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76 images Created 24 Jun 2011

Favorite Montana photos by Tom Dempsey: Glacier National Park, rock patterns, animals, insects, hiking, panoramas, and historic frontier buildings at Nevada City and Elkhorn State Park.

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  • The mountain goat (Oreamnos americanus, or Rocky Mountain Goat) is a large-hoofed mammal found only in North America. This even-toed ungulate is in the family Bovidae, in subfamily Caprinae (goat-antelopes) in the Oreamnos genus (but is NOT a true "goat"–Capra genus). Sperry Campground, Gunsight Pass Trail, Glacier National Park, Montana, USA
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  • Sunburst over Grinnell Lake, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0820-Pano.jpg
  • A grizzly bear sow and cub (Ursus arctos horribilis, a subspecies of brown bear) forage in a field of Bear grass and other alpine plants. Grinnell Glacier Trail, Glacier National Park, Montana, USA. The species Ursus arctos is found across northern Eurasia (including Russia and Scandinavia) and North America and is an omnivorous mammal of the order Carnivora.
    10GLA-3080.jpg
  • Orange and blue striped rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
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  • Akaiyan Lake at sunset, Sperry Glacier Trail, a side trip from Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0595-Pano-Edit.jpg
  • Ancient fossilized orange & purple seabed ripples at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0582.jpg
  • A mountain goat (Oreamnos americanus) shares the Garden Wall Trail near Logan Pass in Glacier National Park, Montana, USA. 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. The name Oreamnos is derived from the Greek term oros (stem ore-) "mountain" (or, alternatively, oreas "mountain nymph") and the word amnos "lamb".
    10GLA-2052.jpg
  • Fresh snow on Gunsight Pass Trail above Gunsight Lake, Glacier National Park, Montana, USA
    2209RV-0394-Pano.jpg
  • Comeau Pass panorama, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0553-Pano.jpg
  • Snow dusting over Gunsight Lake, Glacier National Park, Montana, USA
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  • A stream descends strikingly striated rock layers above Gunsight Lake, in Glacier National Park, Montana, USA
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  • 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
  • Rock pattern, Gunsight Pass, Glacier National Park, Montana, USA
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  • Borer beetle tracks, Gunsight Pass Trail, Glacier National Park, Montana, USA
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  • Gaillardia (or Blanket flower) is a genus of drought-tolerant annual and perennial plants from the sunflower family (Asteraceae). Photo from Baring Creek Valley, in Glacier National Park, in the Rocky Mountains, Montana, USA.
    10GLA-3532.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0183.jpg
  • Angel Wing and Mount Gould tower over blue-green Grinnell Lake and bear grass on the Grinnell Glacier Trail in Glacier National Park, Montana, USA. Bear grass (Xerophyllum tenax, or synonym Helonias tenax) is a grasslike perennial in the family Melanthiaceae, closely related to lilies. Bear grass (also called squaw grass, soap grass, quip-quip, and Indian basket grass) thrives after fire clears surface vegetation. 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 named glaciers remain in the park as of 2010, and all may disappear as soon as 2020, say climate scientists.
    10GLA-3303-p2.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0567-Pano.jpg
  • Florence Falls, Gunsight Pass Trail, Glacier National Park, Montana, USA
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  • Hike through forest to Two Medicine Lake and No Name Lake on the Dawson Pass Trail 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-2403+07-09pan_Two-Medicine-Val...jpg
  • Orange rock pattern with yellow lichen. Grinnell Glacier Trail, Glacier National Park, Montana, USA
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  • Water tumbles through Avalanche Gorge, in Glacier National Park, Montana, USA
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  • Monkeyflower blooms on Grinnell Glacier Trail, Glacier National Park, Montana, USA.
    10GLA-3252.jpg
  • Billion-year-old seabed ripples are fossilized in a blue rock pattern on broken yellow and purple rocks above Logan Pass, in Glacier National Park, Montana, USA. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010. 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-0182.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-1103_Baring-Creek.jpg
  • Rocky Mountains reflect in Bowman Lake, Glacier National Park, Montana, USA. (Panorama stitched from 3 overlapping images.)
