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  • The sun rises over the edge of a basalt cliff that lines the Potholes Canal near Soda Lake in the Columbia National Wildlife Refuge in Washington state.
    WA_Columbia-NWR_Basalt-Cliff_Sunrise...jpg
  • The first light of day illuminates the shrubs atop a basalt cliff that rises over a small pond in the Columbia National Wildlife Refuge in Adams County, Washington.
    WA_Columbia-NWR_Basalt-Cliff-Sunrise...jpg
  • A towering columnar basalt cliff is partially reflected in the waters of Breiðasund in the town of Stykkishólmur, Iceland. Columnar basalt is a volcanic rock formed when basalt lava rapidly cools at or very near the Earth's surface. Basalt, which is naturally grey or black, is rich in iron and can rapidly rust, taking on a reddish-brown appearance.
    Iceland_ColumnarBasalt_Stykkisholmur...jpg
  • A towering columnar basalt cliff is partially reflected in the waters of Breiðasund in the town of Stykkishólmur, Iceland. Columnar basalt is a volcanic rock formed when basalt lava rapidly cools at or very near the Earth's surface. Basalt, which is naturally grey or black, is rich in iron and can rapidly rust, taking on a reddish-brown appearance.
    Iceland_ColumnarBasalt_Stykkisholmur...jpg
  • A rock wren (Salpinctes obsoletus) rests on a basalt rock in the Columbia National Wildlife Refuge in Washington state. Rock wrens mainly feed on insects and spiders, using their long, curved bills to probe around rocks and other objects on the ground.
    Wren-Rock_Columbia-NWR_8491.jpg
  • A field of flowering goldenrods color the valley below a towering basalt cliff in the Columbia National Wildlife Refuge in Adams County, Washington.
    WA_Columbia-NWR_Goldenrod_Cliffs_758...jpg
  • Ripples spread across Soda Lake after a fish jumped out of the water in the Columbia National Wildlife Refuge in Washington state. The sunrise bathes the basalt cliffs on the opposite side of the lake in golden light.
    WA_Columbia-NWR_Soda-Lake_Ripples_09...jpg
  • The John Day River flows past the tall columnar basalt walls that make up Picture Gorge in John Day National Monument, Oregon. The white stains on the columns illustrate how high the water level has been.
    OR_JohnDay_PictureGorge_ColumnarBasa...jpg
  • A rainbow starts to rise from the Atlantic Ocean not far from Reynisdrangar sea stacks just off Reynisfjara beach near Vík í Mýrdal, Iceland. There are a number of Iceland legends about the basalt sea stacks. In the most common legend, two trolls were turned to stone as they were caught dragging a three-masted ship to shore at daybreak.
    Iceland_Vik_Troll-Rocks_Rainbow_2252.jpg
  • Atlantic Ocean waves crash through an arch on the Dyrhólaey peninsula near Vík, Iceland. Dyrhólaey means "the hill island with the door-hole" and there are several arches in the peninsula, including one that is spectacularly large. The peninsula's basalt cliffs are as much as 120 meters (394 feet) tall.
    Iceland_Dyrholaey_Waves_Arch_2218.jpg
  • Atlantic Ocean waves flow into a sea cave in a basalt cliff near Hellnar on the Snæfellsnes peninsula in western Iceland.
    Iceland_Hellnar_Sea-Cave_9271.jpg
  • Basalt cliffs tower over one of the Sage Lakes, located in the Columbia National Wildlife Refuge near Othello, Washington. The wildlife refuge is home to numerous lakes, even though the area receives less than eight inches of rain per year.
    WA_ColumbiaNWR_SageLakes_5767.jpg
  • Latourell Falls plunged 289 feet (76 metres) over a rocky basalt cliff in the Columbia Gorge of Oregon.
    LatourellFalls_8666.jpg
  • Faded petroglyphs depicting wildlife are visible on a basalt rock wall in Hieroglyphic Canyon, located in the Superstition Wilderness in Arizona. The petroglyphs were carved by the Hohokam people who lived in central and southern Arizona as early as 500 A.D.
    Petroglyphs_Superstition-Wilderness_...jpg
  • Pacific Ocean waves crash into Devils Churn, a narrow inlet located on the Oregon coast south of Yachats. Devils Churn is located in the Siuslaw National Forest and is the result of thousands of years of erosion on the basalt shoreline.
