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55 images Created 14 Oct 2011

View Tom Dempsey's favorite Wyoming photographs: Grand Teton National Park mountain peaks reflected in the Snake River; Yellowstone National Park hot springs; and Devils Tower National Monument fall colors.

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  • The barn at John Moulton Homestead, at the corner of Mormon Row and Antelope Flats Road, in the valley of Jackson Hole, Grand Teton National Park, Wyoming, USA.
    1909US1-0508.jpg
  • Mountain peaks reflect in the Snake River at Schwabacher Landing at sunrise, Grand Teton National Park, Wyoming, USA
    04WY-0400.jpg
  • Palette Spring, Mammoth Hot Springs. Yellowstone National Park, Wyoming, USA.
    1709US1-4617_Yellowstone-NP-WY.jpg
  • Sunset at Big Sandy Lake in Bridger Wilderness, in the Wind River Range. 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.
    1909US1-0815-Pano.jpg
  • Aspen yellow fall colors in Devils Tower National Monument. Bear Lodge Mountains, Black Hills, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    1709US1-3377-p1_Devils-Tower-WY.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 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
  • Devils Tower National Monument. Bear Lodge Mountains, Black Hills, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt. This image was stitched from multiple overlapping photos.
    1709US1-3417-19-Pano-Edit_Devils-Tow...jpg
  • Colorful microbial mats coat terraces of Grand Prismatic Spring in Midway Geyser Basin, Yellowstone National Park, Wyoming, USA. Grand Prismatic is the largest hot spring in the United States, and the third largest in the world, next to those in New Zealand. The sterile blue water in the pool’s center is too hot to support life (87 degrees Centigrade or 188 F). Pure water selectively absorbs red wavelengths of visible light, making the center deep blue. But in cooler water along the edges, microbial mats of thermophilic (heat-loving) cyano-bacteria and algae thrive. Yellow, orange, and red pigments are produced by the bacteria as a natural sunscreen. As a result, the pool displays a spectrum of colors from the bright blue water of the center to the orange, red, and brown algal mats along the edges. Summer mats tend to be orange and red, whereas winter mats become dark green. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978. Photo was published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.  Three overlapping images were stitched to make this panorama.
    04WY-0162-164pan-Grand-Prismatic-Spr...jpg
  • Near Jackass Pass, War Bonnet Peak catches sunrise light, in 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. This image was stitched from multiple overlapping photos.
    1909US1-1207-1233-Pano.jpg
  • Admire colorful microbial mats contrasting with turquoise water at Grand Prismatic Spring overlook in Midway Geyser Basin, Yellowstone National Park, Wyoming, USA. Starting from Fairy Falls Trailhead (OK5), walk 2 miles round trip to the Grand Prismatic Spring overlook, up a side trail. Grand Prismatic is the largest hot spring in the United States, and the third largest in the world, next to those in New Zealand. The sterile blue water in the pool’s center is too hot to support life (87 degrees Centigrade or 188 F). Pure water selectively absorbs red wavelengths of visible light, making the center deep blue. But in cooler water along the edges, microbial mats of thermophilic (heat-loving) cyano-bacteria and algae thrive. Yellow, orange, and red pigments are produced by the bacteria as a natural sunscreen. As a result, the pool displays a spectrum of colors from the bright blue water of the center to the orange, red, and brown algal mats along the edges. Summer mats tend to be orange and red, whereas winter mats become dark green. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978.
    1709US1-3978_Yellowstone-NP-WY.jpg
  • Prairie dog (genus Cynomys) in Devils Tower National Monument, Wyoming, USA. Prairie dogs, a type of ground squirrel, are herbivorous burrowing rodents native to the grasslands of North America.
    1709US1-3424.jpg
  • Bison graze on a frosty morning in Grand Teton National Park, Wyoming, USA.
    1709US1-3602_Grand-Teton-NP-WY.jpg
  • Spray from Yellowstone Falls refracts a rainbow in the "Grand Canyon of the Yellowstone," Yellowstone National Park, Wyoming, USA. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978.
