Inge Johnsson Photography

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  • Forest at Sol Duc Falls in Olympic National Park, Washington
    SolDucEnchantedForest3.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierTipsoo9.jpg
  • Barn outside Mount Rainier National Park with the peak of the mountain looming behind it
    MountRainierBarn.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesGargoyle.jpg
  • Swirl in the sandstone at White Pocket, AZ
    WhitePocketsSwirl1.jpg
  • Abstract patterns in Lower Antelope Canyon, Page, Arizona
    AntelopeAbstractCurve1.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise2.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo2.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeSandstonePatterns2.jpg
  • Reflection in the Colorado River at Lava Falls, in the Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    _MG_9398.jpg
  • Prickly Pear cactus at the mouth of Havasu Canyon, Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCactus.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    _MG_9325.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot1.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon2.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park with barrel cacti in foreground
    NankoweapCactus.jpg
  • Rafts at dawn on the Colorado River in the interior of the Grand Canyon
    GrandCanyonDawnRafts1.jpg
  • Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona–Utah border, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163.<br />
<br />
Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, "its five square miles have defined what decades of moviegoers think of when they imagine the American West
    MonumentValleyStagecoach1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierHallwayTrees1.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonHavasuCreekPool2.jpg
  • The Colorado River from Cardenas in the interior of the canyon
    GrandCanyonCardenas1.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • East face of Mount Rainier with Upper Tipsoo Lake in foreground
    MtRainierTipsoo4.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0489.jpg
  • Ruin on a hilltop at Cardenas Creek in the interior of the Grand Canyon
    GrandCanyonHilltop1.jpg
  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado3.jpg
  • Sightseeing helicopter in the Namib-Naukluft National Park in Namibia.<br />
<br />
Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiHelicopter1.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei13.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierChristineFallsWinter3.jpg
  • SummerlandBacklitTrees1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierReflectionTrees2.jpg
  • Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.
    MysteryValleyRock1.jpg
  • First light over Monument Valley from atop Hunts Mesa
    HuntsMesaPano1.jpg
  • Dead tree on Hunt's Mesa in Monument Valley, AZ
    MonumentValleyHuntsMesaDeadTree1.jpg
  • Sand Springs in Monument Valley, shadow of nearby tree
    MonumentValleySandSprings1.jpg
  • Mount Rainier in the winter, seen from the south side
    MtRainierInspiration.jpg
  • East face of Mount Rainier with Upper Tipsoo Lake in foreground
    MtRainierTipsoo4.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierTatooshTrees2.jpg
  • Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon
    JohnDayFossilBeds9.jpg
  • Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon
    JohnDayFossilBeds3.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona ..... Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona, in the United States. Horseshoe Bend is located 5 miles downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles southwest of Page. It is accessible via hiking a 1.5-mile round trip from U.S. Route 89, but an access road also reaches the geological structure, as it is part of a state park. Horseshoe Bend can be viewed from the steep cliff above. The overlook is 4,200 feet (1,300 m) above sea level, and the Colorado River is at 3,200 feet (980 m) above sea level, making it a 1,000-foot (300 m) drop
    HorseshoeBendSunrise1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesBranch1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFins3.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave3.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    TopRockHamburger1.jpg
  • Classic view of the Mittens and Merrick Butte in Monument Valley, AZ
    MonumentValleyMittens1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierChristineFallsWinter3.jpg
  • Winter at Mount Rainier National Park administration building at Longmire, Washington
    MountRainierWinterHouse.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketJuniperScenic.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunset1.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketCandyland.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    TopRockHamburger3.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA
    SnoqualmieFallsRiverWinter2-HDR.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove2.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierTipsoo7.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierNationalParkInn1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierNationalParkInn2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierSnowshoers2.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierTipsoo7.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketLoneJuniper.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesDeadJuniper1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFinRoom1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesLongFin.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunrise1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFlakes.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave3.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave6.jpg
  • Rocks in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    BoneYard3.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    TopRockHamburger1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    WaveBowl1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    WaveColorfulStripes2.jpg
  • The Vermilion Cliffs are the second "step" up in the five-step Grand Staircase of the Colorado Plateau. Reddish or vermilion-colored cliffs are found along U.S. Highway 89 and U.S. Highway 89A near Kanab, Utah (and near Navajo Bridge in Arizona). 112,500 acres (45,500 ha) of the region were designated as the Paria Canyon-Vermilion Cliffs Wilderness in 1984, and an even greater area was proclaimed Vermilion Cliffs National Monument in 2000. Famous locations in the cliff area include Lee's Ferry, Glen Canyon (a national recreational area), The Wave, Coyote Buttes, and others.
    ClingingToEarth.jpg
  • Striated sandstone at South Coyote Buttes, Arizona
    RainbowRocksStriations5.jpg
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.jpg
  • Canyon wall in Buckskin Gulch, Paria Canyon Wilderness. The Buckskin Gulch, a canyon in southern Utah, is one of the main tributaries of the Paria River, which is itself a minor tributary of the Colorado River. It is the longest and deepest slot canyon in the southwest United States and may very well be the longest in the world. As such it is one of the premier destinations for slot canyon hikers, and receives a high amount of foot traffic.<br />
At over 13 miles (21 km) in length it is often visited in conjunction with the longer Paria Canyon, although some prefer to make a long day trip out of the hike. With a distance of 20 miles (32 km), hiking this canyon in one day is possible. Wire Pass, a short tributary to the Buckskin, is an ideal alternative for a short day hike that still takes hikers through the narrow, curving features that are the hallmark of slot canyons
    BuckskinRoughSea.jpg
  • Cracked earth and bushes in Valley of the Gods, Utah
    ValleyOfTheGods2.jpg
  • Classic view of the Mittens and Merrick Butte in Monument Valley, AZ
    MonumentValleyMittens1.jpg
  • Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.
    MysteryValleyPancake1.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCreek2.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot3.jpg
  • Blacktail Canyon, a side canyon to the Grand Canyon.
    GrandCanyonBlacktail2.jpg
  • Small waterfall on Clear Creek, a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonClearCreek1.jpg
  • The Colorado River from Cardenas in the interior of the canyon in the interior of the canyon
    GrandCanyonCardenas4.jpg
  • Ruin on a hilltop at Cardenas Creek in the interior of the Grand Canyon
    GrandCanyonCardenasHilltopRuin3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon2.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Reflection in the Colorado River at the side canyon called National Canyon
    GrandCanyonNationalReflection1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapHoodoos2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSky3.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeRidge2a.jpg
  • Ray of light coming down from the top of the narrow Upper Antelope Canyon
    AntelopeCanyonBeamOfLight.jpg
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