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  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • A bison (Bison bison) warms up by standing in the steam rising from the Emerald Pool in the Black Sand Basin of Yellowstone National Park, Wyoming.
    Bison_Steam_Emerald-Pool_Yellowstone...jpg
  • Tangled Creek in Yellowstone National Park, Wyoming, curves through a patch of dead lodgepole pine trees that have a silica crust at their base, resembling bobby socks. The trees are in the Black Sand Basin of Yellowstone, a geothermal area. When the hot spring runoff shifted, the trees absorbed the silica-rich water.
    Yellowstone_Tangled-Creek_Bobby-Sock...jpg
  • A row of trees at the edge of Iron Spring Creek are encased in ice in the Black Sand Basin of Yellowstone National Park, Wyoming. The Black Sand Basin is home to a number of geothermal features. During the winter, steam can rise from them and freeze to nearby trees.
    Yellowstone_Ice-Encased-Trees_Black-...jpg
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