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  • Bighorn Lake and Bighorn Canyon, part of the Bighorn Canyon National Recreation Area, are visible in this aerial view captured southwest of Yellowtail, Montana. Bighorn Lake is a reservoir formed by Yellowtail Dam, which was finished in 1965. When the reservoir is full, the lake extends 72 miles (115 kilometers) — the entire length of Bighorn Canyon — into Wyoming.
    Montana_Bighorn-Lake_Aerial_3759.jpg
  • A red fox (Vulpes vulpes) pauses to lick its lips as it climbs a snow-covered hillside in the Custer Gallatin National Forest near Cooke City, Montana.
    Fox-Red_Hunting_Winter_Gallatin-NF_7...jpg
  • The first light of day creates a dramatic light show near St. Mary's, on the east side of Glacier National Park in Montana. The fiery cloud dwarfs the trees below.
    GlacierNP_Big-Sky-Sunrise_St-Marys_0...jpg
  • An autumn sunrise reddens the sky over the Missouri River at Coal Banks Landing in the Upper Missouri River Breaks National Monument in Montana.
    MissouriRiver_Coal-Banks_Fiery-Sunri...jpg
  • A cluster of icicles forms over a creek in the Cinnabar Basin in the Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Icicle-Patterns_85...jpg
  • A red fox (Vulpes vulpes) walks through snow to hunt in the Custer Gallatin National Forest near Cooke City, Montana.
    Fox-Red_Hunting_Winter_Gallatin-NF_7...jpg
  • A red fox (Vulpes vulpes) crouches low in the snow to hunt birds in the Custer Gallatin National Forest near Cooke City, Montana.
    Fox-Red_Hunting_Winter_Gallatin-NF_7...jpg
  • In winter, Cinnabar Creek is mostly covered in snow and ice as it flows in the valley of the Cinnabar Basin in the Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Cinnabar-Creek_Fro...jpg
  • In winter, Cinnabar Creek is mostly covered in snow and ice as it flows in the valley of the Cinnabar Basin in teh Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Cinnabar-Creek_Fro...jpg
  • A coyote (Canis latrans) walks among the golden grasses in a snow-covered field in search of food in Yellowstone National Park, Montana.
    Coyote_Snowy-Field_Yellowstone_8084.jpg
  • A pronghorn (Antilocapra americana) walks on a snow-dusted hill in Yellowstone National Park, Montana. They are often mistakenly referred to as antelope, although they are more closely related to giraffes than to Old World antelope.
    Pronghorn_Winter_Yellowstone_3328.jpg
  • An autumn sunrise reddens the sky over the Missouri River at Coal Banks Landing in the Upper Missouri River Breaks National Monument in Montana.
    MissouriRiver_Coal-Banks_Fiery-Sunri...jpg
  • A family of mountain goats (Oreamnos americanus) climbs the steep rugged wall known as Goat Lick in Glacier National Park, Montana. The mountain goats travel for miles to lick the mineral-laden cliffs during the spring and early summer. The cliffs are full of calcium, potassium and magnesium and smaller amounts of sodium and phosphorous. Scientists believe the goats may lick the cliffs to replace minerals they lose from their bones over the long winter. The minerals may also serve as a digestive aid. It's also possible the goats have simply developed a taste for salt.
    Goats_Mountain_Goat-Lick_Glacier_011...jpg
  • Snags rise above the frozen surface of Earthquake Lake in the Gallatin National Forest in Montana. The lake, located west of Yellowstone, was formed in 1959 after a magnitude 7.3 earthquake triggered an 80-million ton landslide, damming the Madison River. The snags here are trees that perished when their roots were flooded.
    MT_Earthquake-Lake_Snags_Winter_2805.jpg
  • Water pours over the face of a moose (Alces alces) after it lifts while feeding on vegetation in Fishercap Lake in the Many Glacier region of Glacier National Park, Montana.
    Moose_FishercapLake_GlacierNP_0352.jpg
  • A red fox (Vulpes vulpes) crouches in the snow behind an old tree trunk to hunt birds in the Custer Gallatin National Forest near Cooke City, Montana.
    Fox-Red_Hunting_Winter_Gallatin-NF_7...jpg
  • A bull elk stands on a hill next to the Roosevelt Arch, which marked the first major entrance into Yellowstone National Park. The arch, located in Gardiner, Montana, is inscribed with the words, "For the benefit and enjoyment of the people," a quote from the Organic Act of 1872, which created Yellowstone, the first national park. The arch was named for President Theodore Roosevelt who was visiting the park during the construction of the arch; he asked to place its cornerstone.
    Yellowstone_Roosevelt-Arch_Elk_5852.jpg
  • The sunrise colors the storm clouds passing over the mountains along Lake McDonald in Glacier National Park, Montana. Lake McDonald is the largest lake in Glacier National Park, approximately 10 miles (16 km) long, and over a mile (1.6 km) wide. Filling a valley that was carved by glaciers, the lake is 472 feet (130 m) deep.
