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Geological Formation

Panamint Valley

Structural and Tectonic Formations

Panamint Valley is a long basin in the northeastern Mojave Desert of eastern California, lying east of the Argus and Slate ranges and west of the Panamint Range. It is an endorheic basin whose drainage never reaches the ocean, with a central salt flat that can fill with a shallow, short-lived lake after rain; during the wetter Pleistocene it held Lake Panamint, which connected to Lake Manly in nearby Death Valley. The valley runs roughly 65 miles from the Panamint Dunes in the north to the Naval Air Weapons Station China Lake in the south, and is more than 10 miles wide in places such as Hall Canyon. It contains the ghost town of Ballarat and the Panamint Springs Resort, the valley's only lodging and services, and Barker Ranch, at its southern end, was Charles Manson's final hideout. 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: Panamint 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: Panamint Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Panamint Valley
Sources
Panamint Valley (Wikipedia)
Lead section
Quote, Lead section
Panamint Valley is a long basin located east of the Argus and Slate ranges, and west of the Panamint Range in the northeastern reach of the Mojave Desert, in eastern California, United States.
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Wikidata: Panamint Valley
Wikidata Q643844, class allow-list match (w-wdresolver-0926)View the Source
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