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  • Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0770.jpg
  • Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0768.jpg
  • Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0765.jpg
  • Valve wheels and meters. Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0754.jpg
  • The national flag of the United States and the state flag of Idaho fly from a mast. The Seal of the Territory of Idaho was adopted in 1863 and redrawn several times before statehood in 1890. The state Great Seal was designed by Emma Edwards Green, the only woman to design a state seal. The outer ring says "Great Seal of the State of Idaho," with the star signifying a new light in the galaxy of states. The inner ring contains a banner with the Latin motto, Esto perpetua ("Let it be perpetual" or "It is forever"). A woman signifies justice, and a man dressed as a miner commemorates the chief industry in the 1890s. A shield shows a pine tree (timber interests), the Snake or Shoshone River, and a man plowing a field. A sheaf of grain and cornucopias (horns of plenty) portray bountiful agriculture.  An elk's head rises above the shield. The state flower (the wild Syringa or Mock Orange) and ripened wheat grow next to the woman.
    07SAW-0763.jpg
  • Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho. Panorama stitched from 2 overlapping photos.
    07SAW-0692-93pan_Yankee-Fork-Gold-Dr...jpg
  • Large metal drive gears. Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0695.jpg
  • Large wire cable spools. Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0700.jpg
  • Liquid tanks. Yankee Fork Gold Dredge operated from 1940-1952 near near Custer Historic Site, in Idaho, USA. This floating gold dredge chewed a wide swath of stream gravel leaving rocky dredge tailings along 5.5 miles of the Yankee Fork, a tributary of the Salmon River, near Stanley, Idaho, USA. It recovered an estimated $1,037,322 in gold and silver at a cost of $1,076,100. Visit Land of the Yankee Fork State Park in Salmon-Challis National Forest near Stanley, Idaho.
    07SAW-0734.jpg
  • At sunrise, peaks of Sawtooth Wilderness reflect in Little Redfish Lake in Sawtooth National Recreation Area, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 4 overlapping photos.
    07SAW-1115-18pan_Little-Redfish-Lake.jpg
  • At sunrise, peaks of Sawtooth Wilderness reflect in Little Redfish Lake in Sawtooth National Recreation Area, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 4 overlapping photos.
    07SAW-1111-14pan_Little-Redfish-Lake.jpg
  • A brown mushroom (fungi) with white edges grows in Sawtooth National Recreation Area, Idaho, USA.
    07SAW-1088.jpg
  • A lupine flower blooms from green leaves, in Sawtooth National Recreation Area, Idaho, USA. Lupines or lupins (Genus: Lupinus) are in the Fabaceae or Leguminosae Family (also called the legume, pea, bean, or pulse family of flowering plants).
    07SAW-1079.jpg
  • Peaks of Sawtooth Wilderness reflect in Little Redfish Lake in Sawtooth National Recreation Area, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 2 overlapping photos.
    07SAW-0611-12pan_Little-Redfish_lake...jpg
  • Alice Lake (8598 feet elevation) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0558.jpg
  • Red canoes and peaks of Sawtooth Wilderness reflect in Little Redfish Lake in Sawtooth National Recreation Area, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0648.jpg
  • Brown, weathered tree trunk wood twists in a pattern, in Sawtooth Wilderness, Blaine County, Idaho, USA. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0524.jpg
  • Twin Lakes (8858 feet elevation) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0520.jpg
  • Orange sunrise light strikes peaks over Alice Lake (8598 feet elevation) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0500.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. Grass swirls in patterns in the water. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    07SAW-0475.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. Grass swirls in patterns in the water. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0468.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 5 overlapping photos.
    07SAW-0455-59pan_El-Capitan.jpg
  • The pyramidal peak of El Capitan rises to 9846 feet or 3001 elevation in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0463.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 3 overlapping photos.
    07SAW-0448-50pan_El-Capitan.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0448-p1.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0432.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 3 overlapping photos.
    07SAW-0443-45_El-Capitan.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0419.jpg
  • Tree needles turn yellow in Sawtooth Wilderness, near Stanley, Idaho, USA. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0417.jpg
  • Yellow lichen grows on a tree burl in Sawtooth Wilderness, near Stanley, Idaho, USA. The Sawtooths are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0416.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). Panorama stitched from 2 overlapping photos.
