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  • 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
  • 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
  • Cathedral Rock, a 4,967 foot (1,514 meter) sandstone butte, is reflected on Oak Creek in Sedona, Arizona. Cathedral Rock is located in the Coconino National Forest.
    AZ_Cathedral-Rock_Oak-Creek_Sedona_6...jpg
  • A band of clouds, showing a hint of pink at dusk, passes over Cathedral Rock near Sedona, Arizona. Cathedral Rock is a 4,967 foot (1,514 meter) sandstone butte that is located in the Coconino National Forest.
    AZ_Cathedral-Rock_Sedona_Clouds_Dusk...jpg
  • Cathedral Rock, a 4,967 foot (1,514 meter) sandstone butte, is reflected in a small pool near Oak Creek in Sedona, Arizona. Cathedral Rock is located in the Coconino National Forest.
    AZ_Cathedral-Rock_Sedona_Reflection_...jpg
  • Elephant Rock, a natural sandstone arch that resembles an elephant with a long trunk, stands at the east side of the Valley of Fire State Park in Nevada.
    vof-elephant-rock.jpg
  • A rock rests in a depression on driftwood on the beach of Marina Beach Park in Edmonds, Washington.
    Driftwood_Rock-Depression_Edmonds_03...jpg
  • A red rock crab (Cancer productus) walks across the murky bottom of Puget Sound off Des Moines Beach Park, Des Moines, Washington.
    Crab_RedRock_DesMoines_F0112.jpg
  • Courthouse Butte becomes intense red at sunset as it stands tall over a small meadow in the Coconino National Forest near Oak Creek, Arizona. Courthouse Butte stands 5,454 feet (1,662 meters) tall and is part of the Red Rock Country area of Sedona.
    AZ_Courthouse-Butte_Sunset_Oak-Creek...jpg
  • Rugged rock faces are turned red at sunrise in the Valley of Fire, Nevada. The Valley of Fire is Nevada's oldest state park and named for the dramatic sandstone formations that are fire-colored in certain types of sunlight.
    VOF_ValleyOfFire_RedRockFace_2200.jpg
  • Courthouse Butte stands tall over a small meadow in the Coconino National Forest near Oak Creek, Arizona. Courthouse Butte stands 5,454 feet (1,662 meters) tall and is part of the Red Rock Country area of Sedona. Lee Mountain, visible in the background, is even taller with a highest point of 6,592 feet (2009 meters).
    AZ_Courthouse-Butte_Lee-Mountain_270...jpg
  • Potholes in the red rock sandstone at Tuweep in Grand Canyon National Park, Arizona, are filled with water after a rainstorm passed at night. The nightime landscape was lit by the full moon.
    AZ_Tuweep_Potholes_Night_4748.jpg
  • Molten lava makes dramatic curved patterns as it breaks through solid rock in Volcanoes National Park, Hawaii.
    LavaFlow-8661.jpg
  • Petroglyphs carved by members of the Fremont Culture are visible in a sheer sandstone face in the Fremont River canyon in Capitol Reef National Park, Utah. The rock face includes symbols of bighorn sheep and other animals as well as people. The Fremont Culture lived in the area from 300-1300 Common Era (CE).
    Capitol-Reef_Petroglyphs_1278.jpg
  • Wilson Mountain, the tallest of the red and white sandstone peaks near Sedona, Arizona, is framed by other formations. Wilson Mountain has an elevation of 7,122 feet (2171 meters), and its summit provides some of the grandest views in northern Arizona.
    AZ_WilsonMountain_Sedona_8968.jpg
  • The moon rises in a break in storm clouds passing over the dramatic red rocks of Bryce Canyon National Park in Utah.
    Bryce-Canyon_Stormy-Moonrise_4351.jpg
  • Approaching storm clouds, turned red by the setting sun, frame the moon as it rises over a large hoodoo in Bryce Canyon National Park, Utah. Hoodoos are remanants of large sandstone fins that have been subjected to centuries of erosion.
