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  • Avalanche lilies and buttercup flowers thrive at Spray Park, Mount Rainier National Park, Washington, USA. Published on the cover of the 1996 Graduate Program Brochure for the Department of Physiology & Biophysics, University of Washington, Seattle.
    85SPR-01-14_Mt-Rainier_Spray-Park.jpg
  • Walk a short loop around Red Rock Canyon in Waterton Lakes National Park, Canadian Rockies, Alberta, Canada. In 1932, Waterton-Glacier International Peace Park joined Glacier National Park in Montana with Waterton. UNESCO honored Waterton-Glacier as a World Heritage Site (1995) containing two Biosphere Reserves (1976). Geology: Rocks in these parks are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    02GLA-12-32-Red-Rock-Canyon.jpg
  • The Merced River plunges 317 feet (97 meters) in the waterfall of Vernal Fall in Yosemite National Park, California, USA. Starting at Happy Isles trail head in Yosemite Valley, hike the steep, paved Mist Trail 2.4 miles round trip with 1000 feet gain to Vernal Fall. Don’t miss Emerald Pool and Nevada Fall further upstream. 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 National Park. Panorama stitched from 4 overlapping photos.
    1111CAL-437-440pan_Vernal-Fall.jpg
  • Trees reflect over stones in Merced River, Yosemite National Park, Sierra Nevada, California, USA. 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 National Park.
    1111CAL-274_Merced-River_Yosemite.jpg
  • Regimental "hoodoos" are eroded pinnacles of soft rock in Bryce Canyon National Park, Utah, USA. Published in Nature, the International Weekly Journal of Science, 17 January 2008 on the cover of the enclosed supplement "Year of Planet Earth," pages 257-304.
    94SW-09-29_Hoodoos_Bryce-Canyon.jpg
  • Mountain goat (Oreamnos americanus), Kootenay National Park, British Columbia, Canada. The mountain goat is an even-toed ungulate of the order Artiodactyla and the family Bovidae (that includes antelopes, gazelles, and cattle). It belongs to the subfamily Caprinae (goat-antelopes), along with thirty-two other species including true goats, sheep, the chamois, and the musk ox. The mountain goat is the only species in the genus Oreamnos. Photo is within the Canadian Rocky Mountain Parks World Heritage Site declared by UNESCO in 1984.
    01CAN-C3-28-Mountain-goat-T.jpg
  • Mountain goat (Oreamnos americanus), Kootenay National Park, British Columbia, Canada. The mountain goat is an even-toed ungulate of the order Artiodactyla and the family Bovidae (that includes antelopes, gazelles, and cattle). It belongs to the subfamily Caprinae (goat-antelopes), along with thirty-two other species including true goats, sheep, the chamois, and the musk ox. The mountain goat is the only species in the genus Oreamnos. Photo is within the Canadian Rocky Mountain Parks World Heritage Site declared by UNESCO in 1984.
    01CAN-C-32_Mountain-goat.jpg
  • Rocky Mountain Bighorn Sheep (Ovis canadensis canadensis), Kootenay National Park, British Columbia, Canada. Wild sheep crossed the Bering land bridge from Siberia during the Pleistocene (about 750,000 years ago) and spread across western North America as far south as Baja California and northwestern Mexico. Genetic divergence from their closest Asian ancestor (snow sheep) occurred about 600,000 years ago. This is part of the Canadian Rocky Mountain Parks World Heritage Site declared by UNESCO in 1984.
    01CAN-09-23-Rocky-Mountain-Bighorn-S...jpg
  • Mountain goat (Oreamnos americanus), Kootenay National Park, British Columbia, Canada. The mountain goat is an even-toed ungulate of the order Artiodactyla and the family Bovidae (that includes antelopes, gazelles, and cattle). It belongs to the subfamily Caprinae (goat-antelopes), along with thirty-two other species including true goats, sheep, the chamois, and the musk ox. The mountain goat is the only species in the genus Oreamnos. Photo is within the Canadian Rocky Mountain Parks World Heritage Site declared by UNESCO in 1984.