    98AUG-C5-17_Yellowstone-Falls-rainbo...jpg
  • In mid October, bright yellow cottonwood tree leaves frame Devils Tower in Belle Fourche River Campground, in Devils Tower National Monument, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    171013_171941_Devils-Tower-WY.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
  • Fresh snow dusts mountain peaks which reflect in the Snake River at Schwabacher Landing at sunrise in Grand Teton National Park, Wyoming, USA. Five images were stitched to make this panorama. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    04WY-0413-417pan_Teton_Schwabacher.jpg
  • Geothermal steam surrounds a snowy boardwalk along Artists’ Paint Pots Trail in Yellowstone National Park, Wyoming, USA. This image was stitched from multiple overlapping photos.
    1709US1-4291-p1-Pano_Yellowstone-NP-...jpg
  • Palette Spring, Mammoth Hot Springs, Yellowstone National Park, Wyoming, USA. Over thousands of years, Mammoth Hot Springs have built white travertine terraces. Algae and bacteria tint the travertine shades of brown, orange, red, and green. Terrace Mountain (including Minerva Terrace) at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The Mammoth Hotel and Fort Yellowstone are built upon the old Hotel Terrace formation. Hot water from Norris Geyser Basin within the Yellowstone Caldera travels underground via a fault line through limestone and deposits calcium carbonate at Mammoth Hot Springs, outside of the active supervolcano’s caldera. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978.
    04WY-0560.jpg
  • A golden sunrise illuminates Grand Teton, the highest mountain (13,775 feet) in Grand Teton National Park. Wyoming, USA.
    1709US1-3543_Grand-Teton-NP-WY.jpg
  • Dead trees form sharp silhouettes against geothermal steam along Artists’ Paint Pots Trail in Yellowstone National Park, Wyoming, USA.
    1709US1-4248_Yellowstone-NP-WY.jpg
  • Slide Lake in Bridger-Teton National Forest, Wind River Range, Rocky Mountains, Wyoming, USA. Hike from Green River Lakes 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.
    1909US1-0299-309-Pano.jpg
  • Snow-covered Teewinot Mountain (on left 12,325 feet) and Grand Teton (center 13,775 ft) in Grand Teton National Park, Wyoming, USA.
    1709US1-3709_Grand-Teton-NP-WY.jpg
  • Orange Spring Mound, Mammoth Hot Springs, Yellowstone National Park, Wyoming, USA. Over thousands of years, Mammoth Hot Springs have built white travertine terraces. Algae and bacteria tint the travertine shades of brown, orange, red, and green. Terrace Mountain (including Minerva Terrace) at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The Mammoth Hotel and Fort Yellowstone are built upon the old Hotel Terrace formation. Hot water from Norris Geyser Basin within the Yellowstone Caldera travels underground via a fault line through limestone and deposits calcium carbonate at Mammoth Hot Springs, outside of the active supervolcano’s caldera.
    04WY-0589.jpg
  • Canary Spring, Upper Terrace Drive, Mammoth Hot Springs. Yellowstone National Park, Wyoming, USA.
    1709US1-4518_Yellowstone-NP-WY.jpg
  • Mt Moran (12,605 feet) reflects in the Snake River at Oxbow Bend, in Grand Teton National Park, Wyoming, USA. <br />
The mountain is named for Thomas Moran, an American western frontier landscape artist. Mount Moran dominates the northern section of the Teton Range rising 6000 feet above Jackson Lake. Several active glaciers exist on the mountain with Skillet Glacier plainly visible on the monolithic east face. This image was stitched from multiple overlapping photos.
    1709US2-624-625-Pano_Grand-Teton-NP-...jpg
  • Bubbles cluster under ice in String Lake, Grand Teton National Park, Wyoming, USA.
    1709US1-3722.jpg
  • Lenticular clouds (lens or wave clouds) cap the peaks of Grand Teton (13,766 feet or 4198.6 meters) and Teewinot. The Teton Range reflects in the Snake River at Schwabacher Landing in Grand Teton National Park, Wyoming, USA. Grand Teton National Park contains the major peaks of the 40-mile (64 km) Teton Range and part of the valley known as Jackson Hole, Wyoming. The Teton Range began their tectonic uplift 9 million years ago (during the Miocene Epoch), making them the youngest range in the Rocky Mountains. A parkway connects from Grand Teton National Park 10 miles north to Yellowstone National Park. Published in the book "Mountain" by Sandy Hill, 2011, Rizzoli International Publications Inc (p. 103), a benefit for the American Alpine Club Library.
