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  • The earth's shadow and the crescent moon are visible over the large silica dome and the fire canyon, located in the Valley of Fire, Nevada.
    VOF_ValleyOfFire_SilicaDomeMoon_9419.jpg
  • The earth's shadow and the crescent moon are visible over the large silica dome and the fire canyon, located in the Valley of Fire, Nevada.
    VOF_ValleyOfFire_SilicaDomeMoon_9420.jpg
  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • A close-up of a a cross-section of petrified wood reveals colors in abstract patterns in the Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_A...jpg
  • A cross-section of petrified wood displays a wide spectrum of colors in the Rainbow Forest of Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_D...jpg
  • A thick layer of minerals, especially silica, lines the edge of the Blue Lagoon (Bláa lónið), a geothermal spa in Iceland. The warm water is rich in silica, sulfur and other minerals, giving the water its color and milky texture. The water is heated by geothermal process and used to produce electricity before it is used in the Blue Lagoon, a popular outdoor spa.
    Iceland_BlueLagoon_1292.jpg
  • Blue-green water flows in channels carved into volcanic rock just outside the Blue Lagoon (Bláa lónið) in Iceland. The warm water is rich in silica, sulfur and other minerals, giving the water its color and milky texture. The water is heated by geothermal process and used to produce electricity before it is used in the Blue Lagoon, a popular outdoor spa.
    Iceland_BlueLagoon_5765.jpg
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