    01CAN-08-36-Mountain-goat+horns.jpg
  • The granite dome of Liberty Cap rises 1700 feet (520 m) from the base of Nevada Fall to 7076 feet (2157 m) elevation along on the John Muir Trail in Yosemite National Park, California, USA. To the left is the south side of Half Dome. Designated a World Heritage Site 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-555-557pan_Liberty-Cap_Nevad...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
  • Cathedral Peak reflects in Cathedral Lake, Yosemite National Park, California, USA. Cathedral Peak is the highest summit of the Cathedral Range, an offshoot of the Sierra Nevada Mountain in south-central Yosemite National Park in Tuolumne County. The sharp cathedral-shaped top of the peak was left uneroded as Pleistocene glaciers scraped its flanks smooth. The west peak (left side) of Cathedral Peak is called Eichorn Pinnacle, after Jules Eichorn, who first ascended a route (difficulty = YDS 5.4 ) in 1931. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    96CAL-06-05_Cathedral-Peak-Lake-Yose...jpg
  • Naches Peak Loop Trail in October, Mount Rainier National Park, Washington, USA. In altitude, Washington varies from sea level up to 14,411 feet (4,392 meters) at the summit of Mount Rainier, which is the highest peak in the Cascade Range. With 26 major glaciers, Mount Rainier is the most heavily glaciated peak in the lower 48 states, with 35 square miles (91 square km) of permanent snowfields and glaciers. This active stratovolcano (composite volcano) is in Pierce County, 54 miles (87 km) southeast of Seattle. Published since 2013 on StayRainier.com and AltaCrystalResort.com web sites. Global warming and climate change: Mount Rainier’s glaciers shrank 22% by area and 25% by volume between 1913 and 1994 in conjunction with rising temperatures (Nylen 2004). As of 2009, monitored glaciers are continuing to retreat (NPS). Over the last century, most glaciers have been shrinking across western North America (Moore et al. 2009) and the globe (Lemke et al. 2007) in association with increasing temperatures.
    02RAI-01-13-MtRainierEast.jpg
  • Icicles patterns freeze in Yosemite National Park, Sierra Nevada, California, USA.
    1111CAL-547_ice-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 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
  • On Mount Rainier (14,411 feet elevation or 4392 meters), a climber at 12,000 feet ascends Emmons Glacier, which terminates 7,000 feet below in the White River which flows northwest into Puget Sound. Watersheds in the upper right flow south into the Columbia River. Little Tahoma (11,138 feet) rises at right.  Permitted climbers can ascend Mount Rainier via the Camp Sherman route starting at White River Campground, in Mount Rainier National Park, Washington, USA. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    82RAI-99-01-EmmonsGlacierClimber_16-...jpg
  • West Point Lighthouse, beach, driftwood. Discovery Park is a 534 acre (2.2 square km) park in the peninsular Magnolia neighborhood of Seattle, Washington. It is the city's largest public park and contains 11.81 miles of walking trails. United Indians of All Tribes' Daybreak Star Cultural Center is within the park's boundaries. On the south side of the North Beach strip is a sewage treatment plant, but it is almost entirely concealed from the marsh, beach and trail. The park is built on the historic grounds of Fort Lawton; most of the Fort Lawton Historic District (FLHD) falls within the park (although an enclave within the district remains in military hands), as does the West Point Lighthouse. Both the FLHD and the lighthouse are on the National Register of Historic Places.
    0902DIS-02_Discovery-Park.jpg
  • Argosy ship cruises by West Point Lighthouse. Discovery Park is a 534 acre (2.2 square km) park in the peninsular Magnolia neighborhood of Seattle, Washington. It is the city's largest public park and contains 11.81 miles of walking trails. United Indians of All Tribes' Daybreak Star Cultural Center is within the park's boundaries. On the south side of the North Beach strip is a sewage treatment plant, but it is almost entirely concealed from the marsh, beach and trail. The park is built on the historic grounds of Fort Lawton; most of the Fort Lawton Historic District (FLHD) falls within the park (although an enclave within the district remains in military hands), as does the West Point Lighthouse. Both the FLHD and the lighthouse are on the National Register of Historic Places.
