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  • Runoff from a rainstorm flows past a water-quality warning sign and into a stormwater drain in Shoreline, Washington. The painted sign features a salmon icon and reads, "Dump no waste. Drains to Sound." Sound refers to Puget Sound, a large body of water in Washington state.
    Stormwater-Drain_Shoreline_7150.jpg
  • With the water of Puget Sound in the background, a sign next to a stormwater drain warns people not to dump toxic materials. The sign reads "No dumping! Drains to stream."
    Stormwater_Drain_Puget-Sound_5850.jpg
  • With the water of Puget Sound in the background, a sign next to a stormwater drain warns people not to dump toxic materials. The sign reads "No dumping! Drains to stream."
    Stormwater_Drain_Puget-Sound_5852.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
  • 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
  • The steaming runoff from the Terrace Springs zigzags across a meadow in Yellowstone National Park, Wyoming.
    Yellowstone_SteamingCreek_1527.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 vibrant rainbow forms during a late-afternoon rainstorm over Waimea Canyon on the Hawaiian island of Kauai. The canyon is 10 miles long and more than 3,500 feet deep. It was carved by runoff from Mount Waialeale, which gets more rain than any other spot on Earth.
    kauai-waimea-rainbow-wide.jpg
  • A close-up of the Painted Hills in John Day National Monument, Oregon reveals their popcorn-like texture. This texture is the result of erosion. The cracks result from the drying of the soil after heavy rain; the deeper channels are caused by the run-off of heavy rain.
    OR_PaintedHills_Texture_3125.jpg
  • The Old Faithful geyser erupts in Yellowstone National Park, Wyoming. When Old Faithful erupts, it can launch as much as 8,400 gallons (32,000 liters) of boiling water as high as 185 feet (56 meters), although the average eruption height is 145 feet (44 meters). The time between eruptions is growing longer on average, possibly because earthquakes have affected underground water levels. The current interval is either 65 or 91 minutes depending on attributes of the prior eruption.
    Old-Faithful_Eruption_Runoff_Yellows...jpg
  • Mineral-rich water from Konungshver, the King's Hot Spring, leaves colorful deposits as it flows from the geothermal spring in Iceland. Konungshver is located in southern Iceland near Geysir.
    Iceland_Konungshver_Runoff_2005.jpg
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