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Geological Formation

Goose Lake Valley

Structural and Tectonic Formations

Goose Lake Valley is a high valley in south-central Oregon and northeastern California, at the northwestern corner of North America Great Basin. It is an alluvial basin formed by faulted blocking, with Pliocene and Pleistocene lava flows overlain by Holocene sedimentary deposits; during the Pleistocene the entire valley was covered by a pluvial lake that may have been up to 300 feet deep, which receded into the present endorheic Goose Lake straddling the Oregon-California border. Native Americans inhabited the valley for thousands of years, the Applegate Trail once crossed it, and Lakeview, Oregon is now its largest settlement, with livestock ranching and lumber milling as its main commercial activities. 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: Goose Lake 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: Goose Lake Valley
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Goose Lake Valley
Sources
Goose Lake Valley (Wikipedia)
Lead section
Quote, Lead section
The Goose Lake Valley is located in south-central Oregon and northeastern California in the United States.
View the Source
Wikidata: Goose Lake Valley
Wikidata Q5584091, class allow-list match (w-wdresolver-0926)View the Source
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