    07SAW-0400-01pan_El-Capitan.jpg
  • The pyramidal peak of El Capitan (9846 feet or 3001 elevation) reflects in the outlet stream of Alice Lake (Pettit Lake Creek) in Sawtooth Wilderness, Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0391.jpg
  • Orange sunrise light strikes Sawtooth Wilderness mountains reflected in Pettit Lake, near Stanley, Idaho, in Sawtooth National Recreation Area, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0341.jpg
  • Orange sunrise light strikes Sawtooth Wilderness mountains reflected in Pettit Lake, near Stanley, Idaho, in Sawtooth National Recreation Area, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0338-p1.jpg
  • Sunrise light illuminates virga clouds over Pettit Lake, near Stanley, Idaho, in Sawtooth National Recreation Area, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0314.jpg
  • Grand Mogul and Heyburn Peak rise above motor boats docked at Redfish Lake Lodge, in Sawtooth National Recreation Area, Idaho, USA. Backpack or day hike 11.8 miles round trip to Baron Lakes viewpoint: From Redfish Lake Lodge (redfishlake.com) take the earliest boat in the morning to Redfish Lake Inlet Transfer Camp, riding about 10 minutes. Hike 3.2 miles then turn right at the fork and begin climbing. At 4.2 miles see Alpine Lake, then switchback past three smaller lakes. At 5.9 miles, see the breathtaking view of Baron Lakes (Upper, Baron, and Little) and jagged points along the ridge of Warbonnet Peak (10,210 feet elevation). Optionally descend past the Upper Lake to reach the shore of Baron Lake at 7.9 miles one way. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0254.jpg
  • The least chipmunk (Neotamias minimus) is the smallest and most widespread species of chipmunk in North America. Photographed in Sawtooth National Recreation Area, Idaho, USA. Chipmunks are small, striped squirrels, which are rodents in the family Sciuridae. All species of chipmunks are found in North America, except for the Siberian chipmunk of Asia. The least chipmunk lives across north-central and western United States and from British Columbia and southern Yukon to western Quebec in Canada, in habitats including mixed deciduous and coniferous forests, boreal forest, and sagebrush plains. They have three dark lines with white in between along their face and five black stripes with brown edges with white in between along their back. They are grey and reddish-brown on the sides and greyish white on their underparts. Their tail is orange-brown. These animals are active during the day and eat seeds, berries, nuts, fruits and insects. They breed in early spring. Females produce one litter usually of 5 or 6 young. They store food in an underground burrow, where they spend the winter. They go into a state of torpor for extended periods, but do not hibernate. Chipmunks have facial stripes, whereas golden-mantled ground squirrels lack facial stripes.
    07SAW-0246.jpg
  • Beneath a craggy granite peak, a hiker descends towards Alpine Lake from the pass that overlooks Baron Lakes, in Sawtooth Wilderness, Blaine County, Idaho, USA. Backpack or day hike 11.8 miles round trip to Baron Lakes viewpoint: From Redfish Lake Lodge (redfishlake.com) take the earliest boat in the morning to Redfish Lake Inlet Transfer Camp, riding about 10 minutes. Hike 3.2 miles then turn right at the fork and begin climbing. At 4.2 miles see Alpine Lake, then switchback past three smaller lakes. At 5.9 miles, see the breathtaking view of Baron Lakes (Upper, Baron, and Little) and jagged points along the ridge of Warbonnet Peak (10,210 feet elevation). Optionally descend past the Upper Lake to reach the shore of Baron Lake at 7.9 miles one way. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0231.jpg
  • Baron Lakes, in Sawtooth Wilderness, Blaine County, Idaho, USA. Backpack or day hike 11.8 miles round trip to Baron Lakes viewpoint: From Redfish Lake Lodge (redfishlake.com) take the earliest boat in the morning to Redfish Lake Inlet Transfer Camp, riding about 10 minutes. Hike 3.2 miles then turn right at the fork and begin climbing. At 4.2 miles see Alpine Lake, then switchback past three smaller lakes. At 5.9 miles, see the breathtaking view of Baron Lakes (Upper, Baron, and Little) and jagged points along the ridge of Warbonnet Peak (10,210 feet elevation). Optionally descend past the Upper Lake to reach the shore of Baron Lake at 7.9 miles one way. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0224-p1-Baron-Lakes.jpg
