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  • Sunrise light shines on the red-orange sandstone of Skyline Arch at Devils Garden Campground, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8362.jpg
  • Sunset shines on the red-orange sandstone of Skyline Arch at Devils Garden Campground, Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8275-99-Pano.jpg
  • Sunset shines on the red-orange sandstone of Skyline Arch at Devils Garden Campground, Arches National Park, Moab, Utah, USA. Three visitors climb up and stand in the arch. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8304.jpg
  • Sunset shines on red sandstone rock formations at Devils Garden Campground, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8262.jpg
  • Delicate Arch and La Sal Mountains, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0676.jpg
  • Delicate Arch, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0663.jpg
  • Ute Rock Art (1650-1850), on the trail to Delicate Arch, Wolfe Ranch, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0621.jpg
  • Cove of Caves in the Windows Section of Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0377-392-Pano.jpg
  • North & South Window Arches. Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0517.jpg
  • The back of Double Arch, seen from Cove of Caves in Windows Section of Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0394.jpg
  • Turret Arch and La Sal Mountains. The Windows Section of Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0348.jpg
  • Turret Arch and La Sal Mountains. The Windows Section of Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0292.jpg
  • Rock pattern in Moonflower Canyon on BLM land, Moab Kane Creek Blvd, Utah, USA. The BLM (Bureau of Land Management) is part of the United States Department of the Interior.
    1804SW-0268.jpg
  • Tower Arch, in Klondike Bluffs, in Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos.
    1804SW-0218-226-Pano.jpg
  • Tower Arch, in Klondike Bluffs, in Arches National Park, Moab, Utah, USA.
    1804SW-0216.jpg
  • Tower Arch, in Klondike Bluffs, in Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos.
    1804SW-0175-181-Pano.jpg
  • Indian Paintbrush (Castilleja) flowers bloom red along Hunter Canyon hiking trail, on BLM land, Moab, Utah, USA. Castilleja is a genus of about 200 species of annual and perennial herbaceous plants native to the west of the Americas plus northeast Asia. These plants are classified in the family Orobanchaceae and are hemiparasitic on the roots of grasses and forbs. The BLM (Bureau of Land Management) is part of the United States Department of the Interior.
    1804SW-0076.jpg
  • Purple flower, Negro Bill Canyon, on BLM federal land near Moab, Utah, USA.
    1403UT-367.jpg
  • Green and purple-tinged prickly pear cactus / Opuntia genus forms a thorny pattern. Hike Negro Bill Canyon, on BLM federal land near Moab, Utah, USA.
    1403UT-360.jpg
  • Corona Arch Trail, on BLM federal land near Moab, Utah, USA. Hike 3 miles round trip up Bootlegger Canyon to the half-freestanding Corona Arch, also called Little Rainbow Bridge, which has an impressive opening of 140 feet wide by 105 feet high. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-273_Corona-Arch.jpg
  • The sun backlights Corona Arch, on BLM federal land near Moab, Utah, USA. Hike 3 miles round trip up Bootlegger Canyon to the half-freestanding Corona Arch, also called Little Rainbow Bridge, which has an impressive opening of 140 feet wide by 105 feet high. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-256_Corona-Arch.jpg
  • A stream flows in Negro Bill Canyon, on BLM federal land near Moab, Utah, USA. The Navajo Sandstone of Morning Glory Natural Bridge spans 243 feet, making it the sixth largest rock span in the United States.
    1403UT-442_Negro-Bill-Canyon.jpg
  • Partition Arch, Devils Garden Trail, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-182_Partition-Arch_Utah.jpg
  • Partition Arch, Devils Garden Trail, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation. This panorama was stitched from 2 overlapping photos.
    1403UT-173-174pan_Partition-Arch_Uta...jpg
  • Landscape Arch, on Devils Garden Trail, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation. This panorama was stitched from 6 overlapping photos.
    1403UT-162-167pan_Landscape-Arch_Uta...jpg
  • Partition Arch hikers, Devils Garden Trail, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation. This panorama was stitched from 2 overlapping photos.
    1403UT-169-170pan_Partition-Arch_Uta...jpg
  • Near Devils Garden Campground, in Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-141_Arches-NP_Utah.jpg
  • Broken Arch is a walk of 1.3 miles round trip from Devils Garden Campground, in Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-123-p4_Broken-Arch_Utah.jpg
  • Broken Arch is a walk of 1.3 miles round trip from Devils Garden Campground, in Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation. This panorama was stitched from 7 overlapping photos.
