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  • A narrow band of sunlight illuminates on band of rolling hills in the Antelope Valley of California near Liebre Mountain.
    CA_Antelope-Valley_Rolling-Hills_462...jpg
  • The tops of some golden grasses poke through deep snow covering rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3364.jpg
  • Hundreds of saguaros (Carnegiea gigantea) fill the valley at the base of the Red Hills, which were cast into shadow by passing clouds, in Saguaro National Park, Arizona.
    Saguaro-NP_Saguaros_Red-Hills_0779.jpg
  • A band of cirrus clouds turns pink at sunset over the Calico Hills in the Red Rock Canyon Conservation Area in Nevada. The Calico Hills are made up of Aztec Sandstone, fossilized sand dunes that were laid down during the early Jurrasic Period 180-190 million years ago.
    NV_Red-Rock-Canyon_Calico-Hills_Suns...jpg
  • A hillside of the Beezley Hills near Quincy, Washington, is filled with blooming Arrowleaf balsamroot (Balsamorhiza sagittata) wildflowers in early spring.
    Balsamroot_Beezley-Hills_Quincy_4047.jpg
  • Oak trees and yellow wildflowers line the rolling hills of Diablo State Park near Clayton, California.
    CA_Mount-Diablo_Rolling-Hills_1962.jpg
  • A burro (Equus asinus), also known as a donkey, stands among the Calico Hills in the Red Rock Canyon Conservation Area in Nevada. Burros were introduced to the area in the 1800s by miners and ranchers who used them to haul heavy cargo. Some escaped or were freed, becoming wild (technically feral). The Red Rock Canyon area is part of the Mojave Desert and is a harsh environment, but the burros are able to survive by finding spring water and feeding on grasses.
    Burro_Calico-Hills_Red-Rock-Canyon_N...jpg
  • Sedimentary layers are visible in this section of the Calico Hills in the Red Rock Canyon Conservation Area in Nevada. The Calico Hills are made up of Aztec Sandstone, fossilized sand dunes that were laid down during the early Jurrasic Period 180-190 million years ago.
    NV_Red-Rock-Canyon_Sedimentary-Layer...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
  • An aerial view shows the great contrast in color of the hills in the Hungry Valley area of Los Angeles County, California.
    CA_Hungry-Valley_Aerial_7722.jpg
  • The crescent moon sets over three hills visible from the Wonderland Trail in Mount Rainier National Park, Washington.
    CrescentMoon_ThreeHills_3575.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
  • 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
  • Mobius Arch, a natural granite arch in the Alabama Hills near Lone Pine, California, frames several high Sierra peaks, including Lone Pine and Mount Whitney. Mount Whitney is the highest mountain in the contiguous United States with an elevation of 14505 feet (4421 meters).
    AlabamaHills_MobiusArch_6740.jpg
  • A natural window in a boulder pile in the Alabama Hills near Lone Pine, California, frames Mount Whitney at sunrise. Mount Whitney, part of the Sierra Nevada range, is the tallest mountain in the 48 contiguous United States with an elevation of 14505 feet (4421 meters).
    MountWhitney_NaturalWindow_6717.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
  • 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
  • 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
  • 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
  • A cluster of trees stands atop snow-covered rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3331.jpg
  • A cluster of trees stands atop snow-covered rolling hills in Ashton, Idaho.
    ID_Ashton_Rolling-Hills_Winter_3288.jpg
  • The hills of the Blue Mountains in Columbia County, Washington, are bathed in golden light after sunset. The Blue Mountains are named for their apparent color when viewed during the day at a distance. Most of the mountain range extends into Oregon and its river valleys and lower levels were occupied by indigenous peoples for thousands of years.
    WA_Blue-Mountains_Sunset_9325.jpg
  • Sediment layers are visible in the badland hills of bluish bentonite clay in an area known as the Blue Mesa in Petrified Forest National Park, Arizona.
    AZ_Petrified-Forest_Blue-Mesa_6618.jpg
  • Sediment layers are visible in the badland hills of bluish bentonite clay in an area known as the Blue Mesa in Petrified Forest National Park, Arizona.