  • Baron Lakes, in Sawtooth Wilderness, Blaine County, Idaho, USA. Backpack or day hike 11.8 miles round trip to Baron Lakes viewpoint: From Redfish Lake Lodge (redfishlake.com) take the earliest boat in the morning to Redfish Lake Inlet Transfer Camp, riding about 10 minutes. Hike 3.2 miles then turn right at the fork and begin climbing. At 4.2 miles see Alpine Lake, then switchback past three smaller lakes. At 5.9 miles, see the breathtaking view of Baron Lakes (Upper, Baron, and Little) and jagged points along the ridge of Warbonnet Peak (10,210 feet elevation). Optionally descend past the Upper Lake to reach the shore of Baron Lake at 7.9 miles one way. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0213.jpg
  • Baron Lakes, in Sawtooth Wilderness, Blaine County, Idaho, USA. Backpack or day hike 11.8 miles round trip to Baron Lakes viewpoint: From Redfish Lake Lodge (redfishlake.com) take the earliest boat in the morning to Redfish Lake Inlet Transfer Camp, riding about 10 minutes. Hike 3.2 miles then turn right at the fork and begin climbing. At 4.2 miles see Alpine Lake, then switchback past three smaller lakes. At 5.9 miles, see the breathtaking view of Baron Lakes (Upper, Baron, and Little) and jagged points along the ridge of Warbonnet Peak (10,210 feet elevation). Optionally descend past the Upper Lake to reach the shore of Baron Lake at 7.9 miles one way. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0195.jpg
  • Hike to Alpine Lake along Redfish Creek (8331 feet), in Sawtooth Wilderness, Blaine County, Idaho, USA. Start from Redfish Lake Inlet Transfer Camp and hike 4.2 miles one way to Alpine Lake. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0133_Alpine-Lake-Sawtooths.jpg
  • Orange sunset lights a granite peak in the Sawtooth Wilderness (above Redfish Lake Creek), Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0101.jpg
  • A granite peak rises in the Sawtooth Wilderness (above Redfish Lake Creek), Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0081.jpg
  • A backpacker with camera gear hikes in Sawtooth Wilderness Area, Idaho, USA. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA). For licensing options, please inquire.
    07SAW-0060.jpg
  • Hike with children in Sawtooth Wilderness Area, Idaho, USA. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0050.jpg
  • Hike to see craggy Heyburn Mountain in Sawtooth Wilderness (above Redfish Lake Creek), Blaine County, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are comprised of the pink granite of the 50 million year old Sawtooth batholith. Sawtooth Wilderness, managed by the US Forest Service within Sawtooth National Recreation Area, has some of the best air quality in the lower 48 states (says the US EPA).
    07SAW-0033.jpg
  • Sunset turns clouds orange in a blue sky over Idaho, USA.
    04ID-0014.jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0092.jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0089.jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0063.jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0051_viewing-platform-Upper-Mes...jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create today's inner canyon.
    04ID-0040.jpg
  • Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0037.jpg
  • Lower Mesa Falls plunges 65 feet along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest near Ashton in southeastern Idaho, USA. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0034.jpg
  • Lower Mesa Falls plunges 65 feet along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest near Ashton in southeastern Idaho, USA. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which compressed and hardened over time. Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River carved a channel through the basalt to create todays inner canyon.
    04ID-0031.jpg
  • Sunset turns clouds orange in a blue sky over Idaho, USA.
    04ID-0014.jpg
  • A ranch gate frames the Sawtooth Mountains near Stanley, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith.
    07SAW-1161.jpg
  • A ranch gate frames the Sawtooth Mountains near Stanley, Idaho, USA. A horse stands behind fencing. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith. Panorama stitched from 2 overlapping photos.
    07SAW-1156-57pan_Sawtooth-Mountains_...jpg
  • Cattle graze in a fenced ranch at the foot of the Sawtooth Mountains, near Stanley, Idaho, USA. The Sawtooth Range (part of the Rocky Mountains) are made of pink granite of the 50 million year old Sawtooth batholith.
    07SAW-1141.jpg
  • The Sunbeam Dam, on the Salmon River, Idaho, was built in 1910 to make electricity for the Sunbeam Mine, which was abandoned in 1911 after bankruptcy. The cliff was breached in 1934 to allow salmon and steelhead to migrate to their spawning beds.