    1403UT-112-118pan_Broken-Arch_Utah.jpg
  • Twisted tree silhouette and red rock shadows, in Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-102_Arches-NP_Utah.jpg
  • Red rock shadows, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-098_Arches-NP_Utah.jpg
  • Devils Garden Trail, Entrada sandstone rock formations, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-232_Devils-Garden-fins.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-032_Fisher-Towers_Utah.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-030_Fisher-Towers_Utah.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-019_Fisher-Towers_Utah.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands. The panorama was stitched from 4 overlapping photos.
    1403UT-015-18pan_Fisher-Towers_Utah.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-007_Fisher-Towers_Utah.jpg
  • Sandstone wall pattern, Corona Arch Trail, on BLM federal land near Moab, Utah, USA. Hike 3 miles round trip up Bootlegger Canyon to the half-freestanding Corona Arch, also called Little Rainbow Bridge, which has an impressive opening of 140 feet wide by 105 feet high. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403SWC-083_sandstone-pattern_Utah.jpg
  • Intrepid Potash Inc. mines potash with a water dissolution and evaporation process at Cane Creek Facility, near Moab, Utah, USA. (Photo taken from a viewpoint on Island in the Sky in Canyonlands National Park, Utah, USA.) Water from the nearby Colorado River is pumped through injection wells into the underground mine. The water dissolves the potash from layers buried 3,000 feet underground. The mineral-laden water (brine) is piped to 400 acres of shallow ponds where the water evaporates, aided by 300 days of sunshine and very low humidity, leaving potash (potassium chloride) and salt (sodium chloride) crystals. A blue dye, similar to food coloring, is added to assist evaporation (saving the burning 400,000 tons of coal each year). The solar ponds are lined with heavy vinyl to prevent brine from leaking into the ground and the Colorado River. Holding ponds catch any spills and return potassium-rich brine to the ponds. The snow-dusted La Sal Mountains reach 12,780 feet in elevation.
    06UT_2209.jpg
  • Sunset shines on the red-orange sandstone of Skyline Arch at Devils Garden Campground, Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8179-80-Pano.jpg
  • Sunset shines on the red-orange sandstone of Skyline Arch at Devils Garden Campground, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1909US1-8178.jpg
  • Moonrise at sunset at Devils Garden Campground, Arches National Park, Moab, Utah, USA.
    1909US1-8323.jpg
  • Sunset silhouettes a dead tree near Devils Garden Campground, Arches National Park, Moab, Utah, USA.
    1909US1-8311.jpg
  • Delicate Arch and La Sal Mountains, Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0689.jpg
  • Upheaval Dome. Island in the Sky District of Canyonlands National Park, Moab, USA.
    1804SW-0590.jpg
  • A balanced rock in the Garden of Eden, in the Windows Section of Arches National Park, Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1804SW-0297.jpg
  • La Sal Mountains. Arches National Park, Moab, Utah, USA.
    1804SW-0241.jpg
  • Tower Arch, in Klondike Bluffs, in Arches National Park, Moab, Utah, USA. This image was stitched from multiple overlapping photos.
    1804SW-0196-203-Pano.jpg
  • La Sal Mountains rise behind the Marching Men, along Tower Arch Trail to Klondike Bluffs, in Arches National Park, Moab, Utah, USA.
    1804SW2-028.jpg
  • Balanced Rock and La Sal Mountains. Arches National Park, Moab, Utah, USA.
    1804SW-0153-p1.jpg
  • Corona Arch Trail is spectacular, on BLM federal land near Moab, Utah, USA. Hike 3 miles round trip up Bootlegger Canyon to the half-freestanding Corona Arch, also called Little Rainbow Bridge, which has an impressive opening of 140 feet wide by 105 feet high. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands. This panorama was stitched from 3 overlapping photos.
    1403UT-286-88pan_Corona-Arch.jpg
  • Corona Arch Trail, on BLM federal land near Moab, Utah, USA. Hike 3 miles round trip up Bootlegger Canyon to the half-freestanding Corona Arch, also called Little Rainbow Bridge, which has an impressive opening of 140 feet wide by 105 feet high. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-248_Corona-Arch.jpg
  • Hike Negro Bill Canyon to Morning Glory Bridge, on BLM federal land near Moab, Utah, USA. The Navajo Sandstone of Morning Glory Natural Bridge spans 243 feet, making it the sixth largest rock span in the United States. This panorama was stitched from 6 overlapping photos.
