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  • A solo hiker walks atop the Pulpit Rock (Prekestolen) 1959 feet above a car ferry on Lysefjord, Forsand municipality, Rogaland county, Ryfylke traditional district, Norway, Europe. The nearest city is Jørpeland, in Strand municipality. Published in Wilderness Travel Catalog of Adventures 1998, 1996, 1988. Winner of "Honorable Mention, Photo Travel Division" in Photographic Society of America (PSA) Inter-Club Slide Competition May 1988. Published 2009 on a commercial web site in Amsterdam. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    81NOR-08-14-The-Pulpit_Prekestolen.jpg
  • 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.
    1503SW-0068_Golden-Throne.jpg
  • 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.
    1503SW-0059_Golden-Throne.jpg
  • The granite monolith of El Capitan rises 3000 feet (900 m) above Yosemite Valley floor to 7569 feet elevation in Yosemite National Park, California, USA. Rock climbers flock from around the world test themselves on the huge granitic face. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, El Capitan and the entire Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 2 overlapping photos.
    1111CAL-031-32pan_El-Capitan_El-Capi...jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-185.jpg
  • The granite monolith of El Capitan reflects in Merced River at Valley View. El Capitan rises 3000 feet (900 m) above Yosemite Valley floor to 7569 feet elevation in Yosemite National Park, California, USA. Rock climbers flock from around the world test themselves on the huge granitic face. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, El Capitan and the entire Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 4 overlapping photos.
    1111CAL-606-609pan_Yosemite-Valley.jpg
  • The granite monolith of El Capitan reflects in Merced River at Valley View. El Capitan rises 3000 feet (900 m) above Yosemite Valley floor to 7569 feet elevation in Yosemite National Park, California, USA. Rock climbers flock from around the world test themselves on the huge granitic face. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, El Capitan and the entire Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 6 overlapping photos.
    1111CAL-596-601pan_Yosemite-Valley.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-676.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-169.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service. Panorama stitched from 2 overlapping images.
    08ORC-157-158pan_Cannon-Beach.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    08ORC-097.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-054.jpg
  • The granite monolith of El Capitan rises 3000 feet (900 m) above Yosemite Valley floor to 7569 feet elevation in Yosemite National Park, California, USA. See Bridalveil Falls from Tunnel View, just east of Wawona Tunnel on State Route 41. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, El Capitan and the entire Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-117_El-Capitan_Yosemite.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-198.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-180.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service. Panorama stitched from 2 overlapping images.
    08ORC-174-175pan_Cannon-Beach.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-110.jpg
  • 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.
    1503SW-0055_Golden-Throne.jpg
  • 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
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-662.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-197.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-191.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-187.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service. Panorama stitched from 2 overlapping images.
    08ORC-119-120pan_Cannon-Beach.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-073.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-048.jpg
  • The pounding Pacific Ocean has eroded a bluff to create Haystack Rock, a 235-foot (72-meter) tall monolith (or sea stack), on Cannon Beach, on the Oregon coast. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-018.jpg
  • 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.
    1503SW-0038_Golden-Throne.jpg
  • 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.
    1503SW-0035_Golden-Throne.jpg
  • The granite monolith of El Capitan reflects in Merced River at Valley View. El Capitan rises 3000 feet (900 m) above Yosemite Valley floor to 7569 feet elevation in Yosemite National Park, California, USA. Rock climbers flock from around the world test themselves on the huge granitic face. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, El Capitan and the entire Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 6 overlapping photos.
    1111CAL-109-114pan_Yosemite-Valley.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    08ORC-189.jpg
  • The pounding Pacific Ocean has eroded bluffs to create Haystack Rock, a 235-foot (72-meter) tall monolith and many other sea stacks, on Cannon Beach, on the Oregon coast, at Ecola State Park. Haystack Rock is part of the Tolovana Beach State Recreation Site and is managed by Oregon Parks and Recreation below the mean high water (MHW) level, and above the MHW level by the Oregon Islands National Wildlife Refuge of the United States Fish and Wildlife Service.
    06OR_206.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet) rises above Lower Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked from Green River Lakes trailhead to Slide Lake (13 miles round trip with 2100 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River). This image was stitched from multiple overlapping photos.
