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Geological Formation

Khan Tengri

Structural and Tectonic Formations

Khan Tengri stands at the China-Kyrgyzstan-Kazakhstan tripoint east of Lake Issyk-Kul, in the Tian Shan range of Central Asia. Its rocky summit reaches about 6,995 meters, while its permanent glacial icecap extends the peak's effective height to about 7,010 meters, a distinction that lets mountaineers count it among the 7,000-meter peaks eligible for the Soviet-era Snow Leopard mountaineering award. It is a non-volcanic peak raised by the same tectonic processes uplifting the wider Tian Shan system, its sharp marble-and-granite pyramid famous for catching alpenglow in a striking reddish color at sunset. This entity documents Khan Tengri specifically as a geological formation, a Tian Shan peak whose glacial icecap qualifies it as a 7,000-meter summit for mountaineering purposes.

Facts
Classification
Protected Status
UNESCO World Heritage Site 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Khan Tengri

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Khan Tengri
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Khan Tengri

Also in Geography Atlas: where this subject is found.

Source Wikidata: Khan Tengri

Also in Geography Atlas: where this subject is found.

Source Wikidata: Khan Tengri
Sources
1. UNEP-WCMC and IUCN, World Database on Protected Areas: WDPA protected areas at the location of Khan Tengri
UNEP-WCMC and IUCN, World Database on Protected AreasWDPA feature: Xinjiang Tianshan
Quote, WDPA feature: Xinjiang Tianshan
"desig_eng": "World Heritage Site (natural or mixed)"
View the Source
Wikidata: Khan Tengri
Wikidata Q211529, class allow-list match (w-wdresolver-0926)View the Source
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