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  • Ponderosa pine trees (Pinus ponderosa) cast shadows on the floor of the Blue Mountain Forest, part of the Wallowa-Whitman National Forest in Oregon.
    OR_Blue-Mountain-Forest_Shadows_8086.jpg
  • Ponderosa pine trees (Pinus ponderosa) cast shadows on the floor of the Blue Mountain Forest, part of the Wallowa-Whitman National Forest in Oregon.
    OR_Blue-Mountain-Forest_Shadows_8086...jpg
  • An Allen's Chipmunk (Tamias senex) — and its shadow — feeds in the Sequoia National Forest near Kings Canyon National Park, California. Allen's Chipmunks, also known as Large Mountain Chipmunks or Shadow Chipmunks, are found from the coast to the mountains, though only the mountain chipmunks hibernate in the winter. Allen's Chipmunks primarily feed on fungi.
    Chipmunk_Allens_Shadow_8041.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 western bluebird (Sialia mexicana) takes flight from its perch in the Blue Mountain Forest, part of the Wallowa-Whitman National Forest in Oregon.
    Bluebird-Western_Blue-Mountains_Oreg...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 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
  • 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
  • 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
  • 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_5105.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
  • A pair of hemlock trees frame a view of Olallie Lake and the forest that surrounds it in the Mount Baker-Snoqualmie National Forest in Washington state.
    WA_Olallie-Lake_Forest_Framed_5798.jpg
  • The opening of the Hidden Forest Cave frames a stand of tall ponderosa pine trees in Deschutes National Forest, Oregon.
    Hidden-Forest-Cave_Oregon_2560.jpg
  • A mustang (Equus caballus) walks under a canopy of mesquite trees in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustang_Forest_Coon-Bluff_4040.jpg
  • Spring wildflowers, mainly desert sand verbena (Abronia villosa), grow in the sandy soil at the base of mesquite snags in the Tonto National Forest near the Coon Bluff Recreation Area in Arizona.
    AZ-Tonto-NF_Coon-Bluff_Wildflowers_4...jpg
  • An Arizona woodpecker (Dryobates arizonae) climbs a juniper tree in the Coronado National Forest in southern Arizona. While it contains "Arizona" in its name, its range is mainly limited to Mexico's Sierra Madre and barely extends into the state. The small woodpecker forages by climbing trees, spiraling around the trunk from bottom to top.
    Woodpecker-Arizona_Coronado-AZ_8440.jpg
  • Mustangs (Equus caballus) gather on a gravel bar in the Salt River in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5673.jpg
  • Mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Feeding_Coon-Bluff_4507.jpg
  • A pair of mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_347...jpg
  • Sliding Rock, a waterfall in the Pisgah National Forest in North Carolina, gently slides about 60 feet (18 meters) over smooth rock. During the summer months, Sliding Rock is a popular tourist attraction with people who use the waterfall as a water slide.
    NC_Sliding-Rock_1371.jpg
  • A desert cottontail (Sylvilagus audubonii) rests rocks near the Salt River in the Tonto National Forest in Arizona. The desert cottontail is also known as Audubon's cottontail.
    Cottontail-Desert_Tonto-NF_4788.jpg
  • Mustangs (Equus caballus) feed in along the edge of the Salt River as the sun sets in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_4638.jpg
  • A mustang (Equus caballus) gets up after giving itself a dirt bath in the Tonto National Forest near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustang_Dirt-Bath_Coon-Bluff_4138.jpg
  • Three mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Feeding_Coon-Bluff_3655.jpg
  • A pair of mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_347...jpg
  • A pair of mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_349...jpg
  • Mustangs (Equus caballus) gather on a gravel bar in the Salt River in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5375.jpg
  • A Pyrrhuloxia (Cardinalis sinuatus) rests on a branch in Ash Canyon in the Coronado National Forest, Arizona.
    Pyrrhuloxia_Ash-Canyon_Arizona_1271.jpg
  • Three shafts of sunlight illuminate Skylight Cave in the Deschutes National Forest in Oregon. Skylight Cave is a lava tube and light enters through three skylights. Two of the skylights are hornito skylights, formed where lava was ejected through the crust of a flow some distance from the source of the magma.
    Skylight-Cave_Three-Beams_2761.jpg
  • Light filters into a lava tube known as Skylight Cave in Deschutes National Forest in Oregon, revealing the texture of its walls.
