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A view of the Salar de Arizaro
A view of the Salar de Arizaro
The dry lakebeds and yardangs in Salar de Arizaro, imaged by NASA's Earth Observing-1 satellite. In the upper left corner, small rounded bumps in the
The dry lakebeds and yardangs in Salar de Arizaro, imaged by NASA's Earth Observing-1 satellite. In the upper left corner, small rounded bumps in the landscape are yardangs, dusty hills formed when soft rocks are weathered and abraded by winds. The yardangs are aligned precisely with the northwesterly winds. On the right, bulbous hills have sharps edges, a formation typical of salt weathering around the base. During salt weathering, rocks are eroded by repeated salt crystal growth. The eroded material has been blown away by the strong winds of the high desert, leaving the sharp edge.
Cono de Arita in Salar de Arizaro
Cono de Arita in Salar de Arizaro
Hexagonal formations in the Salar de Uyuni during the dry season.
Hexagonal formations in the Salar de Uyuni during the dry season.
Natural reflections in the Salar de Uyuni during the rainy season
Natural reflections in the Salar de Uyuni during the rainy season
During the rainy season (December to April), the flat turns into a shallow lake and becomes the world's largest natural mirror, featuring a reflection
During the rainy season (December to April), the flat turns into a shallow lake and becomes the world's largest natural mirror, featuring a reflection of the sky.
Salt production at the salar
Salt production at the salar