    0902DIS-10_Discovery-Park.jpg
  • Red fire hydrant in Discovery Park, Seattle, Washington.
    0902DIS-22_Discovery-Park.jpg
  • See Coleman Glacier, in Jasper National Park, Alberta, Canada, from Snowbird Pass, hiked via Mount Robson Provincial Park, British Columbia. Mount Robson and Jasper are part of the larger Canadian Rocky Mountain Parks World Heritage Site honored by UNESCO in 1984.
    08CAN-2075_Coleman-Glacier_Jasper-NP.jpg
  • A mountain goat rests at Hidden Lake by Bearhat Mountain in Glacier National Park, Montana, USA. The mountain goat (Oreamnos americanus, or Rocky Mountain Goat) is a large-hoofed mammal found only in North America. It is an even-toed ungulate in the family Bovidae, in subfamily Caprinae (goat-antelopes), in the Oreamnos genus, but is NOT a true "goat" (or Capra genus). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear as soon as 2020, say climate scientists.
    02GLA-06-26_Mountain-goat_Hidden-Lak...jpg
  • Sinopah Mountain (8271 feet or 2521 meters) reflects in Pray Lake at sunrise, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1321-p2.jpg
  • In 1930, the Ptarmigan Tunnel was dug 183 feet through the Ptarmigan Wall for hikers from Many Glacier to reach the Belly River Valley in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0699.jpg
  • The peaks of the Livingston Range rise above Lake McDonald at sunrise in Glacier National Park, Montana, USA. Waves caress red shoreline rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0242_Lake-McDonald.jpg
  • In Denali National Park and Preserve  the only national park in America with a working kennel  sled dogs perform essential wintertime duties in a vast expanse of designated Wilderness area. Visit Denali's Alaskan huskies in the park kennels where rangers and dogs demonstrate a traditional Alaskan mode of travel. Sled dogs are important for patrols because snowmobiles are prohibited within the boundaries of the former Mount McKinley National Park. Alaskan huskies (sled dogs) are not a particular breed nor are they crosses of purebred dogs. They are the product of hundreds of years of breeding dogs for running and pulling sleds in cold weather. Alaskan huskies have a strong desire to run and pull, have a thick two-layer coat of fur, a bushy tail, long legs, and great demeanor. Bred for performance rather than looks, huskies vary widely in appearance.
    06AK_4225-husky-dogs-sled-team-demo.jpg
  • See Coleman Glacier, in Jasper National Park, Alberta, Canada, from Snowbird Pass, hiked via Mount Robson Provincial Park, British Columbia. Mount Robson and Jasper are part of the larger Canadian Rocky Mountain Parks World Heritage Site honored by UNESCO in 1984. Panorama stitched from 9 images.
    08CAN-2064-2072pan-Coleman-Glacier_J...jpg
  • Waterton Lakes National Park, Canadian Rockies, Alberta, Canada. In 1932, Waterton-Glacier International Peace Park joined Glacier National Park in Montana with Waterton. UNESCO honored Waterton-Glacier as a World Heritage Site (1995) containing two Biosphere Reserves (1976). Geology: Rocks in these parks are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    02GLA-14-08E-Waterton-Lake.jpg
  • Walk a short loop around Red Rock Canyon in Waterton Lakes National Park, Canadian Rockies, Alberta, Canada. In 1932, Waterton-Glacier International Peace Park joined Glacier National Park in Montana with Waterton. UNESCO honored Waterton-Glacier as a World Heritage Site (1995) containing two Biosphere Reserves (1976). Geology: Rocks in these parks are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    02GLA-13-02_Red-Rock-Canyon.jpg
  • A mountain goat surveys Hidden Lake in Glacier National Park, Montana, USA. The mountain goat (Oreamnos americanus, or Rocky Mountain Goat) is a large-hoofed mammal found only in North America. It is an even-toed ungulate in the family Bovidae, in subfamily Caprinae (goat-antelopes), in the Oreamnos genus, but is NOT a true "goat" (or Capra genus). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    02GLA-05-03_Mountain-goat_Hidden-Lak...jpg
  • Rising Wolf Mountain (9513 feet/2899 meters) and Sinopah Mountain (left) reflect in Pray Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 11 overlapping images.)
