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2015 Mar 3-Apr 8: favorites UT, CO hikes

54 images Created 30 Mar 2018

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  • Golden Throne is a sandstone monolith from the Jurassic geologic period. Start this hike from Capitol Gorge Trailhead, in Capitol Reef National Park, Utah, USA. This panorama was stitched from 2 overlapping photos.
    1503SW3-016-17pan_Golden-Throne.jpg
  • Sunset in Capitol Gorge, Capitol Reef National Park, Utah, USA. Capitol Gorge was the original route for travelers through Waterpocket Fold before State Route 24 cut along Fremont River.
    1503SW-0204_Capitol-Gorge_Utah.jpg
  • The majestic Hickman Natural Bridge has a span of 133 feet. The hike is 1.8 miles round trip with 400 feet gain in Capitol Reef National Park, Utah, USA. This panorama was stitched from 6 overlapping photos.
    1503SW-0264-69pan_Hickman-Natural-Br...jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0282_Navajo-sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0288_Navajo-sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0290_Navajo-sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0364_Navajo-sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0375_Navajo-sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0379_Navajo-sandstone-pattern.jpg
  • Admire fanciful hoodoos, mushroom shapes, and rock pinnacles in Goblin Valley State Park, in Emery County between the towns of Green River and Hanksville, in central Utah, USA. The Goblin rocks eroded from Entrada Sandstone, which is comprised of alternating layers of sandstone (cross-bedded by former tides), siltstone, and shale debris which were eroded from former highlands and redeposited in beds on a former tidal flat. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of rock (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes.
    1503SW-0553_Goblin-Valley.jpg
  • A boy in yellow shirt runs through a panorama of hoodoos in Goblin Valley State Park, in central Utah, USA. Admire fanciful hoodoos, mushroom shapes, and rock pinnacles in fascinating Goblin Valley State Park, in Emery County between the towns of Green River and Hanksville. The Goblin rocks eroded from Entrada Sandstone, which is comprised of alternating layers of sandstone (cross-bedded by former tides), siltstone, and shale debris which were eroded from former highlands and redeposited in beds on a former tidal flat. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of rock (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. This panorama was stitched from 3 overlapping photos.
    1503SW-0580-82pan_Goblin-Valley.jpg
  • Sunrise in the Campground at Goblin Valley State Park, San Rafael Swell, Utah, USA. Admire fanciful hoodoos, mushroom shapes, and rock pinnacles in Goblin Valley State Park, in Emery County between the towns of Green River and Hanksville, in central Utah. The Goblin rocks eroded from Entrada Sandstone, which is comprised of alternating layers of sandstone (cross-bedded by former tides), siltstone, and shale debris which were eroded from former highlands and redeposited in beds on a former tidal flat.
    1503SW-0605_Goblin-Valley.jpg
  • Sandstone erodes into honeycomb depressions in Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands. Honeycomb weathering: rainwater soaks into sandstone, dissolves its cement, and redeposits it near the surface as the water evaporates, forming a resistant outer layer, pockmarked with holes into the soft inner layers enlarged by wind and moisture.
    1503SW-0619_Crack-Canyon_pattern.jpg
  • A white salt crust forms an abstract pattern over orange-red sandstone in Crack Canyon, in San Rafael Swell, near Goblin Valley State Park, Utah, USA.
    1503SW3-055_Crack-Canyon_pattern.jpg
  • A hiker explores beautiful Crack Canyon on public federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. Honeycomb weathering: rainwater soaks into sandstone, dissolves its cement, and redeposits it near the surface as the water evaporates, forming a resistant outer layer, pockmarked with holes into the soft inner layers enlarged by wind and moisture. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0638_Crack-Canyon_pattern.jpg
  • A limb of driftwood lodges high in the slot of Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0675_slot-driftwood_Crack-Can...jpg
  • A pattern of red and yellow sandstone swirls in Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW3-090_Crack-Canyon_pattern.jpg
  • Intricate honeycombs of weathered sandstone decorate Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. Honeycomb weathering: rainwater soaks into sandstone, dissolves its cement, and redeposits it near the surface as the water evaporates, forming a resistant outer layer, pockmarked with holes into the soft inner layers enlarged by wind and moisture. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW3-091_Crack-Canyon_pattern.jpg
  • Intricate honeycombs of weathered sandstone decorate Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. Honeycomb weathering: rainwater soaks into sandstone, dissolves its cement, and redeposits it near the surface as the water evaporates, forming a resistant outer layer, pockmarked with holes into the soft inner layers enlarged by wind and moisture. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW3-107_Crack-Canyon_pattern.jpg
  • Explore the cool honeycombed-sandstone slot of Crack Canyon in San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0717_Crack-Canyon_pattern.jpg
  • Explore the cool honeycombed-sandstone slot of Crack Canyon in San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0727_Crack-Canyon_pattern.jpg
  • A hiker explores the beautiful slot of Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0730_Crack-Canyon_pattern.jpg
  • Find fascinating Jurassic sandstone rock patterns in Wild Horse  Canyon on federal BLM land in the San Rafael Swell (160-175 million years old), Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0738_Jurassic-sandstone-patte...jpg
  • Find fascinating Jurassic sandstone rock patterns in Wild Horse Canyon on federal BLM land in the San Rafael Swell (160-175 million years old), Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0739_Jurassic-sandstone-patte...jpg
  • Find fascinating Jurassic sandstone rock patterns in Wild Horse Canyon on federal BLM land in the San Rafael Swell (160-175 million years old), Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0748_Jurassic-sandstone-patte...jpg
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