    GlacierNP_LakeMcDonaldSunrise_1047.jpg
  • A family of mountain goats (Oreamnos americanus) climbs the steep rugged wall known as Goat Lick in Glacier National Park, Montana. The mountain goats travel for miles to lick the mineral-laden cliffs during the spring and early summer. The cliffs are full of calcium, potassium and magnesium and smaller amounts of sodium and phosphorous. Scientists believe the goats may lick the cliffs to replace minerals they lose from their bones over the long winter. The minerals may also serve as a digestive aid. It's also possible the goats have simply developed a taste for salt.
    Goats_Mountain_Goat-Lick_Glacier_013...jpg
  • Admist light snow, a red fox (Vulpes vulpes) scans the landscape in search of prey in the Custer Gallatin National Forest near Cooke City, Montana.
    Fox-Red_Winter_Gallatin-NF_7716.jpg
  • Early autumn snow dusts the landscape surrounding Warm Creek in Yellowstone National Park, Montana.
    Yellowstone_Warm-Creek_Early-Snow_57...jpg
  • A bright double rainbow connects the mountains on both sides of Logan Pass, located in Glacier National Park, Montana. The rainbow formed as a heavy afternoon thunderstorm moved along the Going-To-The-Sun Road, which passes through the valley at the center of this image.
    Glacier_LoganPassRainbow_0081.jpg
  • The sunrise colors the storm clouds passing over the mountains along Lake McDonald in Glacier National Park, Montana. Lake McDonald is the largest lake in Glacier National Park, approximately 10 miles (16 km) long, and over a mile (1.6 km) wide. Filling a valley that was carved by glaciers, the lake is 472 feet (130 m) deep.
    GlacierNP_LakeMcDonaldSunrise_F03-52...jpg
  • The sunrise colors the storm clouds passing over the mountains along Lake McDonald in Glacier National Park, Montana. Lake McDonald is the largest lake in Glacier National Park, approximately 10 miles (16 km) long, and over a mile (1.6 km) wide. Filling a valley that was carved by glaciers, the lake is 472 feet (130 m) deep.
    Glacier_LakeMcDonald_StormySunrise_1...jpg
  • A grizzly bear (Ursus arctos) feeds on berries in a meadow on Chief Mountain, located in Glacier National Park, Montana.
    GrizzlyBearMTClose.jpg
  • Two bighorn sheep (Ovis canadensis) feast on glacier lilies near Logan Pass in Glacier National Park, Montana. The yellow glacier lilies (Erythronium grandiflorum) are among the first wildflowers to bloom when the snow melts in mountain meadows.
    GlacierNP_BighornSheep_0096.jpg
  • Baring Creek flows through a very narrow gorge, called Sunrift Gorge, in Glacier National Park, Montana. The gorge has very smooth, straight sides because it eroded along vertical fractures in the rock known as joints. Sunrift Gorge began to form after large Pleistocene glaciers began to retreat from that area and with a maximum cut down rate of 0.003 inch per year, this gorge is the result of several millions of years of erosion.
    Glacier_SunriftGorge_0812.jpg
  • Running Eagle Falls in Glacier National Park, Montana, is also known as "Trick Falls" as the waterfall is much larger at the bottom than it is at the top. The waterfall is located in the Two Medicine area of the park and the "trick" is usually visible only in the summer when the water fall is lower.
    RunningEagleFalls_0163.jpg
  • Running Eagle Falls in Glacier National Park, Montana, is also known as "Trick Falls" as the waterfall is much larger at the bottom than it is at the top. The waterfall is located in the Two Medicine area of the park and the "trick" is usually visible only in the summer when the water fall is lower.
    RunningEagleFalls_0156.jpg
  • Several small waterfalls combine not far from the Continental Divide near Logan Pass in Glacier National Park, Montana. Several peaks, including Mount Gould and Mount Siyeh, are visible in the background.
    DividedCombination.jpg
  • The sunrise colors the storm clouds passing over the mountains along Lake McDonald in Glacier National Park, Montana. Lake McDonald is the largest lake in Glacier National Park, approximately 10 miles (16 km) long, and over a mile (1.6 km) wide. Filling a valley that was carved by glaciers, the lake is 472 feet (130 m) deep.
    GlacierNP_LakeMcDonaldSunrise_F03-52...jpg
  • A long exposure blurs the water of Avalanche Creek, which carved the narrow Avalanche Gorge in Glacier Naitonal Park, Montana.
    Glacier_AvalancheGorge_0722.jpg
  • A rainbow forms in the mist of St. Mary Fall, a 50-foot waterfall located on the St. Mary River in Glacier National Park, Montana.
    Glacier_StMaryFall_0717.jpg
  • The full moon shines above St. Mary Lake, the second largest lake in Glacier National Park, Montana, about a half hour before sunrise. The glint of the full moon falls next to Wild Goose Island.
