Salar de Uyuni, in the Daniel Campos Province of Bolivia's Potosi Department, is the largest salt flat on Earth, covering about 10,582 square kilometers at an elevation of roughly 3,656 meters. It formed as a sequence of prehistoric lakes dried up: the region was covered by the giant Lake Minchin around 30,000 to 42,000 years ago, which gave way to Paleo Lake Tauca roughly 13,000 to 26,000 years ago and then to Lake Coipasa about 11,500 to 13,400 years ago, with each successive lake leaving behind a thicker deposit of dissolved salts as it evaporated. Today the surface is an 8-meter-thick crust of salt so flat that elevation varies by less than a meter across the entire expanse. Beneath that crust, brine holds lithium at a concentration of about 0.3 percent, and Bolivia's reserves there, estimated at around 23 million tonnes as of 2024, represent roughly 22 percent of the world's known lithium. This entity documents Salar de Uyuni specifically as a geological formation, an evaporite deposit left by the drying of a chain of Pleistocene lakes.
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Protected StatusIUGS Geological Heritage Site 1 Connections
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Source Wikidata: Salar de Uyuni
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1. Salar de Uyuni (Wikipedia)
Category: Second 100 IUGS Geological Heritage Sites
Wikipedia category: Second 100 IUGS Geological Heritage Sites
In Group: Salt Flats and Playas, Lead sentence
Salar de Uyuni is the largest salt flat in the world, with an area of approximately 10,582 square kilometres (4,086 mi2). It is situated in southwestern Bolivia, within the Daniel Campos Province of the Potosí Department, near the crest of the Andes Mountains, at an elevation of 3,656 m (11,995 ft) above sea level.
View the SourceWikidata: Salar de Uyuni
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