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  • A layered sandstone wall appears to have been twisted and folded by many thousands of years of geological forces in Harris Wash in Grand Staircase-Escalante National Monument, Utah.
    Grand-Staircase-Escalante_Harris-Was...jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4278.jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4282.jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4264.jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4276.jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4280.jpg
  • The top layer of sediment peels away at the base of Harris Wash near Escalante, Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_Peeling_4267.jpg
  • Water stands in Zebra Slot, a narrow slot canyon located in the Harris Wash in the Grand Staircase Escalante, Utah. The slot canyon was carved by the tremendous force from flash floods.
    Utah_ZebraSlot_4210.jpg
  • A small sandstone window frames a view of a narrow slot canyon in the Coyote Wash area of Grand Staircase National Monument in Utah. Flash floods carved narrow canyons in the sandstone.
    Grand-Staircase-Escalante_Coyote-Gul...jpg
  • A small sandstone window frames a view of a narrow slot canyon in the Coyote Wash area of Grand Staircase National Monument in Utah. Flash floods carved narrow canyons in the sandstone.
    Grand-Staircase-Escalante_Coyote-Gul...jpg
  • A hoary marmot (Marmota caligata) washes its face in Revelstoke National Park, British Columbia, Canada.
    MarmotWashRevelstoke.jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase-Escalante National Monument in Utah.
    Grand-Staircase-Escalante_Wall-Curve...jpg
  • A slot canyon makes a sharp curve in Coyote Gulch, located in the Grand Staircase-Escalante National Monument in Utah. The narrow sandstone canyon was carved by flash floods.
    Grand-Staircase-Escalante_Coyote-Gul...jpg
  • A vibrant shaft of light shines on the floor of a particularly narrow section of Upper Antelope Canyon on Navajo tribal land in Page, Arizona. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks." The slot canyon is formed primarily by erosion during flash floods; torrents of water race through the canyon and sculpt the sandstone.
    Antelope-Canyon_Beam_S2574-02.jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase-Escalante National Monument in Utah.
    Grand-Staircase-Escalante_Wall-Curve...jpg
  • A vibrant shaft of light shines on the floor of a particularly narrow section of Upper Antelope Canyon on Navajo tribal land in Page, Arizona. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks." The slot canyon is formed primarily by erosion during flash floods; torrents of water race through the canyon and sculpt the sandstone.
    Antelope-Canyon-Beam_S02-01-04.jpg
  • The standstone in a wash in the Valley of Fire State Park, Nevada shows colorful streaked patterns. This wash is comprised of several different layers of sandstone, which have been exposed through erosion.
    vof-color-wash.jpg
  • A pied-billed grebe (Podilymbus podiceps), the most widespread of the North American grebes, swims among the lily pads in the wetlands of the Washington Park Arboretum in Seattle, Wash. The pied-billed grebe's bill is circled by a broad black band during the summer months.
    Grebe_PiedBilled_LilyPads_2234.jpg
  • A greater roadrunner (Geococcyx californianus) races into a wash in the Sonoran Desert near Chandler, Arizona. Roadrunners, which are found throughout Mexico, Central America and the Southwestern United States, can run at speeds of up to 20 miles per hour (32 km/h).
    Roadrunner_Greater_Motion_Chandler_7...jpg
  • In the low-angle light of sunset, a Heermann's gull (Larus heermanni) waits on Venice Beach, California, for a Pacific Ocean wave to wash food ashore.
    Gull_Heermanns_Shadow_Venice-Beach_0...jpg
  • Layers of driftwood peel away in this detail of a log that washed ashore at Marina Beach Park, Edmonds, Washington.
    Driftwood_Layers_Edmonds_0353.jpg
  • A cross-section of petrified wood displays a wide spectrum of colors in the Rainbow Forest of Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_D...jpg
  • Pacific Ocean waves crash around driftwood that has washed ashore on Second Beach in Olympic National Park, Washington, as the clouds above are colored by the rising sun.
