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  • Numerous caves are visible a soft rock cliff wall in Bandelier National Monument, New Mexico. The national monument protects caves that were used by humans for shelters more than 11,000 years ago.
    NM_Bandelier_Wall-Texture_1635.jpg
  • Numerous caves are visible a soft rock cliff wall in Bandelier National Monument, New Mexico. The national monument protects caves that were used by humans for shelters more than 11,000 years ago.
    NM_Bandelier_Wall-Texture_1633.jpg
  • Mountains fill the view from Montezuma Pass in Coronado National Monument in Arizona. The foreground is dominated by the flank of Coronado Peak, a 6864-foot (2092-meter) peak in Coronado National Monument. In the background, the tallest mountain is Cerro San José, an 8,353-foot (2546-meter) mountain that is located across the border in Mexico.
    CoronadoNM_Montezuma-Pass_7346.jpg
  • A pair of yucca plants grow on a large dunes in White Sands National Monument in New Mexico. The white sand dunes are comprised of gypsum crystals, which is rarely found as sand because it is water-soluble. But the Tularosa Basin is surrounded by mountains and there is no direct outlet to the sea for any rain that falls there. Any water eventually drains through the ground leaving the gypsum behind in a crystalline form called selenite. White Sands National Monument is the largest gypsum dune field in the world.
    NM_WhiteSands_YuccaAndDunes_1295.jpg
  • 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
  • Lichen grows on the walls near the entrance of Beauty Cave, a 300-foot (100-meter) long lava tube in the Craters of the Moon National Monument, Idaho.
    CratersOfTheMoon_Beauty-Cave_2519.jpg
  • The white sand dunes of White Sand Dunes National Monument, New Mexico, appear blue and purple after sunset, reflecting the twilight sky. The white sand dunes are comprised of gypsum crystals, which is rarely found as sand because it is water-soluble. But the Tularosa Basin is surrounded by mountains and there is no direct outlet to the sea for any rain that falls there. Any water eventually drains through the ground leaving the gypsum behind in a crystalline form called selenite. White Sands National Monument is the largest gypsum dune field in the world.
    NM_WhiteSands_Fiery-Sunset_1036.jpg
  • The La Ventana Arch, located in the El Malpais National Monument in New Mexico, has a span of about 120 feet (36 meters), making it the second-largest arch in the state. La Ventana is Spanish for "the window."
    NM_El-Malpais_La-Ventana-Arch_1446.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 gnarled, bleached tree frames one of the many cinder cones in the Craters of the Moon National Monument in Idaho.
    CratersOfTheMoon_Cinder-Cone-Framed_...jpg
  • The La Ventana Arch, located in the El Malpais National Monument in New Mexico, has a span of about 120 feet (36 meters), making it the second-largest arch in the state. La Ventana is Spanish for "the window."
    NM_El-Malpais_La-Ventana-Arch_1440.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
  • This unusual "triple twist tree" growing out of a crack in a lava field at Craters of the Moon National Monument in Idaho helped scientists determine the age of the flow here. The tree has 1,350 rings, so scientists figure the flow here is about 2,000 years old. This flow is the youngest in Craters of the Moon National Monument.
    CratersOfTheMoon_Triple-Twist-Tree_2...jpg
  • A rock squirrel (Spermophilus variegatus) climbs on mesquite on a cliff overlooking Montezuma Well in Montezuma Castle National Monument near Camp Verde, Arizona. The rock squirrel belongs to the ground squirrel family, although it is known to climb trees and boulders.
    Squirrel-Rock_Mesquite_Montezuma-Wel...jpg
  • A close-up image of the trunk of an Arizona sycamore (Platanus wrightii) reveals abstract, almost monochromatic patterns of its bark. The Arizona sycamore is native to the states of Arizona and New Mexico. This Arizona sycamore was found in a lush area near Montezuma Well in Montezuma Castle National Monument.
    Sycamore_Arizona_Bark_Detail_Montezu...jpg
  • A close-up image of the trunk of an Arizona sycamore (Platanus wrightii) reveals abstract, almost monochromatic patterns of its bark. The Arizona sycamore is native to the states of Arizona and New Mexico. This Arizona sycamore was found in a lush area near Montezuma Well in Montezuma Castle National Monument.
