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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.<br />
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This image shows South Tufa beneath moonlight.
    Tufa and Casseopia
  • Last light of the day catches the clouds above South Tufa, Mono Lake
    Evening Light, South Tufa
  • 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.  In this photo tufa towers stand beneath Cassiopeia and the starry sky.
    South Tufa Beneath the Stars
  • Morning lights up rabbit brush and sage along the shores of Mono Lake as surreal tufa formations stand in the background
    Morning, South Tufa
  • Exposed tufa formations which used to lie at the bottom of Mono Lake give a surreal quality to the landscape.
    South Tufa
  • The June Full Moon rises over South Tufa at Mono Lake.
    Moon Rise over South Tufa, Mono Lake
  • A spring snowstorm places a layer of snow on tufa towers along Mono Lake's South Shore.
    South Tufa, Spring Snow
  • 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.
    South Tufa, Mono Lake
  • A storm rolls over Mono Lake
    Storm Over Mono
  • Evening light is reflected on the waters of Mono Lake from South Tufa
    Evening, South Tufa
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