    1403UT-416-21pan_Morning-Glory-Bridg...jpg
  • Partition Arch, Devils Garden Trail, Arches National Park, near Moab, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    1403UT-193_Partition-Arch_Utah.jpg
  • A climber rappels from a hoodoo. The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-060_Fisher-Towers_Utah.jpg
  • The impressive Fisher Towers are eroded from Cutler sandstone capped with Moenkopi sandstone, on BLM federal land near Moab, Utah, USA. Hike the Fisher Towers Trail 4.5 miles round trip with 800 feet gain. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1403UT-029_Fisher-Towers_Utah.jpg
  • Sandstone pinnacles catch sunset light in Arches National Park, Utah, USA.
    06UT_2269_Arches-NP-Utah.jpg
  • From Orange Cliffs Overlook in Canyonlands National Park (Utah, USA), view the Green River in Stillwater Canyon, with the snowy Henry Mountains in the distance. (Panorama stitched from 2 photos.)
    06UT_2203-2204pan_Orange-Cliffs-Over...jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah. Published in "Light Travel: Photography on the Go" by Tom Dempsey 2009, 2010. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3078-Double_Arch.jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3075-Double_Arch.jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3070-Double_Arch.jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3068-Double_Arch.jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3064-Double_Arch.jpg
  • South and North Windows are comprised of the Slick Rock member of Entrada Sandstone on top of the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member, in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset.
    06UT_3017-South+North-Windows.jpg
  • Turret Arch is comprised of the Slick Rock member of Entrada Sandstone on top of the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member, in Arches National Park, Utah, USA.
    06UT_3013-Turret-Arch.jpg
  • Turret Arch is comprised of the Slick Rock member of Entrada Sandstone on top of the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member, in Arches National Park, Utah, USA.
    06UT_3011-Turret-Arch.jpg
  • The Three Gossips erode from the Slick Rock member of Entrada Sandstone in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset.
    06UT_3007-Courthouse-Towers.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. At left are the Three Gossips. The Courthouse Towers are comprised of the Slick Rock member of Entrada Sandstone above the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member. (Panorama stitched from 3 photos.)
    06UT_2287-2289pan_Courthouse-Towers.jpg
  • Skyline Arch eroded within the Slick Rock member of Entrada Sandstone in Arches National Park, Utah, USA
    06UT_2266-Skyline-Arch.jpg
  • Sunset light glows orange on roadside sandstone mesas, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA.
    06UT_2251_Arches-NP-Utah.jpg
  • The La Sal Mountains rise behind arches, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA. The park road curves through fascinating sandstone scenes.
    06UT_2228_Arches-NP-Utah.jpg
  • The La Sal Mountains rise behind arches, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA. (Panorama stitched from 5 photos.)
    06UT_2217-2221pan_Windows-Section-Ar...jpg
  • Mesa Arch frames buttes back lit by sunrise at Canyonlands National Park, Utah, USA.
    06UT_2191_Mesa-Arch_Canyonlands-NP.jpg
  • Mesa Arch glows at sunrise in Canyonlands National Park, Utah in 2006. Panorama stitched from five images. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    06UT_2137-2141pan_Mesa-Arch_Canyonla...jpg
  • Mesa Arch frames buttes in Canyonlands National Park, Utah, USA.
    06UT_2123_Mesa-Arch_Canyonlands-NP.jpg
  • Balanced Rock glows at dusk in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone. The snow-dusted La Sal Mountains reach 12,780 feet in elevation.
    06UT_2098_Arches-NP.jpg
  • Balanced Rock catches golden rays of sunset in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone. The snow-dusted La Sal Mountains reach 12,780 feet in elevation.
    06UT_2090_Arches-NP.jpg
  • Balanced Rock catches golden rays of sunset in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) mounts a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone. The snow-dusted La Sal Mountains reach 12,780 feet in elevation, formed as a result of intrusion of igneous rocks and subsequent erosion of the surrounding less-resistant sedimentary rocks.
    06UT_2075_Arches-NP.jpg
  • Balanced Rock catches golden rays of sunset in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone. The snow-dusted La Sal Mountains reach 12,780 feet in elevation. (Panorama stitched from 2 photos.)
    06UT_2073-2074pan_Arches-NP.jpg
  • Twisted tree branches reach towards Balanced Rock in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone.
    06UT_2057_Arches-NP.jpg
  • Twisted tree branches reach towards Balanced Rock in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone.
    06UT_2056_Arches-NP.jpg
  • Balanced Rock juts 128 feet/39 meters above the desert floor in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone.