    AZ_Petrified-Forest_Blue-Mesa_Detail...jpg
  • Erosion debris from petrified logs and the bentonite clay hills collects at the base of the badlands of the Blue Mesa in Petrified Forest National Park, Arizona.
    AZ_Petrified-Forest_Blue-Mesa_Erosio...jpg
  • The erosion patterns of the hills in the Sante Fe National Forest are visible in this aerial view captured from near El Valle, New Mexico.
    NM_Sante-Fe-Forest_Aerial_2409-BW.jpg
  • Golden California poppies (Eschscholzia californica) grow on the rolling hills of the Morgan Territory Regional Preserve near Antioch, California. Mount Diablo, a prominent upthrust peak that rises 3,849 feet (1,173 meters), is visible in the background.
    CA_Morgan-Territory_Poppies_Mount-Di...jpg
  • Late afternoon storm clouds develop over lichen-covered volcanic rocks and hills near Hveragerði in southern Iceland.
    Iceland_Developing-Clouds_Volcanic-R...jpg
  • Mobius Arch, a natural granite arch in the Alabama Hills near Lone Pine, California, frames Mount Whitney at sunrise. Mount Whitney is the highest mountain in the contiguous United States with an elevation of 14505 feet (4421 m).
    MountWhitney_MobiusArch_Sunrise_6845.jpg
  • A natural window in a boulder pile in the Alabama Hills near Lone Pine, California, frames several Sierra Nevada peaks, including Lone Pine and Mount Whitney. Mount Whitney, at right, is the tallest mountain in the 48 contiguous United States, with an elevation of 14505 feet (4421 m).
    SierraNevada_Window_6727.jpg
  • Needles Eye, a prominent granite formation in Custer State Park in South Dakota, stands nearly 40 feet tall and has an unusual slit that's only a few feet across. The granite in the Black Hills of South Dakota erodes at a rate of about one inch per 40,000 years.
    NeedlesEye.jpg
  • A tree that appears to be wind-swept stands at the summit of a rolling hill in the foothills of Mount Diablo near Clayton, California.
    CA_Clayton_Wind-Swept-Tree_1421.jpg
  • Two oak trees — one young and vibrant, the other old and weathered — stand at the top of a hill in the foothills of Mount Diablo near Clayton, California.
    CA_Clayton_TreesOnHillside_1435.jpg
  • The sun sets in a gap between peaks over the Big Run Basin, the largest single watershed in Shenandoah National Park, Virginia.
    Shenandoah_Big-Run_Sunset_9316.jpg
  • The badlands of Theodore Roosevelt National Park, North Dakota, are turned golden by the setting sun in this view from the Painted Canyon Overlook.
    ND_RooseveltNP_Painted-Canyon_2004.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
  • Diffused golden light at sunrise colors the high desert landscape and rock outcroppings in the Mormon Basin of Malheur County, Oregon.
    OR_Mormon-Basin_Outcroppings_4014.jpg
  • The summit of Dead Indian Ridge, located in Washington County Idaho, is in deep shadow as a band of altostratus clouds pass overhead in this view from near Huntington, Oregon.
    ID_Dead-Indian-Ridge_Shadow_3959.jpg
  • The dramatic Cathedral Spires rise nearly a thousand feet from the surrounding landscape in Custer State Park, South Dakota. This image was captured from the summit of Little Devils Tower.
    CathedralSpires.jpg
  • Several erosion patterns are visible on the steep exposed hillside of Rucker Hill in Everett, Washington, near where Pigeon Creek empties into Puget Sound. At the top of the frame, a blackberry branch swings back and forth like a pendulum, carving a semicircle into the hillside.
    WA_Rucker-Hill_Erosion_7166.jpg
  • Thick fog begins to form on the beach below Strawberry Hill, located on the Oregon coast south of Yachats.
    OR_StrawberryHill_Foggy_3063.jpg
  • Purple Hill is reflected in the icy waters of Lake Pearson, located near Arthur's Pass, New Zealand.
