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  • 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
  • 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 6 overlapping images.)
    10GLA-2393-98pan_Two-Medicine-Valley.jpg
  • Yellow flowers bloom in Two Medicine Valley on the Dawson Pass Trail in Glacier National Park, Montana, USA.
    10GLA-2273.jpg
  • Two Medicine Lake, boat launch, Sinopah Mountain (8271 feet or 2521 meters), Glacier National Park, Montana, USA
    10GLA-2239.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
  • 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
  • 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 2 overlapping images.)
    10GLA-2390-91pan_Two-Medicine-Valley.jpg
  • Harsh alpine climate has stunted and deformed an evergreen tree into Krummholz (or Krumholtz) formation in Two Medicine Valley on the Dawson Pass Trail in Glacier National Park, Montana, USA.
    10GLA-2382_Two-Medicine-Valley.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
  • 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
  • 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
  • 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
  • A boy walks in Pray Lake beneath Sinopah Mountain (8271 feet or 2521 meters) at sunset 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-2205-08pan_Pray-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 11 overlapping images.)
    10GLA-2474-2484pan_Pray-Lake_Glacier...jpg
  • At Dawson Pass, see Nyack Creek Valley in Glacier National Park, Montana, USA. In the far distance (on right), Pumpelly Glacier clings to Blackfoot Mountain and Mount Logan. (Panorama stitched from 2 overlapping images.)
    10GLA-2304-2308pan_Nyack-Creek-Valle...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
  • 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
  • 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
  • At Dawson Pass, see Nyack Creek Valley in Glacier National Park, Montana, USA. In the distance, Pumpelly Glacier clings to Blackfoot Mountain and Mount Logan. (Panorama stitched from 2 overlapping images.)
    10GLA-2301-02pan.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
  • 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
  • Two Medicine Lake, boat launch, Sinopah Mountain (8271 feet or 2521 meters), Glacier National Park, Montana, USA
    10GLA-2249-p2.jpg
  • Two Medicine Lake, boat launch, Sinopah Mountain (8271 feet or 2521 meters), Glacier National Park, Montana, USA. (Panorama stitched from 4 overlapping images.)
    10GLA-2231-34pan.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
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