    Sycamore_Arizona_Bark_Detail_Montezu...jpg
  • A male ornate tree lizard (Urosaurus ornatus) suns itself on a rock in a lush area near Montezuma Well in Montezuma Castle National Monument, Arizona.
    Lizard_Ornate-Tree_Montezuma-Well_55...jpg
  • An autumn sunrise reddens the sky over the Missouri River at Coal Banks Landing in the Upper Missouri River Breaks National Monument in Montana.
    MissouriRiver_Coal-Banks_Fiery-Sunri...jpg
  • An autumn sunrise reddens the sky over the Missouri River at Coal Banks Landing in the Upper Missouri River Breaks National Monument in Montana.
    MissouriRiver_Coal-Banks_Fiery-Sunri...jpg
  • Small caves are visible in the top of a sandstone bluff in El Malpais National Monument in New Mexico.
    NM_El-Malpais_Sandstone-Cave_1424.jpg
  • Late summer wildflowers are mixed in with the grassland as a rain storm approaches at the edge of the Grand Canyon-Parashant National Monument in Arizona.
    Grand-Canyon_Rainstorm_Grassland_491...jpg
  • A couple of trees grow between two large splatter cones resulting from the eruption of the north crater in Craters of the Moon National Monument, Idaho.
    CratersOfTheMoon_Splatter-Cones_Silh...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
  • The weathered remains of a pinyon pine tree appear to hold up cumulus clouds that pass over the Grand Staircase-Escalante National Monument in Utah.
    Grand-Staircase-Escalante_Weathered-...jpg
  • A bitterroot (Lewisia rediviva) grows among the lava rocks that make up a cider cone in the Craters of the Moon National Monument in Idaho.
    CratersOfTheMoon_Lava-Rock_Bitterroo...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
  • Pahoehoe lava, characterized by its smooth, rope-like appearance, is one of three types of lava. Pahoehoe's ropy surface forms when a thin skin of cool lava is shoved into folds by hot, more-fluid lava just below the surface. This sample was found in Craters of the Moon National Monument, Idaho. Pahoehoe is pronounced Pa-hoy-hoy.
    CratersOfTheMoon_Pahoehoe_2534.jpg
  • An adult male summer tanager (Piranga rubra) rests on a branch in a lush area at the base of Montezuma Well, part of Montezuma Castle National Monument in Arizona. Summer tanagers mainly eat bees and wasps and are typically found high in the forest canopy. The male summer tanager is the only completely red bird in all of North America.
    Tanager_Summer_Montezuma-Well_5462.jpg
  • A great horned owl (Bubo virginianus) sits at the entrance to its nest on a rocky ledge overlooking Montezuma Well in Arizona as its young owlet looks out. Montezuma Well is part of the Montezuma Castle National Monument, which protects ancient cliff dwellings built and used by the Sinagua people between 1100 and 1425 AD.
    Owl-Great-Horned_Nest_Montezuma-Well...jpg
  • A Wilson's warbler (Cardellina pusilla) pauses on a branch in the Coronado National Monument in Arizona during its spring migration to breeding grounds in the northern reaches of North America.
    Warbler-Wilsons_Perched_Coronado-AZ_...jpg
  • The Ape Cave makes a sharp bend in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave is 13,042 feet long (3,975 meters), making it the third-longest lava tube in North America. It formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust.
    WA_Ape-Cave_Bend_5094.jpg
  • Several lava rocks hang over the floor of the Ape Cave in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave is a lava tube, formed during an eruption of Mount St. Helens 2,000 years ago. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust. The rocks once hung from the ceiling of the cave, but broke off while lava was still flowing through the tube. They traveled with the flow until they became wedged in a narrow passage.
    WA_Ape-Cave_Lava-Rocks_5114.jpg
  • The ceiling of the Ape Cave, a lava tube in the Mount St. Helens National Volcanic Monument in Washington state, somewhat mimics the shape of the passage below. The Ape Cave is 13,042 feet long (3,975 meters), making it the third-longest lava tube in North America. It formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust.