    NZ_ArthursPass_LakePearson_4859.jpg
  • A large kiawe (Prosopis pallida) tree frames of the southwestern coast of the Hawaiian island of Maui near the town of Makena. The first kiawe tree was introduced to Hawaii in 1828 and is now one of the most common trees in the dry lowlands of the Hawaiian islands. The prominent hill visible just to the right of the center of this image if Pu`u Ola`i, a 320-foot (98-meter) cinder cone formed when molten lava erupted from a volcanic vent and fell back to earth forming a nearly perfect cone. Pu`u Ola`i is also known as Earthquake Hill, Red Hill, and Round Mountain.
    Maui_Makena_Kiawe_PuuOlai_6384.jpg
  • A large kiawe (Prosopis pallida) tree frames of the southwestern coast of the Hawaiian island of Maui near the town of Makena. The first kiawe tree was introduced to Hawaii in 1828 and is now one of the most common trees in the dry lowlands of the Hawaiian islands. The prominent hill visible just to the right of the center of this image if Pu`u Ola`i, a 320-foot (98-meter) cinder cone formed when molten lava erupted from a volcanic vent and fell back to earth forming a nearly perfect cone. Pu`u Ola`i is also known as Earthquake Hill, Red Hill, and Round Mountain.
    Maui_Makena_Kiawe_PuuOlai_6412.jpg
  • Bright green moss engulfs a tree in a ravine on Rucker Hill in Everett, Washington.
    Mossy-Tree_Rucker-Ravine_Everett_041...jpg
  • An adult bald eagle (Haliaeetus leucocephalus) flies next to a snow-covered hillside along the Nooksack River near Welcome, Washington. Hundreds of bald eagles winter in the area to feast on spawned-out salmon.
    Bald-Eagle_Snowy_Hillside_Nooksack_5...jpg
  • Several birch trees frame the view of the fall color that covers the hillsides surrounding Union Falls Pond in the Adirondacks of New York. Gilpin Hill, Bear Mountain, and Cranberry Mountain are visible in this image.
    Adirondacks_UnionFallsPond_Autumn_11...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
  • 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
  • A handful of evergreen trees stand out against a backdrop of bare winter trees on a hillside overlooking Gos Ventre in Grand Teton National Park, Wyoming.
    Grand-Teton-NP_Winter-Hillside_1975.jpg
  • The outstretched wings of a Brown Pelican (Pelecanus occidentalis) in flight mimics the shape of the mountains south of Puerto Vallarta, Mexico.
    Pelican_Brown_PuertoVallarta_Mountai...jpg
  • A power boat races between narrow canyons that meet the Pacific Ocean along the Na Pali coast of Kauai, Hawaii.
    NaPaliAerial2.jpg
  • MissouriRiverJudith1.jpg
  • An adult bald eagle (Haliaeetus leucocephalus) flies next to a snow-covered hillside along the Nooksack River near Welcome, Washington. Hundreds of bald eagles winter in the area to feast on spawned-out salmon.
    Bald-Eagle_Snowy_Hillside_Nooksack_7...jpg
  • Dozens of narrow canyons meet the Pacific Ocean along the Na Pali coast of Kauai, Hawaii.
    NaPaliAerial1.jpg
  • MissouriRiverJudith2.jpg
  • Two fallen Douglas Fir trees rest on a steep hillside overlooking Smallpox Bay on San Juan Island, Washington.
    WA_San-Juan-Island_Downed-Trees_Bay_...jpg
  • A layer of fog passes over Sparks Lake in Deschutes National Forest, Oregon. A small island in the lake is covered with yellow spear-leaf arnica (Arnica longifolia) flowers.
    OR_Sparks-Lake_Island_Arnica_Fog_382...jpg
  • Golden grasses and California poppies blow in the strong wind along the Seaview Trail in Tilden Regional Park near Berkeley, California.
    CA_Tilden_Grasses_Wind_1727.jpg
  • Dozens of narrow canyons meet the Pacific Ocean along the Na Pali coast of Kaua`i, Hawai`i.
