakes in the 15th century submerged the settlement in to the lake. A Muslim cemetery existed in the settlement and was around 14 acres in size.
Articles identified as the world's oldest extant coins were found underwater, with gold wire rings used as small change and a large hexahedral goldpiece. Also found was a bronze cauldron with a level of craftsmanship that is today achieved by using an inert gas environment.
In 1916 the monastery at Issyk-Kul was attacked by Kyrgyz rebels, and seven monks were killed.
Specially protected areas
The first nature reserve in Kyrgyzstan, Issyk-Kul State Reserve was established in 1948 to protect unique nature landscapes and waterfowl at Issyk-Kul. In 1975, it was acknowledged as a Ramsar site. Biosphere Reserve Issyk-Kul covered by UNESCO World Network of Biosphere Reserves was established in year 2000 within the administrative borders of Issyk-Kul Region.
Key facts
- Type
- endorheic lake, lake, ancient lake
- Area
- 6,236 km²
- Elevation
- 1,606 m
- Heritage status
- Ramsar site
Facts from Wikidata.
Tags
Nearby places
Frequently asked questions
Is there an entry fee to visit Issyk-Kul?
No, the lake itself and its open shoreline are free to visit. Some private resort and sanatorium beaches along the shore charge a small admission for their own facilities.
How do you get to Issyk-Kul?
Most travelers fly into Bishkek's Manas International Airport, then drive roughly 3.5–5 hours through the Boom Gorge to Cholpon-Ata on the north shore, or about 6–7 hours to Karakol. A small Issyk-Kul International Airport near the village of Tamchy also exists, but its scheduled flights are seasonal and limited — check the current schedule before relying on it.
What's the best time to swim in Issyk-Kul?
Mid-July through late August is the most reliable swimming window, with water around 22–24°C. June and September run cooler, roughly 16–20°C, with fewer crowds, while the lake is generally too cold for swimming from October to May.
Why does Issyk-Kul never freeze?
It's a combination of factors: the lake's considerable depth (up to about 668 meters) stores summer heat, the water carries some mineral/salt content, and warm springs feed it from below. That's also the origin of its name, which means "warm lake" in Kyrgyz — a reference to it rarely freezing, not to warm water. Shallow coves in the northeast near Tup have been known to ice over in exceptionally cold winters.
How does the north shore (Cholpon-Ata) differ from the south/east shore (Karakol)?
Cholpon-Ata is the resort town — sanatoriums, beach clubs, the Rukh Ordo cultural center, and an open-air petroglyph site on the edge of town. Karakol is quieter and acts as the gateway to the Tian Shan mountains, with the red rock formations of Jeti-Oguz, the hot-spring valley of Altyn-Arashan, and a wooden Dungan mosque in town.
What activities are available at Issyk-Kul?
Swimming, boating, horse riding, trekking into the Tian Shan (such as the 2–3 day hike to Ala-Kul lake), visiting the Cholpon-Ata petroglyph site, and in winter, skiing at the Karakol ski base.
How long should a visit to Issyk-Kul take?
Three to four days covers one shore properly, but many travelers use the lake as a base for a longer stay, combining beach time with a multi-day trek into the surrounding mountains.
Is Karakol a good base for the mountains and skiing?
Yes. The Karakol ski base sits about 7–10 km from town at roughly 2,300 meters and runs in winter (December–March), while the valleys around the city open up for trekking in summer (June–September).
How does Issyk-Kul compare to Lake Balkhash?
Issyk-Kul is a high alpine lake ringed by the snow-capped Tian Shan, clearer and far more developed for tourism, with resorts, guesthouses, and trekking routes close by. Balkhash is a flat steppe lake in Kazakhstan, half fresh and half brackish, much less developed and quieter, appealing more to anglers and nature-watchers than resort travelers.
Is Issyk-Kul worth visiting?
Yes — it's a rare high-altitude lake that lets you combine beach time with Tian Shan trekking in a single region.
Sources
The text on this page comes from: Issyk-Kul (en.wikipedia.org), as of 25 July 2026
Text is available under CC BY-SA 4.0.
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