    04WY-0431.jpg
  • Angel Terrace, Mammoth Hot Springs, Yellowstone National Park, Wyoming, USA. Over thousands of years, Mammoth Hot Springs have built white travertine terraces. Algae and bacteria tint the travertine shades of brown, orange, red, and green. Terrace Mountain (including Minerva Terrace) at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The Mammoth Hotel and Fort Yellowstone are built upon the old Hotel Terrace formation. Hot water from Norris Geyser Basin within the Yellowstone Caldera travels underground via a fault line through limestone and deposits calcium carbonate at Mammoth Hot Springs, outside of the active supervolcano’s caldera.
    04WY-0602.jpg
  • Colorful microbial mats coat terraces of Grand Prismatic Spring in Midway Geyser Basin, Yellowstone National Park, Wyoming, USA. Grand Prismatic is the largest hot spring in the United States, and the third largest in the world, next to those in New Zealand. The sterile blue water in the pool’s center is too hot to support life (87 degrees Centigrade or 188 F). Pure water selectively absorbs red wavelengths of visible light, making the center deep blue. But in cooler water along the edges, microbial mats of thermophilic (heat-loving) cyano-bacteria and algae thrive. Yellow, orange, and red pigments are produced by the bacteria as a natural sunscreen. As a result, the pool displays a spectrum of colors from the bright blue water of the center to the orange, red, and brown algal mats along the edges. Summer mats tend to be orange and red, whereas winter mats become dark green. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978.
    04WY-0099.jpg
  • Palette Spring, Mammoth Hot Springs, Yellowstone National Park, Wyoming, USA. Over thousands of years, Mammoth Hot Springs have built white travertine terraces. Algae and bacteria tint the travertine shades of brown, orange, red, and green. Terrace Mountain (including Minerva Terrace) at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The Mammoth Hotel and Fort Yellowstone are built upon the old Hotel Terrace formation. Hot water from Norris Geyser Basin within the Yellowstone Caldera travels underground via a fault line through limestone and deposits calcium carbonate at Mammoth Hot Springs, outside of the active supervolcano’s caldera. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    04WY-0551.jpg
  • Middle and Grand Teton and Teewinot reflect in the Snake River at Schwabacher Landing, Grand Teton National Park, Wyoming, USA
    04WY-0412.jpg
  • Devils Tower National Monument. Bear Lodge Mountains, Black Hills, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    1709US1-3347_Devils-Tower-WY.jpg
  • In mid October, bright yellow cottonwood tree leaves frame Devils Tower in Belle Fourche River Campground, in Devils Tower National Monument, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    1709US1-3471_Devils-Tower-WY.jpg
  • Admire colorful microbial mats contrasting with turquoise water at Grand Prismatic Spring overlook in Midway Geyser Basin, Yellowstone National Park, Wyoming, USA. Starting from Fairy Falls Trailhead (OK5), walk 2 miles round trip to the Grand Prismatic Spring overlook, up a side trail. Grand Prismatic is the largest hot spring in the United States, and the third largest in the world, next to those in New Zealand. The sterile blue water in the pool’s center is too hot to support life (87 degrees Centigrade or 188 F). Pure water selectively absorbs red wavelengths of visible light, making the center deep blue. But in cooler water along the edges, microbial mats of thermophilic (heat-loving) cyano-bacteria and algae thrive. Yellow, orange, and red pigments are produced by the bacteria as a natural sunscreen. As a result, the pool displays a spectrum of colors from the bright blue water of the center to the orange, red, and brown algal mats along the edges. Summer mats tend to be orange and red, whereas winter mats become dark green. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978.
    1709US1-3956_Yellowstone-NP-WY.jpg
  • Horses graze idyllically by a fence beneath snow-covered Grand Teton, the highest mountain (13,775 feet) in Grand Teton National Park. Wyoming, USA.
    1709US1-3634_Grand-Teton-NP-WY.jpg
  • Snowy Teton peaks reflect in Jenny Lake, Grand Teton National Park, Wyoming, USA. This image was stitched from multiple overlapping photos.
