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  • Billion-year-old rock breaks into a jagged pattern in Glacier National Park, Montana. 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-0077.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-0071.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
  • The Golden Mantled Ground Squirrel feeds 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-0050.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
  • 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-0043.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
  • 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
  • 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
  • An old iron rimmed wooden wagon wheel ages in front of a private white-washed building near Elkhorn State Park, Montana, USA. 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 in this historic State Park within Beaverhead-Deerlodge National Forest.
    04MT-0006.jpg
  • An old car body, shot with bullet holes, missing its engine, rusts in Elkhorn State Park, Montana, USA.
    04MT-0003_old-car-Elkhorn-SP.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
  • Billion-year-old rock breaks into blue and 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).
    02GLA-03-04-Exfoliating-rock-pattern.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).
    02GLA-03-02-Rock-pattern-GlacierNP.jpg
  • A mountain goat rests 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-06-16_Mountain-goat.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 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
  • Orange jagged leaf 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).
    07GLA-1438.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-1103_Baring-Creek.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
  • 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
  • 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 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-0106.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-0041.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-0036.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-0029.jpg
  • Lake McDonald reflects peaks of the Livingston Range 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-0010_Lake-McDonald.jpg
  • Part way down from Swiftcurrent Pass, see Bullhead Lake in Swiftcurrent Creek 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. Starting at Logan Pass Visitor Center parking lot, we backpacked the Northern Highline Trail along the Garden Wall to Granite Park, camped overnight (reservation required), then hiked over Swiftcurrent Pass and down the Swiftcurrent Valley to Many Glacier (15.2 miles one way, in two days, 1400 feet gain, with a car shuttle). Plus we dropped packs and hiked a 2-mile side trip up 1200 feet to spectacular Grinnel Lake Overlook. You can also day hike this route from either end.
    02GLA-11-35-Swiftcurrent-Creek-Valle...jpg
  • 1890s Fraternity Hall, American frontier architecture preserved at Elkhorn State Park, Montana, USA
    04MT-0010_Elkhorn-Gillian-Hall-1880-...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
  • Orange rock pattern with yellow lichen. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0894.jpg
  • Grinnell Glacier is rapidly melting into Upper Grinnell Lake. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0842.jpg
  • Many Glacier Hotel, Swiftcurrent Lake, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0761.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0563.jpg
  • Comeau Pass panorama, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0553-Pano.jpg
  • Fresh snow on Gunsight Pass Trail above Gunsight Lake, Glacier National Park, Montana, USA
    2209RV-0394-Pano.jpg
  • Rime ice on leaves at Gunsight Pass, Glacier National Park, Montana, USA
    2209RV-0401.jpg
  • Borer beetle tracks, Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0324.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-0224.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-0208.jpg
  • Bark beetles carved tracks in a downed log in Glacier National Park, Montana, USA.
    10GLA-3562.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-3532.jpg
  • See Sunrift Gorge and Baring Creek along the Going-to-the Sun Road 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-3382.jpg
  • A grizzly bear (Ursus arctos horribilis, a subspecies of brown bear) sow and cubs walk along the 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-3103.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-3027-31pan_Grinnell-Lake.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
  • Purple-blue lupine and red-salmon colored Indian paintbrush flowers bloom on Apikuni Falls Trail in Glacier National Park, Montana, USA. Lupinus is a genus in the pea family (also called the legume, bean, or pulse family, Latin name Fabaceae or Leguminosae). Castilleja, commonly known as Indian paintbrush or Prairie-fire, is a genus of about 200 species of annual and perennial herbaceous plants native to the west of the Americas from Alaska south to the Andes, as well as northeast Asia. Castilleja is classified in the family Orobanchaceae, and is hemiparasitic on the roots of grasses and forbs.
    10GLA-2580.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
  • Blue dikes infuse 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-2325.jpg
  • Bighorn sheep (Ovis canadensis). Dawson Pass hike, 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).
    10GLA-2283.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
    10GLA-2239.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-2132.jpg
  • Cars ascend the Going-to-the-Sun Road towards Logan Pass, seen from the Garden Wall 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.