    1909US1-0331-332-Pano.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet elevation) rises above Upper Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked a lollipop loop around Lower Green River Lake including the side trip to Upper Green River Lake (totalling 7.2 miles with 700 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River).
    1909US1-0104.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet) rises above Lower Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked from Green River Lakes trailhead to Slide Lake (13 miles round trip with 2100 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River).
    1909US1-0240.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet) rises above Lower Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked from Green River Lakes trailhead to Slide Lake (13 miles round trip with 2100 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River).
    1909US1-0254.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet elevation) rises above Lower Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked a lollipop loop around Lower Green River Lake including the side trip to Upper Green River Lake (totaling 7.2 miles with 700 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River).
    1909US1-0215.jpg
  • The granite monolith of Squaretop Mountain (11,695 feet elevation) rises above Lower Green River Lake, in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We hiked a lollipop loop around Lower Green River Lake including the side trip to Upper Green River Lake (totaling 7.2 miles with 700 feet gain). The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River). This image was stitched from multiple overlapping photos.
    1909US1-0123-Pano.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20290_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20248_Remarkable-Rocks.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-394_Half-Dome_Yosemite.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20270_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20257_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20253_Remarkable-Rocks.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) reflects in Mirror Lake, Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 6 overlapping photos.
    1111CAL-355-362pan_Half-Dome.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) rises above Mirror Lake, Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 6 overlapping photos.
    1111CAL-345_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-303_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-302_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 3 overlapping photos.
    1111CAL-229-231pan_Half-Dome.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-005_Half-Dome_Yosemite.jpg
  • A stone monolith and cemetery headstones rise at Heddal stave church, Norway's largest stave church. This triple nave stave church, which some call "a Gothic cathedral in wood," was built in the early 13th century and restored in 1849-1851 and the 1950s. Heddal stavkirke is in Notodden municipality, Telemark County, Norway.
    11NOR-1666.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20294_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20265_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds. Panorama stitched from 2 overlapping images.
    04AUS-20263-264pan_Remarkable-Rocks.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) reflects in Mirror Lake, Tenaya Creek, Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CALC-101_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-397_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-377_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-178_Half-Dome_Yosemite.jpg
  • One of the largest masses of granite in the Eastern United States, Looking Glass Rock is excellent for rock climbing and gets its name from the shimmering effects of sunlight on its surface when wet. This "pluton monolith" crystallized from magma .slowly cooling below the surface. .Fall leaves color the Blue Ridge Mountains (a subset of the Appalachian Mountains) at Log Hollow Overlook (elevation 4445 feet) at Milepost 416.0 of the Blue Ridge Parkway, in North Carolina. Local trees release hydrocarbons into the atmosphere and create a characteristic blue haze. The Blue Ridge Parkway is a 469-mile (755 km) long scenic highway that connects Shenandoah National Park, Virginia, with the Great Smoky Mountains National Park in North Carolina, following ridge crestlines and the Appalachian Trail. Panorama stitched from 3 overlapping photos.
    08NC-2435-2437pan_Looking-Glass-Rock.jpg
  • One of the largest masses of granite in the Eastern United States, Looking Glass Rock is excellent for rock climbing and gets its name from the shimmering effects of sunlight on its surface when wet. This "pluton monolith" crystallized from magma .slowly cooling below the surface. .Fall leaves color the Blue Ridge Mountains (a subset of the Appalachian Mountains) at Log Hollow Overlook (elevation 4445 feet) at Milepost 416.0 of the Blue Ridge Parkway, in North Carolina. Local trees release hydrocarbons into the atmosphere and create a characteristic blue haze. The Blue Ridge Parkway is a 469-mile (755 km) long scenic highway that connects Shenandoah National Park, Virginia, with the Great Smoky Mountains National Park in North Carolina, following ridge crestlines and the Appalachian Trail.
    08NC-2434.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20267_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20246_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-03-31_Remarkable-Rocks.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) reflects in Mirror Lake, Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 6 overlapping photos.
