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  • 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
  • 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
  • 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
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_CloseUp_3145.jpg
  • This panorama shows the colorful layers that give the Painted Hills in the John Day National Monument in Oregon their name. The layers represent different ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_Panorama_3098.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. Eventually the layers were thrust upward and tilted by movement of the Earth's plates. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_WideView_3192.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. Eventually the layers were thrust upward and tilted by movement of the Earth's plates. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_Palette_3240.jpg
  • Low-angle sunlight shows the texture of the colorful Painted Hills in the John Day National Monument in Oregon. The layers represent different ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_DeepShadow_3175.jpg
  • The Painted Hills in John Day National Monument, Oregon are comprised of several layers of ash and pumice deposits from the Cascades and area volcanoes. The deposits were laid down approximately 33 million years ago. The red comes from rusty iron minerals; golden layers are rich with oxidized magnesium and iron, metamorphic claystone; the black comes from manganese.
    OR_PaintedHills_CloseUp_3185.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
  • 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
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