    WA_Ape-Cave_Ceiling_5110.jpg
  • The Ape Cave gently curves in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave is 13,042 feet long (3,975 meters), making it the third-longest lava tube in North America. It formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust.
    WA_Ape-Cave_Passage_5087.jpg
  • The ceiling of the Ape Cave, a lava tube in the Mount St. Helens National Volcanic Monument in Washington state, somewhat mimics the shape of the passage below. The Ape Cave is 13,042 feet long (3,975 meters), making it the third-longest lava tube in North America. It formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust.
    WA_Ape-Cave_Ceiling_5111.jpg
  • A lava rock known as the "meatball" hangs over the floor of the Ape Cave in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave is a lava tube, formed during an eruption of Mount St. Helens 2,000 years ago. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust. The meatball once hung from the ceiling of the cave, but broke off while lava was still flowing through the tube. It traveled with the flow until it became wedged in a narrow passage.
    WA_Ape-Cave_Meatball_5116.jpg
  • Water that drips into the Ape Cave collects into a stream as it flows through North America’s third-largest lava tube, located in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust. The cave is 13,042 feet long (3,975 meters) and the rock is porous, allowing rainwater to seep in.
    WA_Ape-Cave_Stream_5105.jpg
  • A narrow passage of the Ape Cave gently curves in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave is 13,042 feet long (3,975 meters), making it the third-longest lava tube in North America. It formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust.
    WA_Ape-Cave_Narrow-Curve_5091.jpg
  • Water that drips into the Ape Cave collects into a stream as it flows through North America’s third-largest lava tube, located in the Mount St. Helens National Volcanic Monument in Washington state. The Ape Cave formed during an eruption of Mount St. Helens approximately 2,000 years ago. An 8-mile-long (13-kilometer-long) lava flow poured down the southern flank of the volcano. Lava cools from the outside-in, so the flow became like a straw, allowing lava to continue to flow through a hardened crust. The cave is 13,042 feet long (3,975 meters) and the rock is porous, allowing rainwater to seep in.
    WA_Ape-Cave_Stream_5104.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 side-blotched lizard (Uta stansburiana) rests in a crack in a sandstone cliff in the Grand Canyon-Parashant National Monument near Tuweep, Arizona.
    Lizard_SideBlotched_4594.jpg
  • A yucca plant grows on one of the white dunes in White Sands National Monument in New Mexico. The white sand dunes are comprised of gypsum crystals, which is rarely found as sand because it is water-soluble. But the Tularosa Basin is surrounded by mountains and there is no direct outlet to the sea for any rain that falls there. Any water eventually drains through the ground leaving the gypsum behind in a crystalline form called selenite. White Sands National Monument is the largest gypsum dune field in the world.
    NM_WhiteSands_YuccaAndDunes_1266.jpg
  • A pair of yucca plants grow on a large dunes in White Sands National Monument in New Mexico. The white sand dunes are comprised of gypsum crystals, which is rarely found as sand because it is water-soluble. But the Tularosa Basin is surrounded by mountains and there is no direct outlet to the sea for any rain that falls there. Any water eventually drains through the ground leaving the gypsum behind in a crystalline form called selenite. White Sands National Monument is the largest gypsum dune field in the world.
    NM_WhiteSands_YuccaAndDunes_1299.jpg
  • The five-story cliff dwelling known as Montezuma Castle is visible up a sheer limestone cliff in Montezuma Castle National Monument near Camp Verde, Arizona. Montezuma Castle and other cliff dwellings in the area were built and used by the Sinagua people between approximately 1100 and 1425 AD. Montezuma Castle, which contains 45-60 rooms, is one of the best-preserved cliff dwellings in North America, likely due to its placement 90 feet (27 meters) up the cliff and the protection from the elements provided by the rock overhang.
    AZ_Montezuma-Castle_2489.jpg
  • The five-story cliff dwelling known as Montezuma Castle is visible up a sheer limestone cliff in Montezuma Castle National Monument near Camp Verde, Arizona. Montezuma Castle and other cliff dwellings in the area were built and used by the Sinagua people between approximately 1100 and 1425 AD. Montezuma Castle, which contains 45-60 rooms, is one of the best-preserved cliff dwellings in North America, likely due to its placement 90 feet (27 meters) up the cliff and the protection from the elements provided by the rock overhang.
