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Geological Formation

Tian Shan

Structural and Tectonic Formations

The Tian Shan, also known as the Tengri Tagh or Tengir-Too, is a large system of mountain ranges in Central Asia crossing Kyrgyzstan, China, Kazakhstan, Uzbekistan and Tajikistan, extending about 2,900 kilometers east from Tashkent. Its highest peak, Jengish Chokusu, reaches 7,439 meters in Kyrgyzstan, while its lowest point, the Turpan Depression, lies 154 meters below sea level, positioning the range just north and west of the Taklamakan Desert and the Tarim Basin. The Tian Shan forms part of the Himalayan orogenic belt, raised by the ongoing collision of the Indian and Eurasian tectonic plates during the Cenozoic era, a far-field effect of the same collision that built the Himalayas themselves; its exposed rock is classified as Mesozoic to Cenozoic in age. This entity documents the Tian Shan specifically as a geological formation, a Central Asian mountain system uplifted as a far-field effect of the India-Eurasia collision.

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: Tian Shan

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: Tian Shan
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Tian Shan

Also in Geography Atlas: where this subject is found.

Source Wikidata: Tian Shan

Also in Geography Atlas: where this subject is found.

Source Wikidata: Tian Shan

Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Source Wikidata: Tian Shan
Sources
1. Wikidata: Tian Shan
  • Wikidata Q5474, class allow-list match (w-wdresolver-0926)
  • eastern portion listed as a World Heritage Site at the 2013 Conference on World Heritage
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