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Geological Formation

Yarlung Valley

Valleys

The Yarlung Valley is formed by the Yarlung Chu, a tributary of the Tsangpo River, in the Shannan Prefecture of the Tibet Autonomous Region of China. The name refers especially to the district where the Yarlung Chu joins the Chongye River and broadens into a plain about 2 kilometers wide before flowing into the Tsangpo, and it includes Tsetang, one of Tibet's largest cities, 183 kilometers southeast of Lhasa. Originally well forested and suited to agriculture, the valley and the adjoining Chongye Valley formed the original seat of the Yarlung dynasty of Tibetan kings, until the first Tibetan emperor, Songtsen Gampo, moved the capital to Lhasa. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Erosion, Processes

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

Source Wikidata: Yarlung Valley

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: Yarlung Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Yarlung Valley
Sources
Yarlung Valley (Wikipedia)
Lead section
Quote, Lead section
The Yarlung Valley is formed by Yarlung Chu, a tributary of the Tsangpo River in the Shannan Prefecture in the Tibet autonomous region of China.
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Wikidata: Yarlung Valley
Wikidata Q2296063, class allow-list match (w-wdresolver-0926)View the Source
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