    10GLA-2474-2484pan_Pray-Lake_Glacier...jpg
  • Rising Wolf Mountain (9513 feet/2899 meters) and Sinopah Mountain (left) reflect in Pray Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 4 overlapping images.)
    10GLA-2462-65pan_Pray-Lake.jpg
  • Dawn light illuminates Pray Lake and Sinopah Mountain (8271 feet or 2521 meters) in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 3 images.)
    10GLA-2224-226pan.jpg
  • Hike the Garden Wall Trail from Logan Pass through fields of flowers in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    10GLA-2056-59pan.jpg
  • The Historic Red Bus of Glacier National Park (in Montana, USA) was built on 1930s chassis by the White Motor Company, then rebuilt in 2001 to run on propane. A fleet of these vintage motor coaches provide tours and shuttle services in the park. I highly recommend using public transportation, as park traffic can be very heavy over Going to the Sun Road. A "Jammer" (driver) drives the "Red" (bus). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Published by National Geographic Children's Books 2011: "Ultimate Weird But True."
    07GLA-1464.jpg
  • A hiker crosses a swing bridge over Paradise Creek, on the trail to Cobalt Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1451.jpg
  • Sinopah Mountain (8271 feet or 2521 meters) reflects in Pray Lake at sunrise in Glacier National Park, Montana, USA. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010. (Panorama stitched from 4 overlapping images.) Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1293-96pan-Two-Medicine-Lake-s...jpg
  • Orange hairy caterpillar in Montana, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1228.jpg
  • A Pumpelly Pillar rises above the trail to No Name Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1203.jpg
  • Sinopah Mountain, hikers, and Two Medicine Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1199.jpg
  • Lower Two Medicine Lake reflects peaks in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1195.jpg
  • Hikers walk beneath Sexton Glacier and Going-to-the-Sun Mountain in Glacier National Park, Montana, USA. Hike Siyeh Pass, a gorgeous traverse of 10.3 miles (2300 feet up, 3500 feet down) starting at Siyeh Bend, through Preston Park, and finishing down beautiful Baring Creek Valley. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1074.jpg
  • From Siyeh Pass, see glaciers and orange and purple mountains at the headwaters of Boulder Creek Canyon, in Glacier National Park, Montana, USA (September 2007 photo). Hike Siyeh Pass, a gorgeous traverse of 10.3 miles (2300 feet up, 3500 feet down) starting at Siyeh Bend, through Preston Park, and finishing down beautiful Baring Creek Valley. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-1053-p1.jpg
  • See Mount Wilbur (9321 feet or 2841 meters elevation) along the trail to Iceberg Lake and Ptarmigan Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0735.jpg
  • Hike through forest beneath pyramidal peaks on the trail to Ptarmigan Lake, in Glacier National Park, Montana, USA. (A side trail departs at Ptarmigan Falls to visit Iceberg Lake, which can be a separate day hike, or long extension.) Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0717.jpg
  • See Elizabeth Lake and Belly River Valley from Ptarmigan Tunnel in Glacier National Park, Montana, USA. In 1930, the Ptarmigan Tunnel was dug 183 feet through the Ptarmigan Wall for hikers from Many Glacier to reach the Belly River Valley. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 2 overlapping images.)
    07GLA-0690-691pan_Belly-River-Valley...jpg
  • Glacier National Park, Montana, USA: Hike to Ptarmigan Lake beneath the Ptarmigan Wall, then up to Ptarmigan Tunnel 11.2 miles round trip with 2500 feet gain. (A side trail departs at Ptarmigan Falls to visit Iceberg Lake, which can be a separate day hike, or long extension.) Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0682_Ptarmigan-Lake.jpg
  • Sunrise light hits Going-to-the-Sun Mountain and Little Chief Mountain in the Lewis Range above Saint Mary Lake (4484 feet / 1367 meters elevation) in Glacier National Park, Montana, USA. The Going-to-the-Sun Road runs along the north shore. Here the great plains end and the Rocky Mountains abruptly rise 5000 feet above the lake. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 2 overlapping images.)