    10GLA-1092-94pan_Bowman-Lake.jpg
  • See Josephine Lake and Grinnell Lake on the Grinnell Glacier Trail 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 as soon as 2020, say climate scientists. (Panorama stitched from 11 overlapping images.)
    10GLA-3224-34pan_Grinnell-Lake.jpg
  • Hike to Grinnell Glacier and powder blue Upper Grinnell Lake under the steep Lewis Range and Mount Gould in Glacier National Park, Montana, USA. The spectacular 11 mile round trip walk (with 1700 feet gain) is shortened to 7.6 miles if you take two boat rides. 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. 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. (Panorama stitched from 14 overlapping images.)
    10GLA-3140-53pan_Upper-Grinnell-Lake.jpg
  • Blue dikes penetrate yellow orange sedimentary rocks at Dawson 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.
    10GLA-2322.jpg
  • See Rising Wolf Mountain (9513 feet/2899 meters) from Flinsch Peak (9225 feet/2812 meters) above Dawson Pass, Oldman Lake (left), Young Man Lake, Two Medicine Lake, Glacier National Park, Montana, USA. (Panorama stitched from 15 overlapping images.)
    10GLA-2336-2350pan_Rising-Wolf-Mount...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
  • Many Glacier Hotel was built in 1915 on the shore of Swiftcurrent Lake, Glacier National Park, Montana, USA. Book a boat tour at the dock. 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 overlapping images.)
    10GLA-2625-33pan_Many-Glacier-Hotel.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
  • A wagon with iron-bound wooden wheels stands outside a late 1800s livery stable preserved at the outdoor history museum of Nevada City, Montana, USA. Nevada City was a booming placer gold mining camp from 1863-1876, but quickly declined into a virtual ghost town. This fascinating town inspires you to imagination what life must have been like in early Montana when gold was discovered at nearby Alder Gulch. More than 90 buildings from across Montana have been gathered for preservation at Nevada City, mostly owned by the people of the State of Montana, and managed by the Montana Heritage Commission. In 2001, the excellent PBS television series "Frontier House" used one of the buildings and its furnishings to train families in re-creating pioneer life. A miner's court trial and hanging of George Ives in the main street of Nevada City was the catalyst for forming the Vigilantes, a group of citizens famous for taking justice into their own hands in 1863-1864. Directions: go 27 miles southeast of Twin Bridges, Montana on Highway 287.
    04MT-1036_Nevada-City-ghost-town.jpg
  • Two original buildings, outstanding examples of American frontier architecture, are preserved and open to the public as Elkhorn State Park (managed by the Montana Department of Fish, Wildlife, and Parks; and recorded in the Historic American Buildings Survey). Gillian Hall (left) was built in the 1880s and served as a store, saloon, and dance hall. Fraternity Hall (right), was built in the 1890s for shows, dances, and lodge meetings. The silver, gold and lead mines at Elkhorn began booming in 1875, then declined in 1892 as silver prices dropped. A few miners still work the Elkhorn mines and live in private homes near these historic State Park buildings within Beaverhead-Deerlodge National Forest. Directions: I-15 at Boulder exit, 7 miles south on Montana 69, then 11 miles north on county graveled road. (Lat 46.275,  Lng  -111.946)
    04MT-0015_Elkhorn-Gillian+Fraternity...jpg
  • Blue and white patterns penetrate brown sedimentary rocks at Dawson 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.
    10GLA-2326.jpg
  • A mountain goat appears to smile at 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).
    02GLA-06-12_the-laughing-mountain-go...jpg
  • The hoary marmot (Marmota caligata) is the largest North American ground squirrel and is often nicknamed "the whistler" for its high-pitched warning issued to alert other members of the colony to possible danger. Hike the Garden Wall trail from Logan Pass in Glacier National Park, Montana, USA. Published in 2013 for "Ranger Rick, Jr. Appventures: Bears App".
