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  • Close-up of a male Common Ostrich, Struthio camelus, on the shore of Lake Baringo, Kenya
    18091192.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140169-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140168-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140161-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140158-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140156-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140155-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140154-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140145-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140144-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140143-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140170-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140167-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140166-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140162-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140160-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140152-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140149-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140146-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140165-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140164-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140157-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140153-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140147-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140148-mono-lake.jpg
  • Dead trees surround Maubara Lake in the Liquica district of Timor-Leste (East Timor).
    10041718-east-timor.jpg
  • Moon over Scotts Lake, Sierra Nevada Mountains, California
    06230310.jpg
  • Moon over Scotts Lake, Sierra Nevada Mountains, California
    06230311.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040112.jpg
  • Dead trees surround Maubara Lake in the Liquica district of Timor-Leste (East Timor).
    10041722-east-timor.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040152.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040150.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040126.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040159.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040158.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040155.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040149.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040145.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040144.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040134.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040128.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040125.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040117.jpg
  • Saline Range reflected in Salt Lake. Saline Valley, Death Valley National Park, California
    11040116.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040114.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040111.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040110.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040109.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040101.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040157.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040156.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040147.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040146.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040143.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040142.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040131.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040123.jpg
  • Ruins of wooden structures once used in salt mining at Salt Lake in Saline Valley, Death Valley National Park, California
    11040121.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040119.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040118.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040106.jpg
  • Clouds over Salt Lake in Saline Valley, Death Valley National Park, California
    11040100.jpg
  • Clouds over Salt Lake in Saline Valley, Death Valley National Park, California
    11040099.jpg
  • Salt Lake in Saline Valley, Death Valley National Park, California
    11040096.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140179-mono-lake.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140174-mono-lake.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140176-mono-lake.jpg
  • A Grant's Zebra, Equus quagga boehmi, watches as a tourist takes a photo on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091191.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past a tourist and two local guides on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091190.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091175.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past a group of Greater Flamingoes, Phoenicopterus ruber, on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091040.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060100.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past tourists on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091188.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091184.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091181.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091176.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091172.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091171.jpg
  • A group of White-faced Ibis, Plegadis chihi, stands in shallow water at the shore of Patagonia Lake in Patagonia Lake State Park, Arizona
    19040229pan.jpg
  • A Neotropic Cormorant, Phalacrocorax brasilianus, stands on the shore of Patagonia Lake in Patagonia Lake State Park, Arizona
    19040201.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060127.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060099.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060098.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060097.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060082.jpg
  • A pair of Clark's Grebes, Aechmophorus clarkii, performs a mating dance on Upper Klamath Lake, OregonUpper Klamath Lake, Oregon
    18060079.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past a tourist and two local guides on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091189.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past tourists on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091187.jpg
  • A Grant's Zebra, Equus quagga boehmi, walks past a group of photographers on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091186.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091185.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091183.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091182.jpg
  • Grant's Zebra, Equus quagga boehmi, runs through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091180.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091179.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091178.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091177.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091174.jpg
  • Grant's Zebra, Equus quagga boehmi, walks through shallow water at the edge of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091173.jpg
  • Grant's Zebra, Equus quagga boehmi, walks past a group of egrets and a Greater Flamingo, Phoenicopterus ruber, on the shore of Lake Nakuru in Lake Nakuru National Park, Kenya
    18091039.jpg
  • Grant's Zebra, Equus quagga boehmi, near the shore of Lake Nakuru in Lake Nakuru National Park, Kenya. Behind it are three Greater Flamingoes, Phoenicopterus ruber, and a Saddle-billed Stork, Ephippiorhynchus senegalensis.
    18091036.jpg
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