    07GLA-0597-598pan_Saint-Mary-Lake.jpg
  • From Piegan Pass, hikers descend Cataract Creek Valley beneath the pinnacle of Mount Gould in the Lewis Range, in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0469.jpg
  • From Piegan Pass, hikers descend Cataract Creek Valley beneath the pinnacle of Mount Gould in the Lewis Range, in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0460_Mount-Gould.jpg
  • A hiking group enjoys Piegan Pass and Mount Gould (far right), in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. For licensing options, please inquire.
    07GLA-0425.jpg
  • Blackfoot Mountain and Blackfoot Glacier, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0420.jpg
  • Hikers approach Piegan Pass in the Lewis Range in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0415.jpg
  • Hikers approach Piegan Pass in the Lewis Range in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0404_Piegan-Pass.jpg
  • Sunrise light hits Going-to-the-Sun Mountain and Little Chief Mountain in the Lewis Range above Saint Mary Lake (4484 feet / 1367 meters elevation) in Glacier National Park, Montana, USA. The Going-to-the-Sun Road runs along the north shore. Here the great plains end and the Rocky Mountains abruptly rise 5000 feet above the lake. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 2 overlapping images.)
    07GLA-0389-390pan_Saint-Mary-Lake.jpg
  • Morning light baths Going-to-the-Sun Mountain and Little Chief Mountain in the Lewis Range above Saint Mary Lake (4484 feet / 1367 meters elevation) in Glacier National Park, Montana, USA. The Going-to-the-Sun Road runs along the north shore. Here the great plains end and the Rocky Mountains abruptly rise 5000 feet above the lake. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 2 overlapping images.)
    07GLA-0268-269pan_St-Mary-Lake.jpg
  • The peaks of the Livingston Range rise above bleached tree roots on the shore of Lake McDonald at sunrise in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0262_Lake-McDonald.jpg
  • The Going-to-the-Sun Road climbs the Garden Wall in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0229.jpg
  • Billion-year-old orange and blue sedimentary rocks erode in complex patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0194.jpg
  • Billion-year-old sedimentary rock erodes into blue patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0190.jpg
  • Snow dusts evergreen trees near Hidden Lake, beneath Bearhat Mountain, a hike from Logan Pass, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0058.jpg
  • Snow dusts evergreen trees near Hidden Lake, beneath Bearhat Mountain, a hike from Logan Pass, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0055.jpg
  • Snow dusts pyramidal peaks and evergreen trees above Logan Pass, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0042.jpg
  • Snow dusts evergreen trees above Logan Pass, in Glacier National Park, Montana. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0023.jpg
  • Billion-year-old rock breaks into a jagged pattern in Glacier National Park, Montana. This image is permanently displayed on the glass of two large lightboxes measuring 19.6 by 8.4 meters (64.3 ft wide x 27.5 ft high) and 16.3 by 3.5 meters (53.6 ft wide x 11.6 ft high), which wrap corners of the following skyscraper constructed by Axiom Builders in June 2019: SODO Residences, 620 10 Ave SW, Calgary, Alberta, CANADA (on the Corner of 5th St and 10 Ave SW). Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these older sediments over newer Cretaceous age rocks.
    02GLA-04-38_Rock-edge-pattern.jpg
  • Mammatus clouds bulge beneath cumulonimbus clouds over yellow and red sandstone on the White Domes trail in Valley of Fire State Park,  Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    95NV-15-15_Valley-of-Fire-SP.jpg
  • Longs Peak (14,259 feet) rises high above Chasm Lake Trail, in Rocky Mountain National Park Wilderness, Estes Park, Colorado, USA. Hike 8.5 miles round trip with 2500 feet gain to Chasm Lake. Longs Peak is in the northern Front Range of the Rocky Mountains.
