Show Navigation
American Southwest All Galleries
Add to Cart Download

Utah Landscapes

9 images Created 24 Aug 2014

From dramatic hoodoos of Bryce Canyon to the world's greatest concentration of natural sandstone arches and bridges, Utah features some of the most stunning scenery in the world.

Loading ()...

  • The full moon sets over the Bryce Canyon amphitheater at sunrise. The Earth's shadow and a red band, known as the Belt of Venus, are visible just above the horizon. Bryce Canyon is a national park in Utah.
    BryceCanyonMoon.jpg
  • Hundreds of hoodoos that make up the Bryce Canyon amphitheater are lit at sunrise. Bryce Canyon is national park in Utah. The hoodoos, or spires, are remanants of large sandstone fins that have been subjected to centuries of erosion.
    BryceCanyonAmphitheaterTight.jpg
  • Storm clouds gather over the multi-colored Elkheart Cliffs, located near Mt. Carmel Junction, Utah.
    UT_ElkheartCliffs_StormClouds_0298.jpg
  • Mudcracks in a variety of shapes and sizes are visible in the sediment at the base of Harris Wash in Utah. Mudcracks, also known as desiccation cracks, result when the top layer of sediment dries before lower layers. When the water in the top layer evaporates, the thin layer separates from the layers below. The loss of moisture also causes the layer to shrink somewhat, causing a strain that results in the cracks.
    UT_Mudcracks_HarrisWash_4278.jpg
  • The towering Coral Pink Sand Dunes near Kanab, Utah, are made up of orangish-pink sand, remnants of the Wingate and Kayenta sandstone that forms the Vermilion Cliffs to the southeast.
    CoralPinkSandDunes.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
  • A small sandstone window frames a view of a narrow slot canyon in the Coyote Wash area of Grand Staircase National Monument in Utah. Flash floods carved narrow canyons in the sandstone.
    Grand-Staircase-Escalante_Coyote-Gul...jpg
  • Several small rocks lie at the base of a dry waterfall, which was carved by flash floods in the Coyote Gulch area of the Grand Staircase Escalante, Utah.
    CoyoteGulchDryFall.jpg
  • SipapuBridgeH.jpg
View: 100 | All
  • Facebook
  • Twitter
x

Living Wilderness Nature Photography

  • Nature Photography Galleries
    • All Galleries
    • Search
    • Cart
    • Lightbox
    • Client Area
  • Portfolio
  • Search Nature Photography
  • Books
  • Blog
  • About
  • Contact