    06UT_2053_Arches-NP.jpg
  • Balanced Rock juts 128 feet/39 meters above the desert floor in Arches National Park, Utah, USA. The Entrada Sandstone at Balanced Rock (128 feet/39 meters high) balances a caprock of the hard Slick Rock Member upon a base of the Dewey Bridge Member, a mudstone.
    06UT_2052_Arches-NP.jpg
  • Entrada Sandstone erodes into towers and buttes in Arches National Park, Utah, USA.
    06UT_2041_Arches-NP.jpg
  • Double Arch erodes from Entrada Sandstone in Arches National Park, Utah, USA. A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3072-Double_Arch.jpg
  • North Window arch frames the Windows Section of Arches National Park, Utah, USA. North Window is comprised of the Slick Rock member of Entrada Sandstone on top of the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member. (Panorama was stitched from 10 images.) A thick underground salt bed underlies the creation of the park's many arches, spires, balanced rocks, sandstone fins, and eroded monoliths. Some 300 million years ago, a sea flowed into the area and eventually evaporated to create the salt bed up to thousands of feet thick. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 million years ago) desert conditions deposited the vast Navajo Sandstone. On top of that, about 140 million years ago, the Entrada Sandstone was deposited from stream and windblown sediments. Later, over 5000 feet (1500 m) of younger sediments were deposited and then mostly worn away, leaving the park's arches eroded mostly within the Entrada formation.
    06UT_3045-3054pan_North-Window.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. The Courthouse Towers are comprised of the Slick Rock member of Entrada Sandstone above the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member. A Volkswagon Eurovan Camper parks at a pullout.
    06UT_3008-Courthouse-Towers.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. A Volkswagon Eurovan Camper parks at a pullout. Published in "Light Travel: Photography on the Go" by Tom Dempsey 2009, 2010.
    06UT_3006-Courthouse-Towers.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. The Courthouse Towers are comprised of the Slick Rock member of Entrada Sandstone above the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member.
    06UT_3005-Courthouse-Towers.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. The Courthouse Towers are comprised of the Slick Rock member of Entrada Sandstone above the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member.
    06UT_3004-Courthouse-Towers.jpg
  • The orange sandstone Courthouse Towers resist erosion in Arches National Park, Utah, USA. These rock monuments are beautiful both at sunrise (seen here) and sunset. The Courthouse Towers are comprised of the Slick Rock member of Entrada Sandstone above the red-brown. or chocolate-brown marker beds of the Dewey .Bridge member. At left are the Three Gossips.
    06UT_2281-Courthouse-Towers.jpg
  • Skyline Arch eroded within the Slick Rock member of Entrada Sandstone in Arches National Park, Utah, USA. Fractal branching of a twisted dead tree frames the arch. Published in "Light Travel: Photography on the Go" by Tom Dempsey 2009, 2010.
    06UT_2264-Skyline-Arch.jpg
  • Skyline Arch eroded within the Slick Rock member of Entrada Sandstone in Arches National Park, Utah, USA
    06UT_2257-Skyline-Arch.jpg
  • Sunset light glows orange on roadside sandstone mesas, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA.
    06UT_2256_Arches-NP-Utah.jpg
  • Sunset light glows orange on sandstone mesas, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA. a Volkswagon Eurovan Camper stops at a roadside turnout.
    06UT_2252_Arches-NP-Utah.jpg
  • The La Sal Mountains rise behind arches, buttes, and pinnacles of the Windows Section of Arches National Park, Utah, USA. (Panorama stitched from 4 photos.)
    06UT_2230-33pan_Windows-Section-Arch...jpg
  • Dead Horse Point State Park provides a dramatic overlook of the Colorado River and mesas and cliffs of Canyonlands National Park, in Utah, USA. The area was used in the final scene of the 1991 film "Thelma & Louise."
    06UT_2213-Dead-Horse-Point-SP.jpg
  • The White Rim Road winds across a shelf in Canyonlands National Park, as seen from Grand View Point Overlook on Island in the Sky, above Colorado River canyons, in Utah, USA. (Panorama stitched from 3 photos.)
    06UT_2194-2196pan_Grand-View-Point-O...jpg
  • Mesa Arch frames buttes back lit by sunrise at Canyonlands National Park, Utah, USA.
    06UT_2192_Mesa-Arch_Canyonlands-NP.jpg
  • Mesa Arch bounces golden light at sunrise in Canyonlands National Park, Utah, USA.
    06UT_2184_Mesa-Arch_Canyonlands-NP.jpg
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