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  • A fumerole shoots steam high into the air at Hverir, an especially active geothermal area in northern Iceland.
    hverir-fumerole-backlit.jpg
  • Steam from vents, or fumaroles, in the Norris Basin of Yellowstone National Park, Wyoming, rises at sunrise.
    Yellowstone_Norris-Basin_Sunrise_174...jpg
  • Steam from vents, or fumaroles, in the Norris Basin of Yellowstone National Park, Wyoming, rises at sunrise, partially framing the Gallatin Mountains. In the foreground at left is Ledge Geyser, which once was the second largest geyser in the area, capable of shooting water 125 feet (38 meters) into the air. It has been largely inactive since 1995.
    Yellowstone_NorrisBasin_Fumaroles_17...jpg
  • These tall, narrow pillars known as The Pinnacles were formed during the cataclysmic eruption of Mount Mazama, which formed Crater Lake, Oregon. Volcanic gasses rose through layers of dacite pumice and andesite scoria in vents known as fumaroles. With temperatures of 750 degrees Fahrenheit (400 Celsius), the hot gasses welded the sides of the fumaroles. After erosion carried away the rest of the pumice and scoria, these hardened fossil fumaroles were all that remained.
    CraterLake_Pinnacles_9858.jpg
  • Several fumeroles shoot steam high into the sky at sunrise at Hverir, an especially active geothermal field in northern Iceland.
    hverir-fumeroles.jpg
  • A large kiawe (Prosopis pallida) tree frames of the southwestern coast of the Hawaiian island of Maui near the town of Makena. The first kiawe tree was introduced to Hawaii in 1828 and is now one of the most common trees in the dry lowlands of the Hawaiian islands. The prominent hill visible just to the right of the center of this image if Pu`u Ola`i, a 320-foot (98-meter) cinder cone formed when molten lava erupted from a volcanic vent and fell back to earth forming a nearly perfect cone. Pu`u Ola`i is also known as Earthquake Hill, Red Hill, and Round Mountain.
    Maui_Makena_Kiawe_PuuOlai_6384.jpg
  • A pseudocrater is rendered in silhouette against a volanic cone at sunset in Mývatn in northern Iceland. Mývatn is a lake that was formed approximately 2,300 years ago during a volanic period. The shorter hill is a pseudocrater, also known as a rootless vent. While it resembles a volcanic cinder cone, it formed through a different process. As basaltic lava flowed over soggy lake sediments, it flash heated the moisture into vapor, causing it to blast through the lava. Mývatn means lake with midge flies; the lake is infested with them during the summer months.
    Iceland_Myvatn_Pseudocrater-Silhouet...jpg
  • A boiling mudpot erupts at Sulphur Works in Lassen Volcanic National Park, California. Water from melting snow seeps into the ground above this mudpot, soaks through the soil and works down through cracks and fissures in the rock. Eventually, it touches hot rock and gasses in what used to be the main vent of Brokeoff Volcano, becomes superheated and returns to the surface as hot water or steam.
    Lassen_SulphurWorks_BoilingMudpot_58...jpg
  • A large kiawe (Prosopis pallida) tree frames of the southwestern coast of the Hawaiian island of Maui near the town of Makena. The first kiawe tree was introduced to Hawaii in 1828 and is now one of the most common trees in the dry lowlands of the Hawaiian islands. The prominent hill visible just to the right of the center of this image if Pu`u Ola`i, a 320-foot (98-meter) cinder cone formed when molten lava erupted from a volcanic vent and fell back to earth forming a nearly perfect cone. Pu`u Ola`i is also known as Earthquake Hill, Red Hill, and Round Mountain.
    Maui_Makena_Kiawe_PuuOlai_6412.jpg
  • A pseudocrater is rendered in silhouette against a volanic cone at sunset in Mývatn in northern Iceland. Mývatn is a lake that was formed approximately 2,300 years ago during a volanic period. The shorter hill is a pseudocrater, also known as a rootless vent. While it resembles a volcanic cinder cone, it formed through a different process. As basaltic lava flowed over soggy lake sediments, it flash heated the moisture into vapor, causing it to blast through the lava. Mývatn means lake with midge flies; the lake is infested with them during the summer months.
    Iceland_Myvatn_Pseudocrater-Silhouet...jpg
  • A long exposure shows the action of a boiling mudpot at Sulphur Works in Lassen Volcanic National Park, California. Water from melting snow seeps into the ground above this mudpot, soaks through the soil and works down through cracks and fissures in the rock. Eventually, it touches hot rock and gasses in what used to be the main vent of Brokeoff Volcano, becomes superheated and returns to the surface as hot water or steam.
    Lassen_SulphurWorks_BoilingMudpot_37...jpg
  • Molten lava flows from an opening at the end of a lava tube from the Pu'u O'o Kila vent in Volcanoes National Park on Hawaii.
    LavaFlow-8663.jpg
  • A bright lava flow illuminates full-size trees as it flows past them at night at Volcanoes National Park, Hawaii. The hot lava flows from the Pu'u O'o vent, which has erupted continuously since 1983.
    LavaFlow.jpg
  • Bright molten lava flows into the Pacific Ocean at twilight at Volcanoes National Park, Hawaii. The hot lava vaporizes the crashing waves, which reflect the lava's glow. The lava arrived at the ocean through an underground lava tube connected to the Pu'u O'o vent.
    LavaPacificOcean.jpg
  • The northern lights, or aurora borealis, shine over and are reflect in Lake Mývatn  in northern Iceland. The lake, formed during a lava eruption 2,300 years ago, contains numerous lava pillars and rootless vents, called pseudocraters. Mývatn is Icelandic for "midge lake," and denotes the tremendous number of midge flies found in the area. The aurora borealis, frequently visible during the winter months in Iceland, is caused by charged particles from the sun crashing into the Earth's atmosphere.
    Iceland_Myvatn_NorthernLights_2983.jpg
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