Show Navigation

Search Results

Refine Search
Match all words
Match any word
Prints
Personal Use
Royalty-Free
Rights-Managed
(leave unchecked to
search all images)
{ 17 images found }

Loading ()...

  • 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
  • Rock outcroppings provide a vantage point to take in a sweeping view of the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_MinisterValley_Overlook...jpg
  • Moss, ferns, and trees grow from a large rock outcropping near the Minister Valley in Allegheny National Forest in Warren, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Outcropping_Roots_8656.jpg
  • Moss, ferns, and trees grow from a large rock outcropping near the Minister Valley in Allegheny National Forest in Warren, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Outcropping_Roots_8652.jpg
  • Several evergreen wood ferns (Dryopteris intermedia) grow on a mossy rock outcropping near the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Fern_Rock_8643.jpg
  • Several evergreen wood ferns (Dryopteris intermedia) grow on a mossy rock outcropping near the Minister Valley in the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Fern_Rock_8642.jpg
  • The sun shines between a tree and a large rock outcropping in the Minister Valley area of the Allegheny National Forest in Warren County, Pennsylvania. The Allegheny Front was once part of a vast delta and layers of a hard, sandstone congolomerate were deposited. Between 250 and 320 million years ago, the Allegheny Front was lifted, forming hills and mountains. Over time, erosion exposed, split, or dislodged and moved the former sedimentary rock, resulting in large rock outcroppings.
    PA_Allegheny_Minister_Outcropping_86...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
  • 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
  • Tree roots spread out and nearly cover the face of a rock outcropping near Minister Valley in the Allegheny National Forest, Warren County, Pennsylvania.
    PA_Allegheny_Outcropping_TreeRoots_8...jpg
  • Tree roots spread out and nearly cover the face of a rock outcropping near Minister Valley in the Allegheny National Forest, Warren County, Pennsylvania.
    PA_Allegheny_Outcropping_TreeRoots_8...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
  • 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
  • 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
  • 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
  • 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