    Bryce-Canyon_Moonrise_4375.jpg
  • The Colorado River makes a dramatic, almost circular bend at Horseshoe Bend, south of Page, Arizona, in the Glen Canyon National Recreation Area. The towering red cliffs are about 1,000 feet (305 meters) above the river.
    AZ_Horsehoe-Bend_Stormy-Sunrise_0613.jpg
  • Approaching storm clouds, turned red by the setting sun, frame the moon as it rises over a large hoodoo in Bryce Canyon National Park, Utah. Hoodoos are remanants of large sandstone fins that have been subjected to centuries of erosion.
    Bryce-Canyon_Moonrise_4378.jpg
  • A rock exposed at low tide seems to glow when exposed to ultraviolet light at the edge of Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Low-Tide_Rock_Des-Moines_...jpg
  • Sea life growing on a cracked rock exposed at low tide glows when exposed to ultraviolet light at the edge of Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Low-Tide_Cracked-Rock_Des...jpg
  • A rock exposed at low tide seems to glow when exposed to ultraviolet light at the edge of Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Low-Tide_Rock_Des-Moines_...jpg
  • A western red cedar (Thuja plicata) grows over and around boulders on a bluff near Pigeon Point, Bow, Washington. An American robin (Turdus migratorius) rests on one of the exposed roots.
    Cedar_Western-Red_Boulders_Chuckanut...jpg
  • Balanced Rock (left), a prominent feature of Arches National Park near Moab, Utah, is turned red by the golden light of sunrise. The balanced rock is a cap rock that is 55 feet (17 meters) tall and makes up nearly half the overall height of the formation. The formation is made up of several layers of sandstone, which erode at different rates; the layer between the cap rock and the pedestal erodes at a much faster rate than the others.
    ArchesNP_BalancedRock_F02_2576-08.jpg
  • Balanced Rock, a prominent feature of Arches National Park near Moab, Utah, is turned red by the golden light of sunrise. The balanced rock is a cap rock that is 55 feet (17 meters) tall and makes up nearly half the overall height of the formation. The formation is made up of several layers of sandstone, which erode at different rates; the layer between the cap rock and the pedestal erodes at a much faster rate than the others.
    ArchesNP_BalancedRock_F02_2576-06.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
  • Balanced Rock, lit by the setting sun, is framed by the snow-covered landscape in Arches National Park, Utah.
    BalancedRockSnowH.jpg
  • The setting sun colors the sky above Haystack Rock, a prominent sea stack located off the coast of Cape Kiwanda near Pacific City, Oregon.
    HaystackRockKiwandaSunset.jpg
  • Arch Rock, one of the most famous arches in the Valley of Fire State Park, Nevada, frames another towering sandstone formation.
    vof-ArchRock.jpg
  • Weathered driftwood rests against a large beach rock in Marina Beach Park, Edmonds, Washington.
    Driftwood_Weathered_Smooth_Edmonds_0...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
  • 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
  • Abstract shapes are left behind on an eroded sandstone wall near Landscape Arches National Park, Utah.
    Arches_Sandstone-Wall_Texture_5060.jpg
  • Rain water collects in several potholes in the hard, sandstone desert landscape at Tuweep in Grand Canyon National Park, Arizona. Tuckup Point is visible in the background. This image was captured at night; the landscape was lit by the full moon.
    AZ_Tuweep_Tuckup_Potholes_Night_4757.jpg
  • Rain water collects in several potholes in the hard, sandstone desert landscape at Tuweep, Arizona. Tuckup Point is visible in the background. This image was captured at night; the landscape was lit by the full moon.
    AZ_Tuckup_Potholes_Night_4742.jpg
  • The south rim of the Grand Canyon casts its shadow into the canyon in the late afternoon in this view from near Pipe Creek Vista, Grand Canyon National Park, Arizona.
