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Geological Formation

Owens Valley

Structural and Tectonic Formations

Owens Valley is an arid valley in eastern California, lying between the Sierra Nevada to the west and the White and Inyo Mountains to the east, on the boundary between the Great Basin and Mojave deserts. The valley is a graben, a block of crust dropped down between two vertical faults, built up over roughly three million years of repeated earthquakes; gravity surveys suggest as much as 10,000 feet of sediment fills the trench beneath the valley floor. Its floor sits around 4,000 feet above sea level while peaks on the Sierra Nevada side, including Mount Whitney, rise past 14,000 feet, making it one of the deepest valleys in the United States. The Sierra Nevada casts a rain shadow over the valley, and large-scale water diversions to Los Angeles have left Owens Lake at its southern end mostly a dry alkali flat. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

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: Owens 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: Owens Valley
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Owens Valley
Sources
Owens Valley (Wikipedia)
Lead section
Quote, Lead section
Owens Valley (Mono: Payahǖǖnadǖ, meaning "place of flowing water") is an arid valley of the Owens River in eastern California in the United States.
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Wikidata: Owens Valley
Wikidata Q2042674, class allow-list match (w-wdresolver-0926)View the Source
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