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  • The Snonomish River spilled well beyond its banks during a severe flood, engulfing these three trees near Snohomish, Washington.
    Snohomish-River_Flood_Three-Trunks_9...jpg
  • More than 16 times the typical flow of water gushes over Snoqulamie Falls in Washington state during a November 2006 flood.
    SnoqualmieFalls_Flood_3920.jpg
  • During a flood, North Creek flows around a tree that's partially submerged by the high water in Bothell, Washington
    NorthCreek_SubmergedTree_0128.jpg
  • During a flood, North Creek flows around a tree that's partially submerged by the high water in Bothell, Washington.
    NorthCreek_SubmergedTree_0134.jpg
  • Several small rocks lie at the base of a dry waterfall, which was carved by flash floods in the Coyote Gulch area of the Grand Staircase Escalante, Utah.
    CoyoteGulchDryFall.jpg
  • Seen from the air, the rolling hills of Walla Walla, Washington look like giant, patch-work dunes. The rolling hills of Eastern Washington were formed by massive floods near the end of the last ice age as a ice dam holding back billions of gallons of water over present-day Missoula, Montana would regularly break, releasing a torrent of water that scoured and shaped the landscape.
    WallaWallaDunesAerial.jpg
  • Several ring-billed and herring gulls fly over Dry Falls in Grant County, Washington, which at one time was believed to be the largest waterfall that ever existed. Geologists believe that during the last ice age, ice dams resulted in giant glacial lakes in eastern Washington, Idaho and Montana. When those dams failed, as they did dozens of times, glacial lakes Columbia and Missoula rapidly drained, creating a cataclysmic flood. During the floods, what is now Dry Falls was a spectacular waterfall, 400 feet high (121 meters), 3.5 miles wide (5.63 kilometers). Water may have raced over its massive cliffs at 65 miles an hour (105 km/hour), a flow that's estimated to be ten times as powerful as all the world's current rivers combined. The cliffs shown here represent a small fraction of the ice age waterfall. Dry Falls Lake is pictured in the foreground; Green Lake is visible in the background.
    WA_DryFalls_Gulls_5825.jpg
  • Five North American Beavers (Castor canadensis) rest on top of their lodge in North Creek, Bothell, Washington. Beavers, the largest rodent in North America, live in lodges that are designed to protect them from predators. The mud that holds the sticks together freezes like concrete, making the structure virtually impenetrable. During large winter floods, however, the beavers occasionally have to evacuate the lodge and rest on its roof until the flood waters recede.
    Beavers_Lodge_FiveOnTop_NorthCreek_8...jpg
  • Dry Falls, located in Grant County, Washington, at one time was believed to be the largest waterfall that ever existed. Geologists believe that during the last ice age, ice dams resulted in giant glacial lakes in eastern Washington, Idaho and Montana. When those dams failed, as they did dozens of times, glacial lakes Columbia and Missoula rapidly drained, creating a cataclysmic flood. During the floods, what is now Dry Falls was a spectacular waterfall, 400 feet high (121 meters), 3.5 miles wide (5.63 kilometers). Water may have raced over its massive cliffs at 65 miles an hour (105 km/hour), a flow that's estimated to be ten times as powerful as all the world's current rivers combined. The cliffs shown here represent a small fraction of the ice age waterfall. Dry Falls Lake is pictured in the foreground; Green Lake is visible in the background.
    WA_DryFalls_DryFallsLake_5898.jpg
  • The wind blows blades of dried grass, which carve a light groove into a sand dune in the Juniper Dunes Wilderness near Pasco, Washington. The Juniper Dunes Wilderness is named for the western juniper trees that grow there, the northernmost cluster of such trees. Located in Franklin County, Washington, Juniper Dunes is a protected wilderness area that comprises 7,140 acres (28.9 km²). Some dunes in the area measure more than 130 feet (40 meters) in height and 1,000 feet (305 meters) in width. The dunes formed in what was essentially a flood basin at the end of the last ice age.