    Grand-Canyon_South-Rim-Shadow_Pipe-C...jpg
  • The layers that make up the eroding walls of the Grand Canyon are visible from the Desert View vantage point on the south rim of Grand Canyon National Park, Arizona.
    GrandCanyon_DesertView_8607.jpg
  • The late afternoon sun causes Bright Angel Canyon to fall into a deep shadow. Bright Angel Canyon is one of several tributary canyons that feed into the Grand Canyon. This image was captured from the Mather Point, located on the south rim of Grand Canyon National Park, Arizona.
    BrightAngelCanyon.jpg
  • A cottonwood tree stands at the base of Mount Moroni, which is partially shrouded by storm clouds in Zion National Park, Utah. Mount Moroni is one of three dramatic peaks, which together are known as the Three Patriarchs.
    Zion_MountMoroni_Cottonwood_Stormy_5...jpg
  • A partial rainbow forms in the downpour from a rainstorm passing at the edge of Bryce Canyon National Park in Utah.
    Bryce-Canyon_Rainstorm_4350.jpg
  • An approaching autumn storm is visible on the ampitheater cliffs in this view from Rainbow Point in Bryce Canyon National Park, Utah. Bryce Canyon is known for its ampitheater full of hoodoos, or spires, are remanants of large sandstone fins that have been subjected to centuries of erosion.
    Bryce-Canyon_Rainbow-Point_Fall-Stor...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
  • An aspen tree displays its autumn colors on a ridge in Bryce Canyon National Park, Utah, as a heavy rainstorm approaches.
    Bryce-Canyon_Autumn-Rainstorm_0847.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
  • 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 few stars shine above Mitten Ridge, which is rendered in silhouette just before sunrise near Sedona, Arizona.
    AZ_MittenRidge_Dawn_Sedona_8908.jpg
  • Low clouds and fog rise from between the ridges in Bryce Canyon National Park, Utah.
    Bryce-Canyon_Lifting-Clouds_4165.jpg
  • A pinyon pine (Pinus edulis) tree frames this view of the full moon rising over Bryce Canyon National Park in Utah.
    BryceCanyon_PinyonPine_Moonrise_1064.jpg
  • Sycamore Creek, a tributary of the Verde River, flows through Sycamore Canyon near Williams, Arizona. Sycamore Canyon, which is 21 miles (34 kilometers) long, is the second largest canyon in Arizona's redrock country, behind only Oak Creek Canyon. This scene was captured from Sycamore Point.
    AZ_SycamoreCanyon_8793.jpg
  • A fall thunderstorm passes over Brins Mesa and other peaks west of Sedona, Arizona. This scene was captured from the summit of Doe Mountain.
    AZ_BrinsMesaStorm.jpg
  • A tiny hole in thick storm clouds allows the late afternoon sun to illuminate Bear Mountain while the other peaks near Sedona, Arizona remain in deep shade. This scene was captured from the summit of Doe Mountain.
    AZ_BearMountain.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 rainbow arcs over the Twin Buttes, a sandstone formation near Sedona, Arizona.
    TwinButtesAZRainbow.jpg
  • A layer of altocumulus clouds are turned fiery red by the setting sun as a large rock formation appears to observe in Capitol Reef National Park, Utah.
    Capitol-Reef_Rock-Sunset_1336.jpg
  • Viewed through heavy rain, fall color surrounds the sandstone rocks of the Bear Rocks Preserve in the Monongahela National Forest, West Virginia.
    WV_Bear-Rocks-Preserve_Autumn-Color_...jpg
  • Canyon Creek flows across the Indian Beach in Ecola State Park on the Oregon coast. Several sea stacks are visible in the Pacific Ocean including Submarine Rock (left) and Sea Lion Rock Arch (right).
    OR_Ecola_IndianBeach_Sunrise_0895.jpg
  • The last light of day illuminates the winter snow pack on Mount Rainier in this view from High Rock.
    rainier-winter-sunset.jpg
  • The dramatic golden light of sunset bathes the southwest face of Mount Rainier as the full moon rises over the Tatoosh Range in this panoramic view from the summit of High Rock.