    StMaryLakeMoon.jpg
  • A red fox (Vulpes vulpes) walks along a dried creek bed near Swiftcurrent Creek in Glacier National Park, Montana.
    RedFox_Glacier.jpg
  • A moose (Alces alces) feeds on plant life in Fishercap Lake in Glacier National Park, Montana.
    moose-FishercapLake-0436.jpg
  • A moose (Alces alces) shakes to dry off as it emerges from Fishercap Lake, located in Glacier National Park, Montana. The moose and the flying water droplets are blurred by a long exposure to capture their movement.
    moose-FishercapLake-0377.jpg
  • A grizzly bear (Ursus arctos) hunts for food in a meadow located in the Many Glacier section of Glazier National Park, Montana. Grizzly bears will eat both vegetation and animals. This one was feasting on blueberries growing in the meadow.
    GrizzlyBearMeadow.jpg
  • The full moon sets over St. Mary Lake as the first light of day reddens the skies over the Rocky Mountains and Glacier National Park, Montana. Wild Goose Island is visible to the right of the moon's glint near the center of the lake.
    GlacierStMaryLakeMoonTwilight.jpg
  • Two small creeks actually combine near the Continental Divide above Logan Pass in Glacier National Park, Montana.
    GlacierNPTwoCreeks.jpg
  • A rainbow forms in the mist of St. Mary Fall, a 50-foot waterfall located on the St. Mary River in Glacier National Park, Montana.
    Glacier_StMaryFall_0694.jpg
  • A bright double rainbow connects the mountains on both sides of Logan Pass, located in Glacier National Park, Montana. The rainbow formed as a heavy afternoon thunderstorm moved along the Going-To-The-Sun Road, which passes through the valley at the center of this image.
    Glacier_LoganPassRainbow_0074.jpg
  • The first snow of the winter caps the mountains surrounding St. Mary Lake as the cottonwood trees still show their golden fall color. St. Mary Lake is the second-largest lake in Glacier National Park, Montana.
    StMaryLakeFall.jpg
  • 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
  • A grizzly bear (Ursus arctos) feeds on berries in a meadow on Chief Mountain, located in Glacier National Park, Montana.
    GrizzlyBearFeeding.jpg
  • MissouriRiverJudith1.jpg
  • MissouriRiverJudith2.jpg
  • JudithRiverBend.jpg
  • Several ring-billed and herring gulls fly over Dry Falls in Grant County, Washington, which at one time was believed to be the largest waterfall that ever existed. Geologists believe that during the last ice age, ice dams resulted in giant glacial lakes in eastern Washington, Idaho and Montana. When those dams failed, as they did dozens of times, glacial lakes Columbia and Missoula rapidly drained, creating a cataclysmic flood. During the floods, what is now Dry Falls was a spectacular waterfall, 400 feet high (121 meters), 3.5 miles wide (5.63 kilometers). Water may have raced over its massive cliffs at 65 miles an hour (105 km/hour), a flow that's estimated to be ten times as powerful as all the world's current rivers combined. The cliffs shown here represent a small fraction of the ice age waterfall. Dry Falls Lake is pictured in the foreground; Green Lake is visible in the background.
    WA_DryFalls_Gulls_5825.jpg
  • A coyote looks out from the snow-covered forest south of Glacier National Park, Montana.
    CoyoteStMary.jpg
  • Palouse Falls plunges 180 feet (55 meters) into a giant natural amphitheater surrounded by towering columnar basalt walls near Washtucna, Washington. Palouse Falls was formed at the end of the last ice age when a mammoth ice dam in Montana regularly collapsed, releasing a torrent of water that carved this winding gorge.
    WA_PalouseFalls_Gorge_9389.jpg
  • Seen from the air, the rolling hills of Walla Walla, Washington look like giant, patch-work dunes. The rolling hills of Eastern Washington were formed by massive floods near the end of the last ice age as a ice dam holding back billions of gallons of water over present-day Missoula, Montana would regularly break, releasing a torrent of water that scoured and shaped the landscape.
    WallaWallaDunesAerial.jpg
  • Dry Falls, located in Grant County, Washington, at one time was believed to be the largest waterfall that ever existed. Geologists believe that during the last ice age, ice dams resulted in giant glacial lakes in eastern Washington, Idaho and Montana. When those dams failed, as they did dozens of times, glacial lakes Columbia and Missoula rapidly drained, creating a cataclysmic flood. During the floods, what is now Dry Falls was a spectacular waterfall, 400 feet high (121 meters), 3.5 miles wide (5.63 kilometers). Water may have raced over its massive cliffs at 65 miles an hour (105 km/hour), a flow that's estimated to be ten times as powerful as all the world's current rivers combined. The cliffs shown here represent a small fraction of the ice age waterfall. Dry Falls Lake is pictured in the foreground; Green Lake is visible in the background.
    WA_DryFalls_DryFallsLake_5898.jpg
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