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  • A bright fogbow frames several tress growing on a bluff high above the Missouri River between Poplar and Brockton, Montana. Fogbows are formed much like rainbows, except the bands of colors overlap, resulting in what appears to be a largely white band. (A faint red band is visible on the outer edge; blue, inside.) The full moon is also visible in the inner band, just above the golden tree.
    fogbow.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
  • The north Atlantic Ocean is visible in breaks between bands of cumulus clouds in this aerial view captured between Greenland and Iceland. The tops of the clouds are turned red by the rising sun.
    Clouds_Cumulus_Aerial_Iceland_1532.jpg
  • The north Atlantic Ocean is visible in a narrow break in a band of stratocumulus clouds in this aerial view captured between Greenland and Iceland.
    Clouds_Stratocumulus_Aerial_Iceland_...jpg
  • A fumerole shoots steam high into the air at Hverir, an especially active geothermal area in northern Iceland.
    hverir-fumerole-backlit.jpg
  • The sun sets through storm clouds developing over the Pacific Ocean in this view from Pacific Beach, Washington.
    StormClouds_Sun_PacificBeach_5640.jpg
  • Several fumeroles shoot steam high into the sky at sunrise at Hverir, an especially active geothermal field in northern Iceland.
    hverir-fumeroles.jpg
  • Ground frost, otherwise known as hoar frost, sticks to the grass on a cold morning in Bryce Canyon National Park, Utah. Ground frost typically forms on cold, clear nights when the ground temperature drops below freezing. When water vapor in the warmer air touches the frozen ground, it freezes, forming ice in a process known as sublimation.
    GroundFrost_Grass_BryceNP_1240.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
  • Two layers of water vapor — cirrus clouds and the streaks of a fog bank — frame the flank of Sauk Mountain in Washington state. The mountain is located near the town of Concrete in Skagit County, just west of the crest of the North Cascade Range.
    WA_Sauk-Mountain_Cirrus_Fog-Streaks_...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
  • Steam fog, also known as sea smoke, rises from the Sammamish River near Woodinville, Washington, on a cold morning. Steam fog occurs when cold air — it was 22 degrees Fahrenheit at the time this image was captured — passes over warmer water. Moisture rises from the relatively warm river and turns to vapor inches above the surface when it hits the freezing-cold air.
    Sammamish-River_Steam-Fog_7997.jpg
  • One of the many steam eruptions of Mount St. Helens in the fall of 2004 sends a towering column of water vapor high into the air. The mountain is reflected in Silver Lake.
    StHelensEruption.jpg
  • A particularly heavy ground frost covers a rock in the Central Cascades of Washington state. Ground frost typically occurs on cold, clear nights when the ground temperature drops below freezing. When water vapor in the warmer air touches the frozen ground, it freezes, forming ice in a process known as sublimation.
    GroundFrost_IndexGalenaRd_2409.jpg
  • An oak leaf leaves an impression in the ice covering a small pond in Snohomish County, Washington. The leaf fell on the pond after it froze and protected the ice immediately beneath it from sublimation, a natural process where ice transitions into vapor without turning to liquid first. This is the same process that causes a snow on a field to vanish during a prolonged cold spell. Reflections of trees surrounding the pond are visible around the edges of the leaf impression.
    Leaf_Oak_Ice_Impression_9686.jpg
  • An oak leaf leaves an impression in the ice covering a small pond in Snohomish County, Washington. The leaf fell on the pond after it froze and protected the ice immediately beneath it from sublimation, a natural process where ice transitions into vapor without turning to liquid first. This is the same process that causes a snow on a field to vanish during a prolonged cold spell. Reflections of trees surrounding the pond are visible around the edges of the leaf impression.
    Leaf_Oak_Ice_Impression_9673.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
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