Submerged Tufa

Moods of Mono week 17

This would have to be one of my favorites from the summer.

Tufa is a type of limestone that is formed when calcium-rich spring water mixes with the carbonate-rich water of Mono Lake and precipitates around the spring. The towers grow underneath the water’s 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.

Submerged Tufa

In this photo tufa towers can be seen above and beneath the lakes surface. Those beneath the surface are growing once again as they are  exposed to the high carbonate water.

To view this and the previous 16 week’s images, visit the Eastern Sierra Gallery.

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