    RainierMoonPanorama.jpg
  • Just before sunrise, clouds color the sky above Mount McDowell and the Salt River in the Granite Reef Recreational Area in the Tonto National Forest, Arizona. Mount McDowell is also known as Red Mountain or Fire Rock due to its dramatic glow at sunset.
    AZ-Tonto-NF_Granite-Reef_Sunrise_475...jpg
  • The Three Graces reach high into the sky in the Garden of the Gods in Colorado Springs, Colorado. The Three Graces are just one of many dramatic sandstone features of the park. According to geologists, the sedimentary rock was tilted by the forces that built nearby Pikes Peak and other mountains.
    CO_GardenGods_ThreeGraces_2320.jpg
  • A small starfish is on a rock that seems to glow when exposed to ultraviolet light at low tide on Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Starfish_Des-Moines_2059.jpg
  • The Three Graces reach high into the sky in the Garden of the Gods in Colorado Springs, Colorado. The Three Graces are just one of many dramatic sandstone features of the park. According to geologists, the sedimentary rock was tilted by the forces that built nearby Pikes Peak and other mountains.
    CO_GardenGods_ThreeGraces_1255.jpg
  • The bottom portion of North Fork Falls forms a wide cascade as it flows over reddish rock into Coal Creek in Bellevue, Washington.
    Coal-Creek_North-Fork-Falls_Cascades...jpg
  • A long exposure blurs the action of Puget Sound waves as they crash around the beach rocks at Mukilteo, Washington at sunset.
    MukilteoBeach_Rocks_Waves_LongExposu...jpg
  • A band of cirrus clouds take on pastel colors at sunset in the sky over Mount Larrabee and the Boulder Peaks in the North Cascades of Washington state. Mount Larrabee, which stands 7,865 feet (2,397 meters) is part of the Skagit Range, which is a sub-range of the North Cascades. It is located less than a mile and a half south of the Canadian border and was originally known as Red Mountain. During the summer months, its red peak, caused by the oxidation of iron in its rock, is distinct.
    North-Cascades_Mount-Larrabee_Pastel...jpg
  • The badlands of the Petrified Forest National Park, Arizona, are turned red by the setting sun. Badlands are a type of dry terrain where clay or soft sedimentary rock have been heavily eroded by rain and wind and where vegetation is scarce.
    AZ_Petrified-Forest_Badlands_Sunset_...jpg
  • Dozens of iron concretions are found on a bluff in the Grand staircase Escalante in southern Utah. These iron concretions formed naturally between 6 and 25 million years ago as water dissolved the iron pigment in the red sandstone in the area. The pigment flowed down through the now bleached sandstone and then solidified when it came in contact with oxygenated water, forming a new iron mineral called hematite between the grains of sandstone. Over time, the sandstone eroded away, leaving the more durable iron concretions behind. These largely spherical balls are composed of a hard outer layer of hematite covering a ball of pink sandstone. By volume, the sandstone makes up the majority of these iron concretions, though those found elsewhere in the Colorado Plateau may contain much more hematite. Scientists aren't sure why they form in spheres or if they need something in particular as a nucleus to start growing.
    IronConcretions_HarrisWashUtah_4183.jpg
  • Altocumulus clouds, turned red by the setting sun, streak over badlands near the Blue Mesa in Petrified Forest National Park, Arizona. Badlands are a type of dry terrain where clay or soft sedimentary rock have been heavily eroded by rain and wind and where vegetation is scarce.