    AZ_Montezuma-Castle_Framed_2485.jpg
  • The Ringold Formation, a series of bluffs overlooking the Columbia River near Pasco, Wasington, preserves fossils dating back to the Neogene period and is part of the Hanford Reach National Monument.
    Hanford-Reach_Ringold_6668.jpg
  • The dunes in White Sands National Monument, New Mexico, make up the largest gypsum dune field in the world. The white sand dunes are comprised of gypsum crystals, which is rarely found as sand because it is water-soluble. But the Tularosa Basin is surrounded by mountains and there is no direct outlet to the sea for any rain that falls there. Any water eventually drains through the ground leaving the gypsum behind in a crystalline form called selenite.
    NM_WhiteSands_DuneField_1280.jpg
  • Small caves are visible in the top of a sandstone bluff in El Malpais National Monument in New Mexico.
    NM_El-Malpais_Sandstone-Cave_1416.jpg
  • The sun shines through Owachomo Bridge, one of several natural bridges contained in Natural Bridges National Monument in Utah. Owachomo means "rock mound" in the Hopi language; there is a large rock mound on a bluff overlooking the bridge.
    OwachomoBridgeUT.jpg
  • Moss begins to overtake the rocky landscape within the blast zone at Mount St. Helens National Monument, Washington. This image was captured nearly 30 years after the violent May 18, 1980 eruption. The first wildflowers began to appear in this spot about 20 years after the eruption.
    MountStHelens_lichen_6801.jpg
  • A soaptree yucca (Yucca elata) casts a long shadow over a dune in the White Sands National Monument in New Mexico. Shifting sand has partially buried this yucca. The plant's stem can grow as much as one foot per year to help it keep its leaves above the sand.
    NM_WhiteSands_YuccaShadow_1291.jpg
  • The deep branches in the soil of the Painted Hills in John Day National Monument, Oregon illustrate the dendritic drainage pattern. Numerous feeder streams, creeks and rills flow into the main channel, resulting in a deep channel that resembles the branches of a tree.
    OR_PaintedHills_DendriticDrainage_31...jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_CloseUp_3145.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. Eventually the layers were thrust upward and tilted by movement of the Earth's plates. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_WideView_3192.jpg
  • This panorama shows the colorful layers that give the Painted Hills in the John Day National Monument in Oregon their name. The layers represent different ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_Panorama_3098.jpg
  • Colorful crustose lichens grow on lava rock at Craters of the Moon National Monument in Idaho. Lichens are a symbiosis of a fungus and a green alga and/or cyanobacterium. Crustose are very slow growing, typically growing 1 millimeter or less per year.
    CratersOfTheMoon_Lichen_2479.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. Eventually the layers were thrust upward and tilted by movement of the Earth's plates. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_Palette_3240.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_CloseUp_3185.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
  • Low-angle sunlight shows the texture of the colorful Painted Hills in the John Day National Monument in Oregon. The layers represent different ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_DeepShadow_3175.jpg
  • Sheep Rock, the tall mountain at the center of the frame, towers over Picture Gorge in John Day National Monument, Oregon, at sunrise. The moutain was named for the bighorn sheep that used to live in the area.
    OR_JohnDay_SheepRock_PictureGorge_32...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
  • Towering hummocks - piles of debris from the 1980 eruption of Mount St. Helens - are found along the Hummocks Trail at the Mount St. Helens National Monument in Washington.
    StHelens_Hummocks_6317.jpg
  • Thich fog bunches up and spills over a hillside above Smith Creek in Mount St. Helens National Monument, Washington.
    StHelens_FogFalls_3422.jpg
  • Owachomo Bridge is the smallest, thinnest, and likely oldest natural bridge in Natural Bridges National Monument, Utah. Its span measures 180 feet (55 meters) and its only 9 feet (3 meters) thick at its thinnest point.
    OwachomoSunsetUT.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
  • Grasses and summer wildflowers, including Indian paintbrush, begin to restablish the otherwise barren hillside beneath Johnston Ridge in Mount St. Helens National Monument, Washington.