    Skylight-Cave_Texture_2686.jpg
  • Three shafts of sunlight illuminate Skylight Cave in the Deschutes National Forest in Oregon. Skylight Cave is a lava tube and light enters through three skylights. Two of the skylights are hornito skylights, formed where lava was ejected through the crust of a flow some distance from the source of the magma.
    Skylight-Cave_Three-Beams_2749.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
  • An Arizona woodpecker (Dryobates arizonae) climbs a juniper tree in the Coronado National Forest in southern Arizona. While it contains "Arizona" in its name, its range is mainly limited to Mexico's Sierra Madre and barely extends into the state. The small woodpecker forages by climbing trees, spiraling around the trunk from bottom to top.
    Woodpecker-Arizona_Coronado-AZ_8445.jpg
  • Mustangs (Equus caballus) gather on a gravel bar in the Salt River in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5612.jpg
  • Mustangs (Equus caballus) gather on a gravel bar in the Salt River in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5520.jpg
  • A pair of mustangs (Equus caballus) feeds in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_372...jpg
  • A Pyrrhuloxia (Cardinalis sinuatus) rests on a branch in Ash Canyon in the Coronado National Forest, Arizona.
    Pyrrhuloxia_Ash-Canyon_Arizona_0892.jpg
  • A Pyrrhuloxia (Cardinalis sinuatus) rests on a branch in Ash Canyon in the Coronado National Forest, Arizona.
    Pyrrhuloxia_Ash-Canyon_Arizona_1550.jpg
  • Three shafts of sunlight illuminate Skylight Cave in the Deschutes National Forest in Oregon. Skylight Cave is a lava tube and light enters through three skylights. Two of the skylights are hornito skylights, formed where lava was ejected through the crust of a flow some distance from the source of the magma.
    Skylight-Cave_Three-Beams_2771.jpg
  • Three shafts of sunlight illuminate Skylight Cave in the Deschutes National Forest in Oregon. Skylight Cave is a lava tube and light enters through three skylights. Two of the skylights are hornito skylights, formed where lava was ejected through the crust of a flow some distance from the source of the magma.
    Skylight-Cave_Three-Beams_2740.jpg
  • A crack runs through rhyolite lava in the Inyo National Forest near Mammoth Mountain, California. The crack is part of a feature known as the Mammoth Earthquake Fault, but it's technically an earthquake fissure, resulting from an earthquake that occurred before 1850.
    CA_Mammoth_Earthquake-Fissure_0880.jpg
  • A Pyrrhuloxia (Cardinalis sinuatus) rests on a branch in Ash Canyon in the Coronado National Forest, Arizona.
    Pyrrhuloxia_Ash-Canyon_Arizona_1217.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
  • Mustangs (Equus caballus) gather on a gravel bar in the Salt River in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5683.jpg
  • Two mustangs (Equus caballus) touch muzzles in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Touching-Muzzles_Coon-Bluff...jpg
  • A pair of mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_351...jpg
  • A pair of mustangs (Equus caballus) feed in the Tonto National Forest in the woods near the Salt River in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Pair_Feeding_Coon-Bluff_350...jpg
  • Two mustangs (Equus caballus) cross the Salt River as the sun rises in the Tonto National Forest in Arizona. The free-roaming mustangs are commonly referred to as wild horses, but they are descendants of domesticated Spanish horses that were brought to the continent in the 16th century.
    Mustangs_Salt-River_Arizona_5228pano.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
  • A Wilson's warbler (Cardellina pusilla) bathes in a small pool of water in Cooper Canyon in the Coronado National Forest, Arizona.
    Warbler-Wilsons_Bathing_Coronado-AZ_...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
  • Steam fog seems to erupt from a small pool on an island within Sparks Lake in the Deschutes National Forest near Bend, Oregon. The island is covered with yellow spear-leaf arnica (Arnica longifolia) flowers in mid-summer. Broken Top Mountain rises in the back left of the image. Broken Top, which stands 9,177 feet (2,797 meters) tall, is a stratovolcano that last erupted about 100,000 years ago and has since been eroded by glaciers.
    OR_Sparks-Lake_Broken-Top_Wildflower...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
  • A cluster of icicles forms over a creek in the Cinnabar Basin in the Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Icicle-Patterns_85...jpg
  • In winter, Cinnabar Creek is mostly covered in snow and ice as it flows in the valley of the Cinnabar Basin in the Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Cinnabar-Creek_Fro...jpg
  • In winter, Cinnabar Creek is mostly covered in snow and ice as it flows in the valley of the Cinnabar Basin in teh Gallatin National Forest near Gardiner, Montana.