    1709US1-3745-54-Pano-Edit_Grand-Teto...jpg
  • Admire colorful microbial mats contrasting with turquoise water at Grand Prismatic Spring overlook in Midway Geyser Basin, Yellowstone National Park, Wyoming, USA. Starting from Fairy Falls Trailhead (OK5), walk 2 miles round trip to the Grand Prismatic Spring overlook, up a side trail. Grand Prismatic is the largest hot spring in the United States, and the third largest in the world, next to those in New Zealand. The sterile blue water in the pool’s center is too hot to support life (87 degrees Centigrade or 188 F). Pure water selectively absorbs red wavelengths of visible light, making the center deep blue. But in cooler water along the edges, microbial mats of thermophilic (heat-loving) cyano-bacteria and algae thrive. Yellow, orange, and red pigments are produced by the bacteria as a natural sunscreen. As a result, the pool displays a spectrum of colors from the bright blue water of the center to the orange, red, and brown algal mats along the edges. Summer mats tend to be orange and red, whereas winter mats become dark green. Yellowstone was the first national park in the world (1872), and UNESCO honored it as a World Heritage site in 1978. This image was stitched from multiple overlapping photos.
    1709US1-4013-16-Pano_Yellowstone-NP-...jpg
  • Mound Terrace above Minerva Terrace, Mammoth Hot Springs. Yellowstone National Park, Wyoming, USA.
    1709US1-4578_Yellowstone-NP-WY.jpg
  • Palette Spring, Mammoth Hot Springs, Yellowstone National Park, Wyoming, USA. Over thousands of years, Mammoth Hot Springs have built white travertine terraces. Algae and bacteria tint the travertine shades of brown, orange, red, and green. Terrace Mountain (including Minerva Terrace) at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The Mammoth Hotel and Fort Yellowstone are built upon the old Hotel Terrace formation. Hot water from Norris Geyser Basin within the Yellowstone Caldera travels underground via a fault line through limestone and deposits calcium carbonate at Mammoth Hot Springs, outside of the active supervolcano’s caldera.
    04WY-0576.jpg
  • In Wyoming, horses graze idyllically by a fence beneath snow-covered Grand Teton (on left 13,775 feet), the highest mountain in Grand Teton National Park. On right is Mount Moran (12,605 feet). This image was stitched from multiple overlapping photos.
    1709US1-3642-46-Pano_Grand-Teton-NP-...jpg
  • Lichen polygons. Green River Lakes, 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).
    1909US1-0116.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
  • A little brown bird, seen on the hike to Photographer's Point, Wind River Range, Bridger-Teton National Forest, Rocky Mountains, Wyoming, USA. The Continental Divide follows the crest of the "Winds".
    1909US1-0355.jpg
  • The Pink House, bunkhouse and barn preserved at John Moulton Homestead, at the corner of Mormon Row and Antelope Flats Road, in the valley of Jackson Hole, Grand Teton National Park, Wyoming, USA. This image was stitched from multiple overlapping photos.
    1909US1-0560-564-Pano.jpg
  • East Temple Peak at sunset, 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. 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.
    1909US1-0813.jpg
  • Sunset at Big Sandy Lake in the Wind River Range. 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.
    1909US1-0871.jpg
  • Lenticular-shaped clouds cap the Cirque of the towers. See Cirque of the Towers in the distance as we cross granite rocks along Little Sandy Trail during the ascent from Clear Lake to Deep Lake, 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.
    1909US1-0907.jpg
  • East Temple Peak rises above Deep Lake 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. This image was stitched from multiple overlapping photos.
    1909US1-0946_949-Pano.jpg
  • Sunrise on War Bonnet Peak seen near 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. This image was stitched from multiple overlapping photos.
    1909US1-1283-1289-Pano.jpg
  • Sunrise spotlights the Tetons which reflect beautifully in the Snake River at Schwabacher Landing (16 miles north of Jackson Hole on US26/89/191). Grand Teton National Park, Wyoming, USA.
    1709US2-554_Grand-Teton-NP-WY.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
  • 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.
    1909US1-1347-1349-Pano.jpg
  • Sunset over Sheep Mountain seen from Buffalo Bill State Park, North Shore Campground, Buffalo Bill Reservoir, Cody, Wyoming, USA. This image was stitched from multiple overlapping photos.
    20.10US1-0951-52-Pano.jpg
  • Lower Yellowstone Falls seen from Artist Point on South Rim Trail. The Yellowstone River flows through the Grand Canyon of the Yellowstone in Yellowstone National Park, in Wyoming, USA. Yellowstone River is a major tributary of the Missouri River. Yellowstone was established as the world's first national park in 1872 and was listed by UNESCO as a World Heritage site in 1978.
    20.10US1-1083.jpg
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