    OR_DevilsChurn_6089.jpg
  • A basalt wall is partially reflected onto the water of McMannaman Lake in the Columbia National Wildlife Refuge in Washington state.
    WA_Columbia-NWR_McMannaman-Lake_8782.jpg
  • Summer wildflowers, including lupine, grow on the basalt cliffs overlooking Palouse Falls in Washington state. The waterfall is 200 ft. (61 m) in height and is fed by the Palouse River.
    PalouseFalls_Wildflowers_9318.jpg
  • A band of clouds is reflected on the water of Soda Lake, located in the Columbia National Wildlife Refuge in Washington state.
    WA_Columbia-NWR_Soda-Lake-Panorama_8...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
  • Clouds, lit by the full moon, streak by Devils Tower National Monument in Wyoming. Thinner parts of the clouds caught the moons light; the streaks are the result of a four-minute exposure.
    DevilsTowerStreaks.jpg
  • Fresh snow covers the landscape surrounding Brandywine Falls, a 230-foot (70 meter) waterfall south of Whistler, British Columbia, Canada.
    BrandywineFalls.jpg
  • Comet C/2020 F3 (NEOWISE) shines in the sky above the Columbia National Wildlife Refuge near Othello, Washington, casting its reflection onto McMannaman Lake. Comet NEOWISE is a long-period comet and its current orbital path will take about 6,800 years to complete. Its nucleus is about 3 miles (5 kilometers) across and is covered with sooty, dark particles left over from its formation near the birth of our solar system 4.6 billion years ago.
    WA_Columbia-NWR_Comet-NEOWISE_8737.jpg
  • CratersMoonSplatterSunburst.jpg
  • A burrowing owl (Athene cunicularia) hunts for food from its perch on a rock in a large field in Grant County, Washington.
    Owl-Burrowing_Rock-Perch_Ephrata_020...jpg
  • Comet C/2020 F3 (NEOWISE) shines in the sky above the Columbia National Wildlife Refuge near Othello, Washington, casting its reflection onto McMannaman Lake. Comet NEOWISE is a long-period comet and its current orbital path will take about 6,800 years to complete. Its nucleus is about 3 miles (5 kilometers) across and is covered with sooty, dark particles left over from its formation near the birth of our solar system 4.6 billion years ago.
    WA_Columbia-NWR_Comet-NEOWISE_8072.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
  • Pacific Ocean waves crash up through Devils Churn, a narrow inlet on the Oregon coast near Yachats. Thousands of years of erosion carved an inlet that stretches for several hundred yards inland.
    OR_DevilsChurn_6122.jpg
  • Thick sheets of ice line the river that flows into the Dynjandisvogur Fjord in Iceland's West Fjords.
    Iceland_Dynjandisvogur.jpg
  • DevilsTowerSunrise.jpg
  • UpperMesaFalls.jpg
  • Haystack Rock is bathed in golden evening light as Pacific Ocean waves crash ashore at Chapman Beach near Cannon Beach, Oregon. Haystack Rock is a 235-foot (72-meter) sea stack, the third largest in the world. It was formed about 15 million years ago from basalt lava flows emanating from the Blue Mountains and Columbia basin.
    OR_Cannon-Beach_Haystack-Rock_Evenin...jpg
  • The western face of Haystack Rock in Cannon Beach, Oregon, is bathed in the golden light of the evening sun. Haystack Rock is a 235-foot (72-meter) sea stack, the third largest in the world. It was formed about 15 million years ago from basalt lava flows emanating from the Blue Mountains and Columbia basin.
    OR_Cannon-Beach_Haystack-Rock_Evenin...jpg
  • The midday sun shines behind the cross atop Hallgrímskirkja, a Lutheran church and prominent landmark in Reykjavík, Iceland. Icelandic architect Guðjón Samúelsson designed the church to resemble the basalt columns found around Iceland. Construction of Hallgrímskirkja took 38 years, reaching completion in 1986. Also visible in this image is a Leif Eriksson Memorial, which the United States gave to Iceland in 1930 to celebrate the 1000th anniversary of Iceland's parliament at Þingvellir.
    Iceland_Hallgrímskirkja_9898.jpg
  • Palouse Falls plunges 180 feet (55 meters) into a giant natural amphitheater surrounded by towering columnar basalt walls near Washtucna, Washington. Palouse Falls was formed at the end of the last ice age when a mammoth ice dam in Montana regularly collapsed, releasing a torrent of water that carved this winding gorge.