    2108CO-56.jpg
  • Longs Peak (14,259 feet) rises above Chasm Lake Trail, Rocky Mountain National Park Wilderness, Estes Park, Colorado, USA. Hike 8.5 miles round trip with 2500 feet gain to Chasm Lake. Longs Peak is in the northern Front Range of the Rocky Mountains.
    2108CO-13.jpg
  • Roaring Fork Creek waterfall, Chasm Lake's outlet, Rocky Mountain National Park Wilderness, Estes Park, Colorado, USA. Hike 8.5 miles round trip with 2500 feet gain to Chasm Lake. Longs Peak is in the northern Front Range of the Rocky Mountains.
    2108CO-32.jpg
  • Visitors ride a shuttle boat across Lake Kozjak in Plitvice Lakes National Park (Nacionalni park Plitvicka jezera, in Croatia, Europe). Lake Kozjak connects the Lower Lakes (Donja Jezera) with the Upper Lakes (Gornja Jezera). The park was founded in 1949 and is honored by UNESCO as World Heritage Site. Waters flowing over limestone, dolomite, and chalk in this karstic landscape have, over thousands of years, deposited travertine barriers, creating natural dams, beautiful emerald lakes and waterfalls. Warming conditions after the last Ice Age (less than 12,000 years ago) allowed the natural dams to form from tufa (calcium carbonate) and chalk depositing in layers, bound by plants. Plitvicka Jezera is a municipality of Lika-Senj County, in the Republic of Croatia.
    13CRO-038_Plitvice-Lakes-Croatia.jpg
  • In Denali National Park and Preserve  the only national park in America with a working kennel  sled dogs perform essential wintertime duties in a vast expanse of designated Wilderness area. Visit Denali's Alaskan huskies in the park kennels where rangers and dogs demonstrate a traditional Alaskan mode of travel. Sled dogs are important for patrols because snowmobiles are prohibited within the boundaries of the former Mount McKinley National Park. Alaskan huskies (sled dogs) are not a particular breed nor are they crosses of purebred dogs. They are the product of hundreds of years of breeding dogs for running and pulling sleds in cold weather. Alaskan huskies have a strong desire to run and pull, have a thick two-layer coat of fur, a bushy tail, long legs, and great demeanor. Bred for performance rather than looks, huskies vary widely in appearance.
    06AK_4230-husky-dogs-sled-team-demo.jpg
  • In Denali National Park and Preserve  the only national park in America with a working kennel  sled dogs perform essential wintertime duties in a vast expanse of designated Wilderness area. Visit Denali's Alaskan huskies in the park kennels where rangers and dogs demonstrate a traditional Alaskan mode of travel. Sled dogs are important for patrols because snowmobiles are prohibited within the boundaries of the former Mount McKinley National Park. Alaskan huskies (sled dogs) are not a particular breed nor are they crosses of purebred dogs. They are the product of hundreds of years of breeding dogs for running and pulling sleds in cold weather. Alaskan huskies have a strong desire to run and pull, have a thick two-layer coat of fur, a bushy tail, long legs, and great demeanor. Bred for performance rather than looks, huskies vary widely in appearance.
    06AK_4219-husky-dogs-sled-team-demo.jpg
  • Hike the trail to Marvel Lake, in Banff National Park, Alberta, Canada (along the trail to reach Mount Assiniboine). See Mount Gloria, Eon Mountain (with sharp point, 3310m/10,860 feet), and Aye Mountain (right, 3243meters/10640 feet). This is part of the Canadian Rocky Mountain Parks World Heritage Site declared by UNESCO in 1984.
    09CAN-1196_Marvel-Lake.jpg
  • Rising Wolf Mountain (9513 feet/2899 meters) and Sinopah Mountain (left) reflect in Pray Lake, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 10 overlapping images.)
    10GLA-2501-10pan_Pray-Lake.jpg
  • A nearby forest fire adds a smoky haze over Two Medicine Lake and Sinopah Mountain (8271 feet or 2521 meters), in Montana, in Glacier National Park, part of Waterton-Glacier International Peace Park.
