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Geological Formation

Mount Kailash

Structural and Tectonic Formations

Mount Kailash is a peak in the Gangdise, or Kailash, range of the Transhimalaya in the Tibet Autonomous Region, rising to roughly six thousand six hundred and thirty eight meters. Geologically it lies within the same broad mountain building system produced by the ongoing collision of the Indian and Eurasian tectonic plates that raised the Himalayas, though Kailash itself sits north of the main Himalayan range. The peak is notable for its unusually symmetrical, four sided pyramidal shape, distinct among the surrounding mountains.

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: Mount Kailash

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: Mount Kailash
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Mount Kailash
Sources
Wikidata: Mount Kailash
Wikidata Q229107, class allow-list match (w-wdresolver-0926)View the Source
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