    NaPali_Coast_8233.jpg
  • Moss, ferns, and trees grow from a large rock outcropping near the Minister Valley in Allegheny National Forest in Warren, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Outcropping_Roots_8652.jpg
  • Several dramatic rock formations stand at the top of one of the hills in the Hartman Rocks Recreation Area near Gunnison, Colorado.
    CO_HartmanRocks_1900.jpg
  • A vervet monkey (Chlorocebus pygerythrus) enjoys a meal from its perch high in a eucalyptus tree in the hills near Nyamweru, Rwanda.
    Rwanda_Vervet-Monkey_5468.jpg
  • A compressed view shows the contrasting water flow patterns of two parts of a curved waterfall located in the Frenchman Hills Wasteway in Potholes State Park, Grant County, Washington.
    WA_Potholes_Waterfall-Patterns_7723.jpg
  • The sun shines between a tree and a large rock outcropping in the Minister Valley area of the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Outcropping_86...jpg
  • A lush jungle grows on the hills above Sayulita, Mexico.
    Sayulita_jungle_1052.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
  • Fog hangs low over the East Fork Kimball Creek, hidden behind the trees, as the rising sun colors the clouds over the hills bordering Snoqualmie, Washington.
    WA_Snoqualmie-Valley_Morning-Fog_582...jpg
  • Rock outcroppings provide a vantage point to take in a sweeping view of the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_MinisterValley_Overlook...jpg
  • Several evergreen wood ferns (Dryopteris intermedia) grow on a mossy rock outcropping near the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Fern_Rock_8643.jpg
  • Several evergreen wood ferns (Dryopteris intermedia) grow on a mossy rock outcropping near the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Fern_Rock_8642.jpg
  • A vervet monkey (Chlorocebus pygerythrus) relaxes, clinging to its perch in a tree in the hills near Nyamweru, Rwanda.
    Rwanda_Vervet-Monkey_5571.jpg
  • Moss, ferns, and trees grow from a large rock outcropping near the Minister Valley in Allegheny National Forest in Warren, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Outcropping_Roots_8656.jpg
  • A mule deer (Odocoileus hemionus) climbs a hill in the Blue Mountains of Washington state.
    Deer-Mule_Blue-Mountains-WA_9304.jpg
  • A pronghorn (Antilocapra americana) walks on a snow-dusted hill in Yellowstone National Park, Montana. They are often mistakenly referred to as antelope, although they are more closely related to giraffes than to Old World antelope.
    Pronghorn_Winter_Yellowstone_3328.jpg
  • Two fulmars fly between the southern coast of Iceland and the Dyrhólaey peninsula. The peninsula features several sea arches, resulting its name, which means "the island with the hill door." During the early summer, thousands of fulmars (Fulmarus glacialis) nest on rocky cliffs throughout Iceland.
    Iceland_Dyrholaey_Fulmars_7525.jpg
  • Mount Angeles is obscured by thick clouds and fog. This sunset scene was captured from the summit of a rocky peak along the Hurricane Hill trail in Olympic National Park, Washington.
    OlympicNP_Mount-Angeles_Fog_5024.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
  • A bull elk stands on a hill next to the Roosevelt Arch, which marked the first major entrance into Yellowstone National Park. The arch, located in Gardiner, Montana, is inscribed with the words, "For the benefit and enjoyment of the people," a quote from the Organic Act of 1872, which created Yellowstone, the first national park. The arch was named for President Theodore Roosevelt who was visiting the park during the construction of the arch; he asked to place its cornerstone.
    Yellowstone_Roosevelt-Arch_Elk_5852.jpg
  • The sun sets behind a hill overlooking a field of cholla cacti in Abiquiu, New Mexico.
    NM_Abiquiu_Cholla_Sunset_6702.jpg
  • A telephoto lens compresses the view of bare winter trees in and on a hill overlooking Golden Gardens Park, Seattle, Washington.
    Forest_Winter_Abstract_Golden-Garden...jpg
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