    07SAW-0818-Sunbeam-Dam.jpg
  • Old fire wagon. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0808-0ld-wagon.jpg
  • Ore stamping mill. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0811-Custer-stamp-mill.jpg
  • An old Singer sewing machine is powered by a foot crank. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0798.jpg
  • Gears to hand crank an early washing machine. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0790-hand-cranked_washer.jpg
  • Lanterns. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0785.jpg
  • Old egg beater. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0784.jpg
  • A plunge bath tub and old wooden rocking chair sit in a bare room with peeling wallpaper in the former gold mining town of Custer which dates from 1879-1910. Custer Historic Site now preserves this ghost town near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0777.jpg
  • Old iron wood-burning stove. Formerly a gold mining town from 1879-1910, Custer Historic Site is now a ghost town, near Stanley, Idaho, USA. The city of Custer was named after General George Armstrong Custer, who was killed in battle in 1876. Custer is now part of the Land of the Yankee Fork State Park and Challis National Forest Historic Area.
    07SAW-0780.jpg
  • Rock Fringe (Epilobium obcordatum) is in the primrose family (Onagraceae) and is native to the western United States from California to Idaho, where it is found in rocky mountainous areas. It has stems lined with oval or rounded leaves. At the stem tips are flowers each with four petals, magenta to purple, rounded and notched, often in a perfect heart shape, one or two centimeters long. Off Highway 88 near Carson Pass, hike a varied loop through lush wildflower fields from Woods Lake Campground to Winnnemucca Lake then Round Top Lake, in Mokelumne Wilderness, El Dorado National Forest, Sierra Nevada, California, USA. The excellent loop trail is 5.3 miles with 1250 feet gain (or 6.4 miles with 2170 feet gain if adding the scramble up Round Top).
    1507CAL-1045.jpg
  • Triteleia grandiflora flowers bloom atop a leafless stem along the Wenaha River Trail, in the Blue Mountains, Umatilla National Forest, Oregon, USA. Triteleia grandiflora (Largeflower Tripletlily or Wild Hyacinth) is native to western North America from British Columbia to extreme northern California, eastward into Idaho, Montana and northern Utah, with patches in Wyoming and Colorado. This perennial herb grows from a corm. Each funnel-shaped flower bloom is on a pedicel 4 to 5 centimeters long. The flower may be up to 3.5 centimeters long including the tubular throat and six tepals each just over a centimeter long. The inner set of three tepals are ruffled and broader than the outer tepals. The flower corolla may be deep blue to almost white with a darker blue mid-vein. The six stamens have purple or yellow anthers.
    1405OR-046.jpg
  • Howser Spires (11,150 feet) reflect in a pretty tarn (mountain pond) in Bugaboo Provincial Park, south of Golden, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago. Published in the Irish Mountain Log, "The magazine for Walkers and Climbers in Ireland", Summer 2008.
    01CAN-15-04-Howser-Spire-reflects.jpg
  • Sunrise light strikes Snowpatch Spire (10,050 feet) and reflects in a mountain pond (tarn) in Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    01CAN-14-05-Snowpatch-Spire-reflects.jpg
  • Hound's Tooth and Bugaboo Glacier, Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago.
    01CAN-14-02_Hounds-Tooth-2.jpg
  • Hound's Tooth and Bugaboo Glacier, Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago.
    01CAN-13-39_Bugaboo-Glacier-Hounds-T...jpg
  • Sunset light hits the Rocky Mountains at Conrad Kain Hut, Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago.
    01CAN-13-07_Kain-Hut-Rockies-sunset.jpg
  • Sextet Ridge Glacier and larch trees in the fall at Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    01CAN-12-31-Sextet-Ridge-glacier-lar...jpg
  • Chicken wire and posts make a barrier to keep porcupines from chewing on vital hoses and lines under cars in Bugaboo Provincial Park, British Columbia, Canada. The Bugaboos are a range in the Purcell Mountains, which are a subrange of the Columbia Mountains, which are west of the Rocky Mountain Trench. (Some USA maps label the “Percell Mountains” where their southern limit protrudes into the states of Idaho and Montana.) The igneous Bugaboo intrusion of 135 million years ago cooled into hard crystalline granite and was scraped into spires by glaciers eroding surrounding rock dating from 600 million to 1 billion years ago.
    01CAN-09-27-fenced-camper.jpg
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