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  • 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
  • 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
  • Many Glacier Hotel was built in 1915 on the shore of Swiftcurrent Lake, Glacier National Park, Montana, USA. Book a boat tour at the dock. (Full 360 degree panorama stitched from 22 photographs.) 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-3335-3356pan_Many-Glacier-Hote...jpg
  • The Golden Mantled Ground Squirrel thrives 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-0049-Squirrel.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
  • Gaillardia (or Blanket flower) is a genus of drought-tolerant annual and perennial plants from the sunflower family (Asteraceae). Photo from Baring Creek Valley, in Glacier National Park, in the Rocky Mountains, Montana, USA.
    10GLA-3537.jpg
  • Angel Wing and Mount Gould tower over blue-green Grinnell Lake and bear grass on the Grinnell Glacier Trail in Glacier National Park, Montana, USA. Bear grass (Xerophyllum tenax, or synonym Helonias tenax) is a grasslike perennial in the family Melanthiaceae, closely related to lilies. Bear grass (also called squaw grass, soap grass, quip-quip, and Indian basket grass) thrives after fire clears surface vegetation. 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 named glaciers remain in the park as of 2010, and all may disappear as soon as 2020, say climate scientists. (Panorama stitched from 3 overlapping images.)
    10GLA-2680-82pan_Grinnell-Lake.jpg
  • Many Glacier Hotel was built in 1915 on the shore of Swiftcurrent Lake, 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  6 overlapping images.)
    10GLA-2615-20pan_Many-Glacier-Hotel_...jpg
  • The sticky purple geranium (Geranium viscosissimum) is a perennial in the Geraniaceae family of flowering plants. Apikuni Falls trail, Glacier National Park, Montana, USA.
    10GLA-2559.jpg
  • A mountain goat (Oreamnos americanus) shares the Garden Wall Trail near Logan Pass in Glacier National Park, Montana, USA. 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. The name Oreamnos is derived from the Greek term oros (stem ore-) "mountain" (or, alternatively, oreas "mountain nymph") and the word amnos "lamb".
    10GLA-2072.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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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 sedimentary rocks form complex patterns 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-0038.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
  • 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
  • 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
  • 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
  • Billion-year-old sedimentary rock erodes into yellow and blue patterns in Glacier National Park, Montana, USA. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010. 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-0164.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-0100.jpg
  • Iron-bound wooden wheels decay and rust outside a late 1800s wood building preserved in the outdoor history museum of Nevada City, Montana, USA. Nevada City was a booming placer gold mining camp from 1863-1876, but quickly declined into a virtual ghost town. This fascinating town inspires you to imagination what life must have been like in early Montana when gold was discovered at nearby Alder Gulch. More than 90 buildings from across Montana have been gathered for preservation at Nevada City, mostly owned by the people of the State of Montana, and managed by the Montana Heritage Commission. In 2001, the excellent PBS television series "Frontier House" used one of the buildings and its furnishings to train families in re-creating pioneer life. A miner's court trial and hanging of George Ives in the main street of Nevada City was the catalyst for forming the Vigilantes, a group of citizens famous for taking justice into their own hands in 1863-1864. Directions: go 27 miles southeast of Twin Bridges, Montana on Highway 287.
    04MT-1033_Nevada-City-ghost-town.jpg
  • Hidden Lake seen from flank of Reynolds Mountain. Glacier National Park, Montana, USA
    2209RV-0057-Pano.jpg
  • From Dragon's Tail ridge, see Hidden Lake & Bearhat Mountain in Glacier National Park, Montana, USA
    2209RV-0098-Pano-2.jpg
  • Sharp rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0254.jpg
  • A rainbow shines over the eastern entrance of Glacier National Park, seen from the Blackfeet Indian Memorial on Highway 89, near Saint Mary, Montana, USA.
    2209RV-0266.jpg
  • Deadwood Falls on Reynolds Creek, Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0274.jpg
  • Snow dusting over Gunsight Lake, on Gunsight Pass Trail, in Glacier National Park, Montana, USA
    2209RV-0361-Pano.jpg
  • Red & yellow autumn foliage color at Lake Ellen Wilson, Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0494-Pano.jpg
  • Akaiyan Lake, Sperry Glacier Trail, a side trip from Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0538-Pano.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0767.jpg
  • Orange and blue streaked rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0840.jpg
  • Orange & blue rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0866.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
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