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Tufa and Casseopia

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Tufa is a type of limestone that is formed when calcium-rich spring water mixes with the carbonate-rich Mono Lake water and precipitates around the spring. The towers grow underneath the waters surface. These towers were exposed when the city of Los Angeles diverted four of the five streams flowing into Mono Lake. Deprived of its freshwater sources, the lake volume dropped by half, exposing nesting colonies of gulls to predation and again doubling the lakes salinity. The entire eco-system began to collapse. In response David Gaines formed the Mono Lake Committee, a citizens group that was formed to reverse this trend and save the lake. In 1994 the California Supreme Court mandated that the lake should rise to a level of 6,392 feet, which will partially restore the ecosystem and migratory bird habitat.

This image shows South Tufa beneath moonlight.
Copyright
Russ Taylor
Image Size
4256x2828 / 10.8MB
Contained in galleries
Eastern Sierra
Tufa is a type of limestone that is formed when calcium-rich spring water mixes with the carbonate-rich Mono Lake water and precipitates around the spring. The towers grow underneath the waters surface. These towers were exposed when the city of Los Angeles diverted four of the five streams flowing into Mono Lake.  Deprived of its freshwater sources, the lake volume dropped by half, exposing nesting colonies of gulls to predation and again doubling the lakes salinity. The entire eco-system began to collapse. In response David Gaines formed the Mono Lake Committee, a citizens group that was formed to reverse this trend and save the lake. In 1994 the California Supreme Court mandated that the lake should rise to a level of 6,392 feet, which will partially restore the ecosystem and migratory bird habitat.<br />
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This image shows South Tufa beneath moonlight.