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  • A fractured tree hangs suspended in the air along Wapaloosie Mountain Trail, in Colville National Forest, Kettle Range, Washington, USA
    1406WA-025.jpg
  • View eastwards from Copper Butte, Marcus Trail, Colville National Forest, Kettle Range, Washington, USA
    1406WA-014.jpg
  • Lichen forms polygons on a rock atop Copper Butte, Marcus Trail, Colville National Forest, Kettle Range, Washington, USA
    1406WA-017.jpg
  • Wrangell Mountains, seen from Nabesna Road, in Wrangell-St. Elias National Park and Preserve, southeast Alaska, USA. Nabesna Road offers spectacular scenery in a seldom-seen, wild corner of Alaska, the headwaters of the Copper River. Here at Mile Post 16.6, Kettle Lake picnic site offers a great view of the Wrangell Mountains. A humorous sign here says "TOILET 1 MILE". The Wrangell Lavas built the Wrangell Mountains over the past 10 million years. Mount Wrangell (14,163 ft) is the largest andesite shield volcano in North America. The cinder cone of Mount Zanetti (13,009 ft) rose prominently 1000 feet above its northwest flank during the past 25,000 years. Wrangell reportedly erupted in 1784 and 1884–85. Occasional steam plumes rise from the park's only active volcano, and ash sometimes coats the summit snow. Flowing northward from it is the Copper Glacier, source of Copper River which flows northward, then westward along the end of the Wrangell Range, then southward to the Gulf of Alaska near Cordova, cutting through the coastal barrier of the Chugach Mountains, marking most of Park's western boundary. This image was stitched from multiple overlapping photos.
    1906AKH-2792-97-Pano-Edit.jpg
  • At Nabesna Road Mile Post 16.6, Kettle Lake picnic site offers a great view of the Wrangell Mountains. A humorous sign here says "TOILET 1 MILE". in Wrangell-St. Elias National Park and Preserve, southeast Alaska, USA. Nabesna Road offers spectacular scenery in a seldom-seen, wild corner of Alaska, the headwaters of the Copper River. The Wrangell Lavas built the Wrangell Mountains over the past 10 million years. Mount Wrangell (14,163 ft) is the largest andesite shield volcano in North America. The cinder cone of Mount Zanetti (13,009 ft) rose prominently 1000 feet above its northwest flank during the past 25,000 years. Wrangell reportedly erupted in 1784 and 1884–85. Occasional steam plumes rise from the park's only active volcano, and ash sometimes coats the summit snow. Flowing northward from it is the Copper Glacier, source of Copper River which flows northward, then westward along the end of the Wrangell Range, then southward to the Gulf of Alaska near Cordova, cutting through the coastal barrier of the Chugach Mountains, marking most of Park's western boundary.
    1906AKH-2800.jpg
  • Reflection Pond reflects the flanks of Denali in the Alaska Range. Reflection Pond is a kettle hole left where an ancient block of glacial ice melted. Denali National Park, Alaska, USA. At 20,310 feet elevation or 6191 m, the peak of Denali (previously known as Mount McKinley) is the highest mountain in North America. When measured from its base, it is earth's tallest (most prominent) mountain on land. Denali is a granitic pluton uplifted by tectonic pressure while erosion has simultaneously stripped away the softer surrounding sedimentary rock.
    1906AKH-2219.jpg
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