    1111CALC-104-109pan_Half-Dome_Yosemi...jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-320_Half-Dome_Yosemite.jpg
  • A stone monolith and cemetery headstones rise at Heddal stave church, Norway's largest stave church. This triple nave stave church, which some call "a Gothic cathedral in wood," was built in the early 13th century and restored in 1849-1851 and the 1950s. Heddal stavkirke is in Notodden municipality, Telemark County, Norway.
    11NOR-1658.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    04AUS-20288_Remarkable-Rocks.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-03-32_Remarkable-Rocks.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-256_Half-Dome_Yosemite.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite. Panorama stitched from 3 overlapping photos.
    1111CAL-232-234pan_Half-Dome.jpg
  • The granite monolith of Half Dome (8836 feet or 2693 meters elevation) is a famous symbol of Yosemite National Park, Sierra Nevada, California, USA. The peak rises 4737 ft (1444 m) above the valley floor. Designated a World Heritage Site by UNESCO in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity. 100 million years ago, the Sierra Nevada crystallized into granite from magma 5 miles underground. The range started uplifting 4 million years ago, and glaciers eroded the landscape seen today in Yosemite.
    1111CAL-176_Half-Dome_Yosemite.jpg
  • In Columbia Gorge National Scenic Area, see Pierce Island in Columbia River from Beacon Rock State Park, Washington, in the Pacific Northwest, USA. The Columbia River cuts its gorge over 80 miles (130 km) westwards through the Cascade Range, with mountain walls reaching 4000 feet high (1200 meters). The gorge begins near the Deschutes River confluence with the Columbia and extends to the eastern Portland metropolitan area. The canyon connects the Columbia River Plateau with the Pacific Ocean, providing the only navigable route through the Cascades and defining the border between Washington and Oregon. The federally protected Gorge is managed by the US Forest Service. Beacon Rock is a striking monolith composed of basalt, 848 feet high (258 meters). In 1805, Lewis and Clark originally referred to it as Beaten Rock, later as Beacon Rock. They found that Beacon Rock marked the eastern-most tidal influence in the Columbia. It was later known as Castle Rock until 1915 when its name changed back to Beacon Rock. The panorama was stitched from 17 overlapping images. Published by Columbia Land Trust, Fieldbook Early Fall 2013, www.columbialandtrust.org
    1003GOR-0015-31pan_Columbia_River.jpg
  • Beacon Rock, Columbia River Gorge National Scenic Area, Washington (seen from the Oregon side of the river), USA. Beacon Rock is a striking monolith composed of basalt, 848 feet high (258 meters). In 1805, Lewis and Clark originally referred to it as Beaten Rock, later as Beacon Rock. They found that Beacon Rock marked the eastern-most tidal influence in the Columbia. It was later known as Castle Rock until 1915 when its name changed back to Beacon Rock.
    10GOR-0119.jpg
  • Beacon Rock, Columbia River Gorge National Scenic Area, Washington (seen from the Oregon side of the river), USA. Beacon Rock is a striking monolith composed of basalt, 848 feet high (258 meters). In 1805, Lewis and Clark originally referred to it as Beaten Rock, later as Beacon Rock. They found that Beacon Rock marked the eastern-most tidal influence in the Columbia. It was later known as Castle Rock until 1915 when its name changed back to Beacon Rock.
    10GOR-0092.jpg
  • Pinetree Arch, Devils Garden Trail, 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.
    1909US1-8135.jpg
  • Sunrise sunburst 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.
    1909US1-8394-99-Pano.jpg
  • Double O 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 3 overlapping photos.
    1403UT-223-225pan_Double-O-Arch_Devi...jpg
  • Dark Angel is a red sandstone pinnacle on Devils Garden Trail, 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.
    1909US1-8117-18-Pano.jpg
  • Double O Arch, Devils Garden Trail, Arches National Park, Moab, Utah, USA. Double O Arch is the second largest arch within the Devils Garden area. Its larger arch spans 71 feet, stacked atop a 21-foot arch on the same sandstone fin. Double O Arch is 1.93 miles from the Devils Garden trailhead at the far end of the Devils Garden Primitive Loop. 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.
    1909US1-8062-73-Pano.jpg
  • Navajo Arch, Devils Garden Trail, 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.