    AZ_Petrified-Forest_Badlands_Sunset_...jpg
  • Dozens of iron concretions are trapped in a sandstone pothole in the Grand Staircase Escalante in southern Utah. These iron concretions formed naturally between 6 and 25 million years ago as water dissolved the iron pigment in the red sandstone in the area. The pigment flowed down through the now bleached sandstone and then solidified when it came in contact with oxygenated water, forming a new iron mineral called hematite between the grains of sandstone. Over time, the sandstone eroded away, leaving the more durable iron concretions behind. These largely spherical balls are composed of a hard outer layer of hematite covering a ball of pink sandstone. By volume, the sandstone makes up the majority of these iron concretions, though those found elsewhere in the Colorado Plateau may contain much more hematite. Scientists aren't sure why they form in spheres or if they need something in particular as a nucleus to start growing.
    IronConcretions_Pothole_HarrisWashUt...jpg
  • Dozens of iron concretions are trapped in a small crack in the Grand staircase Escalante in southern Utah. These iron concretions formed naturally between 6 and 25 million years ago as water dissolved the iron pigment in the red sandstone in the area. The pigment flowed down through the now bleached sandstone and then solidified when it came in contact with oxygenated water, forming a new iron mineral called hematite between the grains of sandstone. Over time, the sandstone eroded away, leaving the more durable iron concretions behind. These largely spherical balls are composed of a hard outer layer of hematite covering a ball of pink sandstone. By volume, the sandstone makes up the majority of these iron concretions, though those found elsewhere in the Colorado Plateau may contain much more hematite. Scientists aren't sure why they form in spheres or if they need something in particular as a nucleus to start growing.
    IronConcretions_HarrisWashUtah_4194.jpg
  • Iron concretions are found on a bluff in the Grand staircase Escalante in southern Utah. These iron concretions formed naturally between 6 and 25 million years ago as water dissolved the iron pigment in the red sandstone in the area. The pigment flowed down through the now bleached sandstone and then solidified when it came in contact with oxygenated water, forming a new iron mineral called hematite between the grains of sandstone. Over time, the sandstone eroded away, leaving the more durable iron concretions behind. These largely spherical balls are composed of a hard outer layer of hematite covering a ball of pink sandstone. By volume, the sandstone makes up the majority of these iron concretions, though those found elsewhere in the Colorado Plateau may contain much more hematite. Scientists aren't sure why they form in spheres or if they need something in particular as a nucleus to start growing.
    IronConcretions_HarrisWashUtah_4193.jpg
  • Dozens of iron concretions are trapped in cracks in the Grand staircase Escalante in southern Utah. These iron concretions formed naturally between 6 and 25 million years ago as water dissolved the iron pigment in the red sandstone in the area. The pigment flowed down through the now bleached sandstone and then solidified when it came in contact with oxygenated water, forming a new iron mineral called hematite between the grains of sandstone. Over time, the sandstone eroded away, leaving the more durable iron concretions behind. These largely spherical balls are composed of a hard outer layer of hematite covering a ball of pink sandstone. By volume, the sandstone makes up the majority of these iron concretions, though those found elsewhere in the Colorado Plateau may contain much more hematite. Scientists aren't sure why they form in spheres or if they need something in particular as a nucleus to start growing.
    IronConcretions_HarrisWashUtah_4202.jpg
  • Red clouds lit by the sunrise seem to swarm from the fossilized sand dunes known as the Beehives in the Valley of Fire State Park, Nevada. The dunes were formed by a proccess known as aeolian erosion.
    vof-beehives.jpg
  • A heart cockle (Clinocardium nuttallii) and kelp both appear to glow red when under ultraviolet light at low tide at the edge of Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Low-Tide_Heart-Cockle_Des...jpg
  • Against a backdrop of fiery clouds illuminated by the rising sun, two burrowing owls (Athene cunicularia) look out from their perches among the rocks in Grant County, Washington.
    Owls-Burrowing_Two_Sunrise_Ephrata_0...jpg
  • A variety of colorful spring flowers bloom among the large rocks in the bluffs of Malibu, California.
    Malibu_Big-Rocks_Wildflowers_4105.jpg
  • Against a backdrop of fiery clouds illuminated by the rising sun, two burrowing owls (Athene cunicularia) look out from their perches among the rocks in Grant County, Washington.
