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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 stream of water flows over river rocks along the Snoqualmie River near Fall City, Washington.
    Snoqualmie-River_Rocks_Fall-City_292...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 the sky above Haystack Rock, a prominent sea stack located off the coast of Cape Kiwanda near Pacific City, Oregon.
    HaystackRockKiwandaSunset.jpg
  • The setting sun shines through the arch of Haystack Rock, located off Cape Kiwanda on the Oregon Coast near Pacific City, Oregon.
    HaystackKiwandaSunburst.jpg
  • A small rock rests next to a large crack in the ice on Rattlesnake Lake, located in King County, Washington, near the city of North Bend.
    Rattlesnake-Lake_Ice_Crack_Rock_8555.jpg
  • Pacific Ocean waves created an arch in the sandstone cliffs of Cape Kiwanda, near Pacific City, Oregon. The crashing waves are blurred by a 15-second exposure.
    CapeKiwandaArch.jpg
  • Several tufa columns are turned golden by the rising sun at Mono Lake, California. Tufa forms only underwater. When calcium-rich springs flow up through the lake bottom, the calcium bonds to the carbonates in the lake water, forming calcium carbonate, a type of limestone. The solid material builds on itself, gradually forming a tufa tower. The tufa towers form only underwater; they were exposed when the lake was drained to provide drinking water for cities. After environmental groups took legal action, less water is being diverted for cities and the lake is slowly refilling.
    CA_MonoLake_Tufas_Golden_9336.jpg
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