Inge Johnsson Photography

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  • 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
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorseHoodoosSunset2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesGargoyle.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
  • Dead juniper in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesDeadBranch.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
  • Juniper tree and rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    NorthCoyoteButtesJuniper.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
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.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.
    WahweapSingleHoodoo2.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
  • TurtleBackRocks.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.
    _Y6A0520.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
  • 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.
    _Y6A0487.jpg
  • Asgaard pass route to the Enchantment Lakes in Washington with Colchuck Lake down below
    EnchantmentsFog2.jpg
  • Waterfall along Asgaard pass route to the Enchantment Lakes in Washington with Dragontail Peak in the background
    AsgaardWaterfall1.jpg
  • Ridges at John Day Fossil Beds Natiional Monument
    JohnDayFossilBeds7.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 White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketTree4.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunset2.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
    SouthCoyoteButtesFins3.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
    SouthCoyoteButtesFlakes.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave3.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
  • Striated sandstone at South Coyote Buttes, Arizona
    RainbowRocksStriations5.jpg
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.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
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • Slickrock ridges at White Pocket
    WhitePocketSunrise1.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketTree4.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    CoyoteSouthSunset1.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
    SouthCoyoteButtesSunset2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    Manzanita1.jpg
  • Sandstone "snail" against a sandstone wall in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSnail-2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSnail.jpg
  • Dead tree contrasted against a sandstone wall in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesDeadTree.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFins3.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 White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketAfterglow1.jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorseHoodoosSunrise1.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
    TopArch1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    WaveColorfulStripes2.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    BoneYard1.jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorsePointRocks5.jpg
  • Striated sandstone at South Coyote Buttes, Arizona
    RainbowRocksStriations5.jpg
  • Sandstone formations in bowl in the interior of Rainbow Rocks
    SandstoneAnvils.jpg
  • Dead bush at Rainbow Rocks, Arizona
    RainbowRocksDeadBush1.jpg
  • Fantastic colors and shapes in sandstone detail at South Coyote Buttes, Arizona
    RainbowRocksStriations3.jpg
  • Swirl in the sandstone at White Pocket, AZ
    WhitePocketsSwirl1.jpg
  • Colorful rock called "Lollipop Rock" at White Pocket, Arizona
    WhitePocketLollipop1.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.
    WahweapSky1.jpg
  • Rock formations that look somewhat like men with triangular hats near Page, Arizona
    StudhorsePointRocks4.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendWider (Drumscan).jpg
  • "The Wave" formation in the North Coyote Buttes BLM unit
    TheWaveAndClouds.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.
    _Y6A0525.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.
    MetateArch1.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.
    _Y6A0497-HDR.jpg
  • Sandstone "snail" against a sandstone wall in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSnail.jpg
  • Hoodoo "garden" in the Grand Staircase-Escalante National Monument
    RimrocksHoodoos1.jpg
  • Den Tilsandede Kirke church in Denmark near Skagen
    SkagenTilsandedeKirke2.jpg
  • Asgaard pass route to the Enchantment Lakes in Washington with Colchuck Lake down below
    EnchantmentsFog1.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.
    WahweapSky1.jpg
  • TurtleBackRocks.jpg
  • Rock formations that look somewhat like men with triangular hats near Page, Arizona
    StudhorsePointRocks4.jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorsePointRocks2.jpg
  • PsychadelicRock1.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendWider.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendWider (Drumscan).jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorsePointRocks5.jpg
  • Asgaard pass route to the Enchantment Lakes in Washington with Colchuck Lake down below
    EnchantmentsFog1.jpg
  • Waterfall along Asgaard pass route to the Enchantment Lakes in Washington with Dragontail Peak in the background
    EnchantmentsAsgaardPassCascade.jpg
  • Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon
    JohnDayFossilBeds9.jpg
  • JohnDayFossilBeds6.jpg
  • Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon
    JohnDayFossilBeds5.jpg
  • Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon
    JohnDayFossilBeds1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    BoneYard1.jpg
  • Den Tilsandede Kirke church in Denmark near Skagen
    SkagenTilsandedeKirke1.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorseHoodoosSunset2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesGargoyle.jpg
  • Slickrock ridges at White Pocket
    WhitePocketSunrise1.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
    CoyoteSouthSunset1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesBranch1.jpg
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