    1909US1-6022.jpg
  • Partition Arch, Devils Garden Trail, 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.
    1909US1-6019.jpg
  • Sunrise light 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.
    1909US1-8348-61-Pano.jpg
  • Sunrise light 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.
    1909US1-8382-83-Pano.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.
    1909US1-8306.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.
    1909US1-8213.jpg
  • In Cirque of the Towers, Pingora Peak rises above Lonesome Lake at sunrise, seen from Jackass Pass, in Bridger Wilderness, Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We backpacked to Big Sandy Lake Campground (11 miles round trip with 1000 feet gain). Two hours before sunrise, I departed from Big Sandy Lake to reach Jackass Pass viewpoint for Cirque of the Towers and Lonesome Lake (6.5 miles round trip, 1860 ft gain) on the Continental Divide Trail. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. This image was stitched from multiple overlapping photos.
    1909US1-1301-Pano.jpg
  • Sunrise on Pingora Peak seen from Jackass Pass, Cirque of the Towers, Bridger Wilderness, Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We backpacked to Big Sandy Lake Campground (11 miles round trip with 1000 feet gain). Two hours before sunrise, I departed from Big Sandy Lake to reach Jackass Pass viewpoint for Cirque of the Towers and Lonesome Lake (6.5 miles round trip, 1860 ft gain) on the Continental Divide Trail. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys.
    1909US1-1071.jpg
  • Sunrise on Pingora Peak seen from Jackass Pass, Cirque of the Towers, Bridger Wilderness, Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. We backpacked to Big Sandy Lake Campground (11 miles round trip with 1000 feet gain). Two hours before sunrise, I departed from Big Sandy Lake to reach Jackass Pass viewpoint for Cirque of the Towers and Lonesome Lake (6.5 miles round trip, 1860 ft gain) on the Continental Divide Trail. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys.
    1909US1-1095.jpg
  • The sharp point of East Temple Peak rises above Deep Lake in  Bridger Wilderness. At left is the shoulder of Haystack Mountain. Backpack to Big Sandy Lake Campground (11 miles round trip with 1000 feet gain). Day hike from Big Sandy Lake to Clear Lake and Deep Lake below East Temple Peak then loop back via Temple Lake, Miller Lake, and Rapid Lake (7.5 miles, 1060 ft gain) on the Continental Divide Trail. Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. This image was stitched from multiple overlapping photos.
    1909US1-1002-Pano-2.jpg
  • Sunrise hits our tent at Big Sandy Lake Campground in Bridger Wilderness, Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA.  Backpack to Big Sandy Lake Campground (11 miles round trip with 1000 feet gain). Day hike from Big Sandy Lake to Clear Lake and Deep Lake below East Temple Peak then loop back via Temple Lake, Miller Lake, and Rapid Lake (7.5 miles, 1060 ft gain) on the Continental Divide Trail. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaci
    1909US1-0876.jpg
  • Wind River Range seen from Photographer's Point, Bridger-Teton NF, Rocky Mountains, Wyoming, USA. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys.
    1909US1-0401.jpg
  • Clear Creek Valley, seen along the hike from Green River Lakes to Slide Lake (13 miles round trip with 2100 feet gain) in the Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. The Continental Divide follows the crest of the "Winds". Mostly composed of granite batholiths formed deep within the earth over 1 billion years ago, the Wind River Range is one of the oldest mountain ranges in North America. These granite monoliths were uplifted, exposed by erosion, then carved by glaciers 500,000 years ago to form cirques and U-shaped valleys. Glaciers scoured the terminal moraine which naturally dams the Green River Lakes, the headwaters of the Green River (chief tributary to the Colorado River).
    1909US1-0263.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-0664.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-0654.jpg
  • Cliffs of the Colorado River seen to the southeast from 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-0531.jpg
  • Turret Arch 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-0521.jpg
  • See the back of Double Arch, from Cove of Caves in 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-0502-507-Pano.jpg
  • Cove Arch. Cove of Caves in 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-0446-449-Pano.jpg
  • Cove Arch, in Cove of Caves in the Windows Section of Arches National Park, Moab, Utah, USA. At left is the back of Double 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.
    1804SW-0395.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
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