    10GLA-2092.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-2080.jpg
  • A field of Glacier Lilies blooms at Logan Pass in late July 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-1253-54.jpg
  • A fisherman carries a fish and rod on the shore of Bowman Lake as sunset illuminates the Rocky Mountains in Glacier National Park, Montana, USA.
    10GLA-1110.jpg
  • A photographer walks the shore of Bowman Lake, Glacier National Park, Montana, USA
    10GLA-1083.jpg
  • Bowman Lake, Rainbow Peak (right, 9891 feet elevation), Numa Ridge (left), Glacier National Park, Montana, USA. (Panorama stitched from 4 overlapping images.)
    10GLA-1010-13pan_Bowman-Lake.jpg
  • Garden Wall hike at Logan Pass, Glacier National Park, Montana, USA
    2209RV-0008.jpg
  • Tyrannosaurus rex dinosaur skeleton, 60% real bone (darker color), displayed at Museum of the Rockies, Bozeman, Montana, USA. It stands 12 feet high and 38 feet long. The skull mounted on the skeleton is a full replica with lighter color indicating reconstructed elements, and brown representing the real elements of the actual skull, which is displayed in an adjacent box at eye level.
    20221007_105301.jpg
  • Orange rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0889.jpg
  • Orange rock pattern with yellow lichen. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0892.jpg
  • Spotted Tussock caterpillar (Lophocampa maculata). Glacier National Park, Montana, USA
    2209RV-0882.jpg
  • Grinnell Falls cuts through purple rock layers, along Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0872.jpg
  • Orange & blue rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0866.jpg
  • Orange & blue rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0869.jpg
  • Orange & blue rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0867.jpg
  • Grinnell Glacier. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0863.jpg
  • A boulder on lip of Grinnell Glacier, rapidly melting into Upper Grinnell Lake. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0860.jpg
  • Grinnell Glacier is rapidly melting into Upper Grinnell Lake. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0845-Pano.jpg
  • Orange and blue striped rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0839.jpg
  • Orange and blue streaked rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0840.jpg
  • Orange and blue striped rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0837.jpg
  • Grinnell Falls, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0834.jpg
  • Sunburst over Grinnell Lake, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0829.jpg
  • Sunburst over Grinnell Lake, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0820-Pano.jpg
  • Sunburst along Grinnell Glacier Trail, Grinnell Lake, Glacier National Park, Montana, USA
    2209RV-0800-Pano.jpg
  • Waves on Grinnell Lake, Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0797.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0767.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0772.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0766.jpg
  • Yellow lichen pattern on orange rock. Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0724.jpg
  • 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
    2209RV-0709.jpg
  • Sperry Campground, sunset, Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0688.jpg
  • 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
    2209RV-0692.jpg
  • Golden sunset twilight, purple mountains, bare forest after a fire, seen along Sperry Glacier Trail, a side trip from Gunsight Pass Trail, in Glacier National Park, Montana, USA
    2209RV-0680.jpg
  • Golden sunset twilight, purple mountains, Sperry Glacier Trail, a side trip from Gunsight Pass Trail, in Glacier National Park, Montana, USA
    2209RV-0679.jpg
  • Sunset seen from Sperry Glacier Trail, a side trip from Gunsight Pass Trail, in Glacier National Park, Montana, USA
    2209RV-0666-Pano.jpg
  • Seen at sunset, Sperry Glacier Trail cuts through purple scree, in Glacier National Park, Montana, USA. Seen here in 2022, the forested slopes are recovering from the fires of 2017.
    2209RV-0654.jpg
  • Feather Woman Lake at sunset, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0605-Pano.jpg
  • Broken purple boulders, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0646.jpg
  • Ancient fossilized orange & purple seabed ripples at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0582.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0567-Pano.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0572.jpg
  • Remnants of Sperry Glacier at Comeau Pass, Glacier National Park, Montana, USA
    2209RV-0562.jpg
  • Stairway slot to Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0550.jpg
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