    JuniperDunes_GrassBlownByWind_5289.jpg
  • Three prominent Washington state volcanoes are visible over the Cascade foothills in this aerial view taken from over North Bend, Washington. In the center, Mount Rainier, with an elevation of 14,411 feet (4,392 meters), is the tallest mountain in Washington and the highest volcano in the Cascade Range. At left, Mount Adams, at 12276 ft. (3742 m), is the second-tallest mountain in the state. At right is Mount St. Helens, a 8,365 feet (2,550 m) volcano that lost nearly 15 percent of its height in a 1980 eruption. The body of water in the lower-right is the Howard A. Hanson reservoir, used for flood control and to provide drinking water to Tacoma.
    Rainier_Adams_St-Helens_Aerial_1417.jpg
  • Some bark remains intact around the base of a dead tree that had been submerged for 100 years in Rattlesnake Lake near North Bend, Washington. The lake level dropped after a prolonged flood, exposing the stump and the preserved bark that's pulling away from it.
    Rattlesnake-Lake_Bark-Exposed-Peelin...jpg
  • The Juniper Dunes Wilderness, northeast of Pasco, Washington, is home to the largest sand dunes in Washington state. The dunes, some of which are as much as 100 feet high, are located in what was essentially a flood basin at the end of the last ice age.
    JuniperDunesSunburst.jpg
  • Some bark remains intact around the base of a dead tree that had been submerged for 100 years in Rattlesnake Lake near North Bend, Washington. The lake level dropped after a prolonged flood, exposing the stump and the preserved bark that's pulling away from it.
    Rattlesnake-Lake_Bark-Exposed-Peelin...jpg
  • Several tall mountains stand over the ancient lava flow Búrfells-hraun in northern Iceland. Geologists believe a large lava lake formed here and then collapsed, releasing a flood of lava. Pieces of the lava crust flowed as much as 10 km (6.2 miles) downstream.
    Iceland_Burfells-hraun_3957.jpg
  • Several tall mountains stand over the ancient lava flow Búrfells-hraun in northern Iceland. Geologists believe a large lava lake formed here and then collapsed, releasing a flood of lava. Pieces of the lava crust flowed as much as 10 km (6.2 miles) downstream.
    Iceland_Burfells-hraun_3941.jpg
  • Wind blows across a curved dune, creating streaks of sand in the Juniper Dunes Wilderness in Washington state. The Juniper Dunes Wilderness, northeast of Pasco, Washington, is home to the largest sand dunes in Washington state. The dunes, some of which are as much as 100 feet high, are located in what was essentially a flood basin at the end of the last ice age. The Juniper Dunes Wilderness, located in Franklin County, is a wilderness preserve that spans more than 7,000 acres.
    JuniperDunes_CurvedSummit_Windy_6122.jpg
  • A blade of grass grows from and casts its shadow on a rippled sand dune in the Juniper Dunes Wilderness near Pasco, Washington. The Juniper Dunes Wilderness is named for the western juniper trees that grow there, the northernmost cluster of such trees. Located in Franklin County, Washington, Juniper Dunes is a protected wilderness area that comprises 7,140 acres (28.9 km²). Some dunes in the area measure more than 130 feet (40 meters) in height and 1,000 feet (305 meters) in width. The dunes formed in what was essentially a flood basin at the end of the last ice age.
    JuniperDunes_GrassShadow_5980.jpg
  • A passage bends through a very narrow section of Upper Antelope Canyon on Navajo Nation land near Page, Arizona. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_6255.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
  • 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 narrow path winds through the tall undulating walls of Upper Antelope Canyon on Navajo Nation land in northern Arizona. Antelope Canyon is a slot canyon, a small sandstone canyon that is carved by violent flash floods. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_6243.jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_709...jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Textured-Walls_6218c.jpg
  • The curved walls of Rattlesnake Canyon join to form abstract patterns on Navajo Nation land near Page, Arizona. Rattlesnake Canyon is a slot canyon — a narrow sandstone canyon that's carved by flash floods.
    AZ_Rattlesnake-Canyon_Curved-Walls_6...jpg
  • Two North American Beavers (Castor canadensis) groom each other on the top of their lodge in North Creek, Bothell, Washington. Beavers are typically most active at night and spend the winter in the safety of their lodges. During significant floods, however, the beavers climb on top of their lodges, waiting for the waters to recede.