    StHelens_Wildflowers_6335.jpg
  • A rainbow stretches across the sky above the Vermilion Cliffs near Page, Arizona. The Vermilion Cliffs, which rise as much as 3,000 feet (914 meters), are the second step in the five-step Grand Staircase of the Colorado Plateau, which stretches from northern Arizona to southern Utah.  The cliffs are made up of sedimentary rocks, primarily sandstone, siltstone, limestone, and shale, that have eroded over millions of years. The Vermilion Cliffs were designated as the Vermilion Cliffs National Monument in 2000.
    AZ_VermilionCliffs_Rainbow_8507.jpg
  • Paulina Creek drops 80 feet (24 meters) at Paulina Falls, located in the Newberry National Volcanic Monument in Deschutes County, Oregon. Paulina Falls is located on the west flank of the Newberry Volcano, a potentially active volcano that last erupted nearly 1,500 years ago. The waterfall flows over and erodes remnants of previous eruptions; over a period of 2,000 years, geologists believe the waterfall has moved 200 feet (61 meters) upstream due to erosion.
    OR_PaulinaFalls_Newberry_9870.jpg
  • Sunrise turns golden the rugged coastline of the Otter Cliffs and Monument Cove in Acadia National Park, Maine.
    Acadia_OtterCliffs_0877.jpg
  • El Capitan, a prominent granite monolith in Yosemite National Park, California, extends about 3,000 feet (900 meters) from the Yosemite Valley floor. The summit of El Capitan is at an elevation of 7,573 feet (2,308 meters).
    Yosemite_ElCapitan_PicnicView_1110.jpg
  • El Capitan, a prominent granite monolith in Yosemite National Park, California, is turned golden by the rising sun. The summit of El Capitan is at an elevation of 7,573 feet (2,308 meters); it extends about 3,000 feet from the Yosemite Valley floor.
    Yosemite_ElCapitan_Sunrise_0923.jpg
  • LeaningTreeCratersMoon.jpg
  • CratersMoonSplatterSunburst.jpg
  • SipapuBridgeV.jpg
  • SipapuBridgeH.jpg
  • DevilsTowerSunrise.jpg
  • Numerous Sierra Nevada mountains and ridges are visible through a hazy, golden sunset above Kings Canyon in California. Among the peaks are Converse Mountain (foreground), Rogers Ridge (foreground center), 8167-foot (2489-meter) Patterson Mountain (background right), and 6697-foot (2041-meter) Dinkey Mountain (background left).
    CA_KingsCanyon_SierraNevada_GoldenSu...jpg
  • Tens of thousands of California goldfields (Lasthenia californica) blanket the Carrizo Plain in the southern San Joaquin Valley of California. The Carrizo Plain is the single largest remaining section of native grasslands, which used to be common in Califonria.
    CA_Goldfields_CarrizoPlain_7830.jpg
  • Life returns to the blast zone near Mount St. Helens in Washington state. Trees line a large pond. Large hummocks -- hills of volcanic debris -- are visible behind the pond.
    MountStHelens_Hummocks_Pond_6807.jpg
  • Mount St. Helens glows bright white in the alpenglow after sunset. The Toutle River winds through the blast zone created during the May 18, 1980 eruption. That eruption reduced the Washington mountain's summit from9,677 feet (2,950 m) to 8,365 feet (2,550 m).
    MountStHelens_Alpenglow_6841.jpg
  • The horseshoe-shaped crater of Mount St. Helens is visible in this aerial view of the Washington state volcano. During the May 18, 1980 eruption, the north face of the volcano collapsed. Since then, new lava domes have formed in the crater and are visible here. Mount St. Helens now stands ‎8,363 feet (2,549 meters), losing about 13 percent of its summit in the 1980 eruption. It is the most active volcano in the Cascade Range during the Holocene epoch (past 10,000 years).
    MountStHelens_Crater_Aerial-View_Alp...jpg
  • A black-tailed prairie dog looks out from its burrow in a grassy field near Devil's Tower National Monument, Wyoming.
    PrairieDogWyoming.jpg
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