    07GLA-1458.jpg
  • Orange rock and yellow lichen form a pattern in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-1430.jpg
  • Red and green rocks shine in Cobalt Creek, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-1367.jpg
  • Sinopah Mountain (8271 feet or 2521 meters) reflects in Pray Lake at sunrise, in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 4 overlapping images.)
    07GLA-1331-34_Two-Medicine-Lake.jpg
  • Baring Creek tumbles and falls over red sedimentary rocks in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-1128_Baring-Creek.jpg
  • Baring Creek tumbles and falls over red sedimentary rocks in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-1102.jpg
  • Baring Creek tumbles and falls over red sedimentary rocks in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-1099_Baring-Creek.jpg
  • McDonald Creek flows against stone in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-0758_McDonald-Creek.jpg
  • In 1930, the Ptarmigan Tunnel was dug 183 feet through the Ptarmigan Wall for hikers from Many Glacier to reach the Belly River Valley in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0687.jpg
  • Orange butterfly (an insect of the order Lepidoptera) in Glacier National Park, Montana, USA. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks.
    07GLA-0498.jpg
  • From Piegan Pass, hikers descend Cataract Creek Valley beneath the pinnacle of Mount Gould in the Lewis Range, in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0440_Mount-Gould_Cataract-Vall...jpg
  • From Piegan Pass, descend Cataract Creek Valley beneath the pinnacle of Mount Gould in the Lewis Range, in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists.
    07GLA-0436_Mount-Gould_Cataract-Vall...jpg
  • From Piegan Pass, descend Cataract Creek Valley beneath the pinnacle of Mount Gould in the Lewis Range, in Glacier National Park, Montana, USA. A scenic walking traverse starts from Siyeh Bend over Piegan Pass to Many Glacier, visiting glorious mountains, valleys and lakes over 13 miles (2260 feet up, 3520 feet down). Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976). Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Glaciers carved spectacular U-shaped valleys and pyramidal peaks as recently as the Last Glacial Maximum (the last "Ice Age" 25,000 to 13,000 years ago). Of the 150 glaciers existing in the mid 1800s, only 25 active glaciers remain in the park as of 2010, and all may disappear by 2020, say climate scientists. (Panorama stitched from 2 overlapping images.)
    07GLA-0433-434pan_Mount-Gould_Catara...jpg
  • Billion-year-old orange sedimentary rocks erode in complex patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0188.jpg
  • Billion-year-old orange sedimentary rocks erode in complex patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0187.jpg
  • Billion-year-old orange sedimentary rocks erode in complex patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0186.jpg
  • Billion-year-old sedimentary rock erodes into orange patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0169.jpg
  • Billion-year-old sedimentary rock erodes into orange patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0168.jpg
  • Billion-year-old rock breaks into blue, orange, and purple patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0163.jpg
  • Billion-year-old rock breaks into blue, orange, and purple patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0137.jpg
  • Billion-year-old rock breaks into blue, orange, and red patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0129.jpg
  • Billion-year-old rock breaks into blue, orange, and red patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0127.jpg
  • Billion-year-old rock breaks into blue, orange, and red patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0123.jpg
  • Billion-year-old sedimentary rock erodes into yellow and purple patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0102.jpg
  • Billion-year-old sedimentary rock erodes into yellow and purple patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0098.jpg
  • Billion-year-old rock breaks into blue, orange, and purple patterns in Glacier National Park, Montana, USA. Rocks in the park are primarily sedimentary layers deposited in shallow seas over 1.6 billion to 800 million years ago. During the tectonic formation of the Rocky Mountains 170 million years ago, the Lewis Overthrust displaced these old rocks over newer Cretaceous age rocks. Since 1932, Canada and USA have shared Waterton-Glacier International Peace Park, which UNESCO declared a World Heritage Site (1995) containing two Biosphere Reserves (1976).
    07GLA-0097.jpg
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