    OlympicNP_Second-Beach_Driftwood_Sun...jpg
  • Pacific Ocean waves crash around driftwood that has washed ashore on Second Beach in Olympic National Park, Washington, as the clouds above are colored by the rising sun.
    OlympicNP_Second-Beach_Driftwood_Sun...jpg
  • Pacific Ocean waves crash around driftwood that has washed ashore on Second Beach in Olympic National Park, Washington, as the clouds above are colored by the rising sun.
    OlympicNP_Second-Beach_Driftwood_Sun...jpg
  • A close-up of a a cross-section of petrified wood reveals colors in abstract patterns in the Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_A...jpg
  • Millions of microscopic organisms called dinoflagellates briefly emit a blue light when they are disturbed in the calm waters of Mosquito Bay on the island of Vieques, Puerto Rico. Mosquito Bay — also known as Puerto Mosquito, Caño Hondo and Bahía Bioluminiscente — is the brightest bioluminescent bay in the world with 2.4 million dinoflagellates per gallon of water at the time of this image. The dinoflagellates in Mosquito Bay are Pyrodinium bahamense and are a type of plankton, a subgroup of algae, that are found in Atlantic seawater warmer than 68 °F (20 °C). Mosquito Bay has a number of features that allow these dinoflagellates to exist in record concentrations. First, the bay has a very narrow opening to the Caribbean Sea, so when they are washed into the bay, they tend to get stuck. Mosquito Bay is also lined with mangrove trees, which provide abundant food for the dinoflagellates as they decompose.
    Puerto-Rico_Vieques_Mosquito-Bay_Bio...jpg
  • Green and yellow lichen grows on the peeling bark of driftwood that has washed ashore in Faye Bainbridge Park on Bainbridge Island, Washington state.
    Driftwood_Lichen_Bainbridge-Island_0...jpg
  • Atlantic Ocean waves crash into icebergs that have washed ashore at Breiðamerkursandur, a beach in southeast Iceland.
    Iceland_Icebergs_Beach_3889.jpg
  • A juvenile bald eagle (Haliaeetus leucocephalus) rests on driftwood that washed up on the beach of the Protection Island National Wildlife Refuge in Jefferson County, Washington. Protection Island, located at the mouth of Discovery Bay in the Strait of Juan de Fuca, is a 364-acre island mainly covered with grass and low brush. The island, which also has high sandy bluffs, serves as a nesting ground for 72 percent of the seabirds that nest in the Puget Sound area. Bald eagles prey on those seabirds and their young.
    BaldEagle_Juvenile_Driftwood_Protect...jpg
  • Water from the Greenland Sea, considered part of the Arctic Ocean, washes into Öxarfjörður, Iceland, exposing part of a black sand beach that was covered with snow.
    Iceland_Snow_BlackSandBeach_Öxarfjör...jpg
  • A Caspian tern (Hydroprogne caspia) dives for fish in Possession Sound near Everett, Washington.
    Tern-Caspian_Diving_Everett_0454.jpg
  • Three adult bald eagles (Haliaeetus leucocephalus) rest on logs that have washed up along the Nooksack River near Deming, Washington. Hundreds of bald eagles winter in the area to feast on spawned-out salmon.
    Bald-Eagles_Log_Three_Nooksack-River...jpg
  • A juvenile bald eagle (Haliaeetus leucocephalus) rests on driftwood that washed up on the beach of the Protection Island National Wildlife Refuge in Jefferson County, Washington. Protection Island, located at the mouth of Discovery Bay in the Strait of Juan de Fuca, is a 364-acre island mainly covered with grass and low brush. The island, which also has high sandy bluffs, serves as a nesting ground for 72 percent of the seabirds that nest in the Puget Sound area. Bald eagles prey on those seabirds and their young.
    BaldEagle_Juvenile_Driftwood_Protect...jpg
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