    MT_Cinnabar-Basin_Cinnabar-Creek_Fro...jpg
  • Fall color surrounds a seasonal waterfall that drops from Granite Mountain in the Mount Baker-Snoqualmie National Forest near Snoqualmie Pass, Washington.
    Snoqualmie-Pass_Denny-Creek_Fall-Col...jpg
  • Two snowy egrets (Egretta thula) fly low over the Salt River in the Tonto National Forest, Arizona.
    Egrets-Snowy_Salt-River_Reflections_...jpg
  • Fiery red ground cover carpets the Rohrbaugh Plains in fall color, located in the Dolly Sods Wilderness in the Monongahela National Forest, West Virginia.
    WV_Dolly-Sods_Rohrbaugh-Plains_Autum...jpg
  • Snags rise above the frozen surface of Earthquake Lake in the Gallatin National Forest in Montana. The lake, located west of Yellowstone, was formed in 1959 after a magnitude 7.3 earthquake triggered an 80-million ton landslide, damming the Madison River. The snags here are trees that perished when their roots were flooded.
    MT_Earthquake-Lake_Snags_Winter_2805.jpg
  • A snowy egret (Egretta thula) flies low over the Salt River in the Tonto National Forest, Arizona.
    Egret-Snowy_Salt-River_Reflection_48...jpg
  • Badlands formations known as the Tepees in Petrified Forest National Park, Arizona, are turned golden red near sunset. Tepees, also spelled tipi or teepee, is a tent that is traditionally made of animal skins over wooden poles. While humans have lived for 13,000 years in and around the modern day Petrified Forest National Park, the native dwellings were more commonly pithouses and pueblos.
    AZ_Petrified-Forest_Tepees_Sunset_64...jpg
  • A cross-section of petrified wood displays a wide spectrum of colors in the Rainbow Forest of Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_D...jpg
  • Altocumulus clouds, turned pink by the setting sun, fill the sky over badlands formations known as the Tepees in Petrified Forest National Park, Arizona. Tepees, also spelled tipi or teepee, is a tent that is traditionally made of animal skins over wooden poles. While humans have lived for 13,000 years in and around the modern day Petrified Forest National Park, the native dwellings were more commonly pithouses and pueblos.
    AZ_Petrified-Forest_Tepees_Sunset_64...jpg
  • A close-up of a a cross-section of petrified wood reveals colors in abstract patterns in the Petrified Forest National Park in Arizona. The petrified wood in the park is made up of almost solid quartz and the colors are the result of impurities in the quartz, such as iron, carbon and manganese. It formed more than 200 million years ago when logs washed into an ancient river system. The logs were quickly buried by sediment, which slowed decay. Over time, minerals, including silica, were absorbed into the porous wood, replacing the original organic material over hundreds of thousands of years.
    AZ_Petrified-Forest_Petrified-Wood_A...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
  • Colorful layers of siltstone, mudstone and shale are visible in the badlands near the Blue Mesa in Petrified Forest National Park, Arizona. The layers contain iron and manganese, which provide the pigments for the brilliant and varied colors.
    AZ_Petrified-Forest_Badlands_Painted...jpg
  • Moss drapes from the thick brances of old-growth bigleaf maple trees (Acer macrophyllum) that are beginning to show their fall colors in the Hall of Mosses, part of the Hoh Rain Forest in Olympic National Park, Washington. The Hoh Rain Forest is a temperate forest, receiving between 140 and 170 inches (355 to 432 centimeters) of rain per year. The lush forest has been named by UNESCO as both a World Heritage Site and a Biosphere Reserve.
    Hoh-Rain-Forest_Hall-Of-Mosses_Autum...jpg
  • Backlit clubmoss contrasts with the vibrant fall colors of the leaves on a bigleaf maple (Acer macrophyllum) tree in the Hoh Rain Forest in Olympic National Park, Washington. These trees are in the Hall of Mosses, an old-growth section of the forest.
    Hoh-Rain-Forest_Maple-Leaves_Clubmos...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
  • The canopy of a riverine forest near the Mara River in the Maasai Mara National Reserve in Kenya is visible in this aerial view captured from a hot air balloon.