    WA_PalouseFalls_Gorge_9389.jpg
  • Gulls forage at the edge of the Pacific Ocean as Haystack Rock stands tall in the background in Cannon Beach, Oregon. Haystack Rock is a 235-foot (72-meter) sea stack, the third largest in the world. It was formed about 15 million years ago from basalt lava flows emanating from the Blue Mountains and Columbia basin.
    OR_Cannon-Beach_Haystack-Rock_Gulls_...jpg
  • A narrow band of cirrus clouds turn pink at sunrise high in the sky over Haystack Rock, a prominent sea stack on the Oregon coast at Cannon Beach. Haystack Rock is composed of basalt and was formed about 15 million years ago from lava flows emanating from the Blue Mountains and Columbia basin.
    HaystackRock_Pastel-Sunrise_Cannon-B...jpg
  • An ocean storm and one of the highest tides of the year causes water to spray high out of Devils Churn, a very narrow inlet located south of Yachats, Oregon. Pacific Ocean waves eroded the very narrow channel in the basalt. During storms and the highest tides, water erupts out of the end of the inlet.
    OR_DevilsChurn_Wide_5955.jpg
  • Red rock lines a large volcanic crater, one of many in an area known as Diamond Craters in southeastern Oregon. The area contains dozens of basaltic lava flows, cinder cones, and maars ranging in age from 6,000 to 60,000 years old.
    OR_DiamondCraters_3438.jpg
  • Two hardened tubes are visible in the Ape Cave, a lava tube located near Mount St. Helens in the Gifford Pinchot National Forest in Washington state. The ape cave formed about 2,000 years ago during the only known period when fluid basaltic lava erupted from the volcano. The outside edges of the lava flow cooled first, providing a crust that allowed fluid lava to continue flowing inside. This period of activity may have lasted a year during which the lava level rose and fell, leading to the unique shapes inside the cave. The Ape Cave lava tube is 13,042 feet (3976 meters) long, ranking as the third-longest in North America. The cave is named for a local hiking club, the St. Helens Apes.
    WA_Ape-Cave_Two-Tubes_1065.jpg
  • A pseudocrater is rendered in silhouette against a volanic cone at sunset in Mývatn in northern Iceland. Mývatn is a lake that was formed approximately 2,300 years ago during a volanic period. The shorter hill is a pseudocrater, also known as a rootless vent. While it resembles a volcanic cinder cone, it formed through a different process. As basaltic lava flowed over soggy lake sediments, it flash heated the moisture into vapor, causing it to blast through the lava. Mývatn means lake with midge flies; the lake is infested with them during the summer months.
    Iceland_Myvatn_Pseudocrater-Silhouet...jpg
  • Two hardened tubes are visible in the Ape Cave, a lava tube located near Mount St. Helens in the Gifford Pinchot National Forest in Washington state. The ape cave formed about 2,000 years ago during the only known period when fluid basaltic lava erupted from the volcano. The outside edges of the lava flow cooled first, providing a crust that allowed fluid lava to continue flowing inside. This period of activity may have lasted a year during which the lava level rose and fell, leading to the unique shapes inside the cave. The Ape Cave lava tube is 13,042 feet (3976 meters) long, ranking as the third-longest in North America. The cave is named for a local hiking club, the St. Helens Apes.
    WA_Ape-Cave_Two-Tubes_5130.jpg
  • A pseudocrater is rendered in silhouette against a volanic cone at sunset in Mývatn in northern Iceland. Mývatn is a lake that was formed approximately 2,300 years ago during a volanic period. The shorter hill is a pseudocrater, also known as a rootless vent. While it resembles a volcanic cinder cone, it formed through a different process. As basaltic lava flowed over soggy lake sediments, it flash heated the moisture into vapor, causing it to blast through the lava. Mývatn means lake with midge flies; the lake is infested with them during the summer months.
    Iceland_Myvatn_Pseudocrater-Silhouet...jpg
  • Molten pahoehoe lava flows at the end of a lava tube in Volcanoes National Park, Hawaii. Pahoehoe is the hottest – and most liquid – form of basaltic lava. This ropy pahoehoe results with the thin crust partially solidifies. Lava continues to flow behind it, pushing and folding it, not unlike an accordion.
    HI_Volcanoes_Pahoehoe_8679.jpg
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