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  • Dramatic limestone curtains form the ceiling of the Ruakuri Cave, located in Waitomo, New Zealand. These limestone curtains are a type of stalactite. Water drips from above, disolving limestone. Where the water evaporates, the limestone is left behind. The limestone curtains are formed along a line where water drips from several places.
    NZ_RuakuriCaveCurtains_1508.jpg
  • Large limestone formations, known as tufa, rise from Mono Lake in eastern California. The tufa result from calcium-rich springs that flow up from the bottom of the lake. The calcium bonds to carbonates in the water, forming calcium carbonate, a type of limestone. The calcium carbonate builds on itself, gradually forming towering columns. Those columns grow only when under water; they stop growing when the lake level drops and they are exposed.
    CA_MonoLake_Sunrise_Silhouette_9259.jpg
  • An osprey (Pandion haliaetus) takes off with a scrap of food from a tufa in Mono Lake, California. Tufa are limestone columnns that form naturally due to a chemical reaction in the lake. They form underwater and were exposed when the lake level dropped.
    Osprey_MonoLake_Tufa_0867.jpg
  • Several tufa columns are turned golden by the rising sun at Mono Lake, California. Tufa forms only underwater. When calcium-rich springs flow up through the lake bottom, the calcium bonds to the carbonates in the lake water, forming calcium carbonate, a type of limestone. The solid material builds on itself, gradually forming a tufa tower. The tufa towers form only underwater; they were exposed when the lake was drained to provide drinking water for cities. After environmental groups took legal action, less water is being diverted for cities and the lake is slowly refilling.
    CA_MonoLake_Tufas_Golden_9336.jpg
  • The Pancake Rocks, located in Punakaiki on the West Coast of New Zealand, are layered columns of limestone, somewhat resembling stacks of pancakes. Geologists are not certain of their origin. New Zealand's Southern Alps are visible on the horizon.
    NZ_PancakeRocks_5038.jpg
  • Several thousand stalactites hang over and are reflected on Dream Lake, one of the wonders in the Luray Caverns in Virginia.
    VA_Luray-Caverns_Dream-Lake_9364c.jpg
  • Rabbitbrush (Chrysothamnus nauseosus var. consimilis) grows under a fiery sunrise at the edge of Mono Lake in Mono County, California. Mono Lake has no outlet, so salt accumulates and makes the water alkeline. Limestone columns called tufa towers are visible in the lake. Tufa towers form under water. They were exposed when Los Angeles diverted some of the fresh water that feeds the lake, causing the lake level to drop.
    Mono-Lake_Rabbitbrush_Sunrise_0748.jpg
  • The five-story cliff dwelling known as Montezuma Castle is visible up a sheer limestone cliff in Montezuma Castle National Monument near Camp Verde, Arizona. Montezuma Castle and other cliff dwellings in the area were built and used by the Sinagua people between approximately 1100 and 1425 AD. Montezuma Castle, which contains 45-60 rooms, is one of the best-preserved cliff dwellings in North America, likely due to its placement 90 feet (27 meters) up the cliff and the protection from the elements provided by the rock overhang.
    AZ_Montezuma-Castle_2489.jpg
  • The five-story cliff dwelling known as Montezuma Castle is visible up a sheer limestone cliff in Montezuma Castle National Monument near Camp Verde, Arizona. Montezuma Castle and other cliff dwellings in the area were built and used by the Sinagua people between approximately 1100 and 1425 AD. Montezuma Castle, which contains 45-60 rooms, is one of the best-preserved cliff dwellings in North America, likely due to its placement 90 feet (27 meters) up the cliff and the protection from the elements provided by the rock overhang.
    AZ_Montezuma-Castle_Framed_2485.jpg
  • A rainbow stretches across the sky above the Vermilion Cliffs near Page, Arizona. The Vermilion Cliffs, which rise as much as 3,000 feet (914 meters), are the second step in the five-step Grand Staircase of the Colorado Plateau, which stretches from northern Arizona to southern Utah.  The cliffs are made up of sedimentary rocks, primarily sandstone, siltstone, limestone, and shale, that have eroded over millions of years. The Vermilion Cliffs were designated as the Vermilion Cliffs National Monument in 2000.
    AZ_VermilionCliffs_Rainbow_8507.jpg
  • The late afternoon sun dips behind a cloud in this view from Ruffner Mountain, Birmingham, Alabama. The area was once home to iron ore mines and limestone quarries, but was set aside for nature conservation in 1977.
    AL_Ruffner-Mountain_Sunburst_8791.jpg
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