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  • Autumn color lines the base of a large granite rock formation in the City of Rocks National Reserve in Idaho as a heavy rainstorm passes.
    Idaho_CityOfRocks_Autumn-Rainstorm_0...jpg
  • A couple of trees grow between two large splatter cones resulting from the eruption of the north crater in Craters of the Moon National Monument, Idaho.
    CratersOfTheMoon_Splatter-Cones_Silh...jpg
  • An osprey (Pandion haliaetus) flies with a red kokanee salmon (Oncorhynchus nerka) that it caught in Hayden Lake, Idaho. Kokanee are genetically similar to sockeye salmon. The main difference is that kokanee spend their entire lives in freshwater, unlike salmon with spend most of their lives in the ocean and return to freshwater to spawn.
    Osprey_Kokanee_Hayden-Lake_2135.jpg
  • The tops of some golden grasses poke through deep snow covering rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3364.jpg
  • A pair of Canada geese (Branta canadensis) splash water as they land on Hayden Lake in Idaho.
    Geese-Canada_Hayden-Lake_1977.jpg
  • An osprey (Pandion haliaetus) flies with a red kokanee salmon (Oncorhynchus nerka) that it caught in Hayden Lake, Idaho. Kokanee are genetically similar to sockeye salmon. The main difference is that kokanee spend their entire lives in freshwater, unlike salmon with spend most of their lives in the ocean and return to freshwater to spawn.
    Osprey_Kokanee_Hayden-Lake_1853.jpg
  • Lichen grows on the walls near the entrance of Beauty Cave, a 300-foot (100-meter) long lava tube in the Craters of the Moon National Monument, Idaho.
    CratersOfTheMoon_Beauty-Cave_2519.jpg
  • An osprey (Pandion haliaetus) flies with a red kokanee salmon (Oncorhynchus nerka) that it caught in Hayden Lake, Idaho. Kokanee are genetically similar to sockeye salmon. The main difference is that kokanee spend their entire lives in freshwater, unlike salmon with spend most of their lives in the ocean and return to freshwater to spawn.
    Osprey_Kokanee_Hayden-Lake_1873.jpg
  • A few wispy clouds catch the golden light of sunset and are reflected on the still waters of a wetland that borders Shepherd Lake near Sagle, Idaho.
    ID_Sagle_Marsh-Susnet_0414.jpg
  • The summit of Dead Indian Ridge, located in Washington County Idaho, is in deep shadow as a band of altostratus clouds pass overhead in this view from near Huntington, Oregon.
    ID_Dead-Indian-Ridge_Shadow_3959.jpg
  • A bitterroot (Lewisia rediviva) grows among the lava rocks that make up a cider cone in the Craters of the Moon National Monument in Idaho.
    CratersOfTheMoon_Lava-Rock_Bitterroo...jpg
  • An osprey (Pandion haliaetus) flies with a red kokanee salmon (Oncorhynchus nerka) that it caught in Hayden Lake, Idaho. Kokanee are genetically similar to sockeye salmon. The main difference is that kokanee spend their entire lives in freshwater, unlike salmon with spend most of their lives in the ocean and return to freshwater to spawn.
    Osprey_Kokanee_Hayden-Lake_1956.jpg
  • A cluster of trees stands atop snow-covered rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3331.jpg
  • An osprey (Pandion haliaetus) flies with a red kokanee salmon (Oncorhynchus nerka) that it caught in Hayden Lake, Idaho. Kokanee are genetically similar to sockeye salmon. The main difference is that kokanee spend their entire lives in freshwater, unlike salmon with spend most of their lives in the ocean and return to freshwater to spawn.
    Osprey_Kokanee_Hayden-Lake_1877.jpg
  • A cluster of trees stands atop snow-covered rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3288.jpg
  • A gnarled, bleached tree frames one of the many cinder cones in the Craters of the Moon National Monument in Idaho.
    CratersOfTheMoon_Cinder-Cone-Framed_...jpg
  • Pahoehoe lava, characterized by its smooth, rope-like appearance, is one of three types of lava. Pahoehoe's ropy surface forms when a thin skin of cool lava is shoved into folds by hot, more-fluid lava just below the surface. This sample was found in Craters of the Moon National Monument, Idaho. Pahoehoe is pronounced Pa-hoy-hoy.
    CratersOfTheMoon_Pahoehoe_2534.jpg
  • This unusual "triple twist tree" growing out of a crack in a lava field at Craters of the Moon National Monument in Idaho helped scientists determine the age of the flow here. The tree has 1,350 rings, so scientists figure the flow here is about 2,000 years old. This flow is the youngest in Craters of the Moon National Monument.
    CratersOfTheMoon_Triple-Twist-Tree_2...jpg
  • A large granite arch frames a pinyon pine as well as several prominent City of Rocks features, including Elephant Rock (at left) and the Bread Loaves (at right). This arch is part of Window Rock in the City of Rocks National Reserve in southern Idaho.
    Idaho_CityOfRocks_Arch_Sunrise_0993.jpg
  • The setting sun colors wispy cirrus clouds that reflect in an unnamed lake in Sagle, Idaho.
    Idaho_Sagle_Lake_Sunset_0416.jpg
  • Colorful crustose lichens grow on lava rock at Craters of the Moon National Monument in Idaho. Lichens are a symbiosis of a fungus and a green alga and/or cyanobacterium. Crustose are very slow growing, typically growing 1 millimeter or less per year.
    CratersOfTheMoon_Lichen_2479.jpg
  • LeaningTreeCratersMoon.jpg
  • CratersMoonSplatterSunburst.jpg
  • UpperMesaFalls.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
  • Cave Falls, located in the southwest portion of Yellowstone National Park in Wyoming, may only be 20 feet tall, but it stretches 250 feet across the Falls River. Cave Falls, the widest waterfall in Yellowstone, is named for a 50-foot cave at its base. While Cave Falls is in Wyoming, it can only be accessed from a road in Idaho.
    Wyoming_CaveFalls_2366.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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