    Beavers_Lodge_Grooming_NorthCreek_90...jpg
  • A vibrant shaft of light illuminates a tumbleweed on the floor of Antelope Canyon in Page, Arizona. Antelope Canyon is a slot canyon that was carved by violent flash floods. Beams of light form only when the sun is nearly overhead, lighting up the blowing sand that fills the canyon, which is dozens of feet deep. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    AntelopeCanyon_Beam_Tumbleweed_0493.jpg
  • A heart shape appears among the curves of the ceiling of Upper Antelope Canyon on Navajo land near Page, Arizona. Violent flash floods sculpt the sandstone slot canyon, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Heart_7109.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
  • Sand falls from a ledge in Upper Antelope Canyon on Navajo Nation land near Page, Arizona. Antelope Canyon is a narrow sandstone canyon, known as a slot canyon. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Sand-Falls_7097.jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_622...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
  • The walls of a particularly narrow passage of Upper Antelope Canyon in Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon-Beam_S2574-01.jpg
  • A Florida tree snail (Liguus fasciatus) climbs a tree along the Gumbo Limbo Trail in the Everglades National Park, Florida. The trail winds through a tropical hardwood hammock, a dense forest that forms only in areas that are protected from fires and floods. This area is only three feet higher than the neighboring wetlands. There are 52 different color forms of the Florida tree snail found in south Florida.
    Everglades_Florida-Tree-Snail_3369.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
  • 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
  • Snags rise above the frozen surface of Earthquake Lake in the Gallatin National Forest in Montana. The lake, located west of Yellowstone, was formed in 1959 after a magnitude 7.3 earthquake triggered an 80-million ton landslide, damming the Madison River. The snags here are trees that perished when their roots were flooded.
    MT_Earthquake-Lake_Snags_Winter_2805.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
  • The walls of a particularly narrow passage of Upper Antelope Canyon in Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_Looki...jpg
  • Bright streaks fall down the curved walls of Upper Antelope Canyon in the Navajo Nation, Arizona. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Streaks_6235.jpg
  • The curved walls of Rattlesnake Canyon join to form abstract patterns on Navajo Nation land near Page, Arizona. Rattlesnake Canyon is a slot canyon — a narrow sandstone canyon that's carved by flash floods.
    AZ_Rattlesnake-Canyon_Curved-Walls_6...jpg
  • With just a narrow crack in the ceiling of Upper Antelope Canyon near Page, Arizona, little sunlight reaches the floor by mid-afternoon. Violent flash floods sculpt the sandstone, leaving undulating, layered walls that appear violet or purple in the very faint indirect afternoon light. The Navajo people call Antelope Canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks." The light in the canyon was so dim at the time that this image was captured that it required a more than one-minute exposure to reveal the detail of the canyon walls.
    Antelope-Canyon_Texture_S2571-05.jpg
  • A vibrant shaft of light shines like a spotlight on the floor of Antelope Canyon in Page, Arizona. Antelope Canyon is a slot canyon that was carved by violent flash floods. Beams of light form only when the sun is nearly overhead, lighting up the blowing sand that fills the canyon, which is dozens of feet deep. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon-Beam_S2574-09.jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase Escalante, Utah.
    CoyoteGulchWavyWalls.jpg
  • Three vibrant shafts of light appear in a narrow passage in Antelope Canyon, a slot canyon carved by violent flash floods in Page, Arizona. The beams form only when the sun is nearly overhead, lighting up the blowing sand that fills the canyon, which is dozens of feet deep. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    AntelopeCanyonBeams.jpg
  • Two North American Beavers (Castor canadensis) rest atop their flooded lodge in North Creek, Bothell, Washington. Beavers are typically most active at night and spend the winter in the safety of their lodges. During significant floods, however, the beavers climb on top of their lodges, waiting for the waters to recede.
    Beavers_Lodge_Resting_NorthCreek_898...jpg
  • A heart shape appears among the curves of the ceiling of Upper Antelope Canyon on Navajo land near Page, Arizona. Violent flash floods sculpt the sandstone slot canyon, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Heart_7110.jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_622...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
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