    Owls-Burrowing_Two_Sunrise_Ephrata_0...jpg
  • Puget Sound and the rocky beach at Mukilteo catch the last light of day as the sun sets behind Whidbey Island, Washington. A long exposure blurs the movement of the waves on Puget Sound.
    MukilteoBeach_WideView_Twilight_1188.jpg
  • A large sea stack is partially reflected in the sand at Ecola State Park, near Cannon Beach, Oregon.
    SeastackReflectionEcola1.jpg
  • Bright molten lava flows into the Pacific Ocean at twilight at Volcanoes National Park, Hawaii. The hot lava vaporizes the crashing waves, which reflect the lava's glow. The lava arrived at the ocean through an underground lava tube connected to the Pu'u O'o vent.
    LavaPacificOcean.jpg
  • Plant and animal life in a tide pool glows under ultraviolet light at the edge of Puget Sound in Des Moines, Washington. The glow is the result of phosphors that convert ultraviolet radiation, which is invisible to human eyes, into wavelengths that are visible. This scene was captured under black light.
    BlackLight_Low-Tide_Pool_Des-Moines_...jpg
  • SipapuBridgeH.jpg
  • Several tufa columns are turned golden by the rising sun at Mono Lake, California. Tufa forms only underwater. When calcium-rich springs flow up through the lake bottom, the calcium bonds to the carbonates in the lake water, forming calcium carbonate, a type of limestone. The solid material builds on itself, gradually forming a tufa tower. The tufa towers form only underwater; they were exposed when the lake was drained to provide drinking water for cities. After environmental groups took legal action, less water is being diverted for cities and the lake is slowly refilling.
    CA_MonoLake_Tufas_Golden_9336.jpg
  • SipapuBridgeV.jpg
  • An ohia lehua tree (Metrosideros polymorpha) provides rare color on a lava field in Volcanoes National Park, Hawaii. Ohio lehua are the most abundant native trees in Hawaii and are among the first life in new lava flows. According to Hawaiian legend, the tree is actually a young warrior. Pele, the goddess of fire, wanted to marry the warrior. When he refused, she turned him into a tree. The other gods weren't able to turn him back, so they turned his true love into the lehua blossom so they could be reunited. It's said that if you pick one of the blossoms, it will rain - the tears of lovers.
    HI_Volcanoes_OhiaLehua_Blossom_8493.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
  • A rainbow rises from a carpet of fall color as a heavy rainstorm passes over the Bear Rocks in the Dolly Sods Wilderness, West Virginia.
    WV_Dolly-Sods_Bear-Rocks_Rainbow_434...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
  • 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
  • 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
  • The sunrise colors the sky above the Kilauea Caldera and Mauna Loa in this view from Volcanoes National Park, Hawaii. Mauna Loa, one of the most active volcanoes on Earth, is also the largest, standing about 56,000 feet from its summit to its base on the ocean floor. (It stands 13,680 above sea level.) Mauna Loa means "long mountain." The steaming cliffs are visible at the caldera rim. Rain falls into cracks and is then turned into steam by the hot rocks below the surface.
    Volcanoes_Kilauea-Caldera_8636.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
  • Water boils out of a small spring on the Birds Nest Terrace in the Waimangu Volcanic Rift Valley near Rotorua, New Zealand. The terrace is part of a hydrothermal system in 1886 by the volcanic eruption of Mount Tarawera. Waimangu means 'black water' in Māori, the indigenous language of New Zealand. The area was given that name because its largest geyser erupted water that was filled with mud and rocks.
    NZ_Waimangu_BirdsNestTerrace_9002.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
  • 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
  • Asay Creek cuts an S-shaped curve through the snow-covered winter landscape in South Central Utah. The cliffs of Red Rock Canyon are visible in the background.
    AsayCreekUtahWinter.jpg
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