    Kenya_Maasai-Mara_Riverine-Forest_Ae...jpg
  • The canopy of a riverine forest near the Mara River in the Maasai Mara National Reserve in Kenya is visible in this aerial view captured from a hot air balloon.
    Kenya_Maasai-Mara_Riverine-Forest_Ae...jpg
  • The Mara River bends around a riverine forest in this aerial view over the Maasai Mara National Reserve in Kenya.
    Kenya_Maasai-Mara_Mara-River_Forest_...jpg
  • The Mara River bends through a riverine forest in this aerial view over the Maasai Mara National Reserve in Kenya.
    Kenya_Maasai-Mara_Mara-River_Forest_...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
  • Comet C/2020 F3 (NEOWISE) shines bright over a forested ridge in Mount Rainier National Park, Washington. 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.
    Comet_Neowise_C2020F3_Forest-Ridge_8...jpg
  • A strip of Mount Hornaday is visible between snow clouds and trees coated in fresh snow in Yellowstone National Park, Wyoming. Mount Hornaday is a 10,003-foot (3,049-meter) mountain that is part of the Absaroka Range.
    Yellowstone_Mount-Hornaday_Snow-Stor...jpg
  • A mountain gorilla (Gorilla beringei beringei) sits to rest in the forest of Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Sitting_6800.jpg
  • A young mountain gorilla (Gorilla beringei beringei) caresses the face of its mother in the rain forest of the Volcanoes National Park in Rwanda. The gorillas are members of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorillas_Mother_Chil...jpg
  • A mountain gorilla (Gorilla beringei beringei) feeds on leaves in the rain forest of Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Feeding_6086.jpg
  • A young mountain gorilla (Gorilla beringei beringei) caresses the face of its mother in the rain forest of the Volcanoes National Park in Rwanda. The gorillas are members of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorillas_Mother_Chil...jpg
  • A Great Blue Heron (Ardea herodias) sits at the top of a snag in the Hoh Rain Forest in Washington's Olympic National Park.
    Olympics_Heron_Snag_9833.jpg
  • A mountain gorilla (Gorilla beringei beringei) closes its eyes to rest in the rain forest of Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Resting_6181.jpg
  • A mountain gorilla (Gorilla beringei beringei) rests in Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Resting_Clos...jpg
  • A mountain gorilla (Gorilla beringei beringei) feeds on leaves in the rainforest of Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Feeding_Mist...jpg
  • A mountain gorilla (Gorilla beringei beringei) bites down on a small leaf in Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Feeding_6338.jpg
  • A mountain gorilla (Gorilla beringei beringei) is almost completely obscured by thick vegetation as he sits in the rainforest of Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Vegetation_7...jpg
  • A bright rainbow stretches across a forested valley in Egmont National Park located in the Taranaki District on the North Island of New Zealand.
    NZ_EgmontNP_Rainbow_0999.jpg
  • A mountain gorilla (Gorilla beringei beringei) feeds on leaves in the rainforest of Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Vegetation_8...jpg
  • A mountain gorilla (Gorilla beringei beringei) sets admist wet vegetation as rain falls in Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Sitting_Mist...jpg
  • A mountain gorilla (Gorilla beringei beringei) sets admist wet vegetation as rain falls in Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Feeding_Mist...jpg
  • Red leaves at the peak of their fall color stand out against the ash-colored trunks in the forest in Acadia National Park, Maine.
    Acadia_Fall-Color_0899.jpg
  • A mountain gorilla (Gorilla beringei beringei) feeds on leaves in Volcanoes National Park in Rwanda. The gorilla is a member of the Kwitonda group, which means "humble one" in Kinyarwanda, the national language of Rwanda. The Kwitonda group migrated from the Democratic Republic of Congo and now inhabits the lower slopes of Mount Muhabura in Rwanda.
    Rwanda_Mountain-Gorilla_Feeding_6065.jpg
  • A mountain gorilla (Gorilla beringei beringei) sets admist wet vegetation as rain falls in Volcanoes National Park in Rwanda. This gorilla is a member of the Umubano group, which means "living together" in Kinyarwanda, the national language of Rwanda.
    Rwanda_Mountain-Gorilla_Vegetation_8...jpg
  • A large Douglas fir (Pseudotsuga menziesii) stands in contrast to the snow-dusted forest at a slightly higher elevation in the early autumn in the Lamar Valley of Yellowstone National Park, Wyoming.
    Yellowstone_Douglas-Fir_Boulders_Lam...jpg
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