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Lauren Grabelle

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Lauren Grabelle

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  • View of Glacier National Park with bison in foreground while passing through East Glacier in late fall
    lgphoto_101113_0181.jpg
  • Cowboy and herd of horses on the roadside
    LGP_5655.jpg
  • lgphoto_120726_0361.jpg
  • Early morning flight out of Glacier National Airport heading over Hungry Horse Reservoir with views of the Bob Marshall and Great Bear Wilderness and Glacier National Park
    lgphoto_100716_0003.jpg
  • Avalance Lake at Glacier National Park
    LGP_8518.jpg
  • Avalance Lake at Glacier National Park
    LGP_8518.jpg
  • Big horn sheep standing in a handicap parking space at Logan Pass Visitor Center in Glacier National Park
    lgphoto_120726_0409.jpg
  • Sperry Glacier as viewed from Mount Clements is on the left side of the distant peak known as Gunsight Mountain, Glacier National Park, Montana, Tuesday, October 7, 2014. Sperry Glacier, one of the largest glaciers remaining in the park, is the glacier most studied by the USGS. Hidden Lake is visible in the lower center frame. Edwards Mountain is to the right of Gunsight.
    lgphoto_141007_0196.jpg
  • Sperry Glacier as viewed from Mount Clements is on the left side of the distant peak known as Gunsight Mountain, Glacier National Park, Montana, Tuesday, October 7, 2014. Sperry Glacier, one of the largest glaciers remaining in the park, is the glacier most studied by the USGS. Edwards Mountain is to the right of Gunsight.
    lgphoto_141007_0194.jpg
  • Sperry Glacier as viewed from Mount Clements is on the left side of the distant peak known as Gunsight Mountain, Glacier National Park, Montana, Tuesday, October 7, 2014. Sperry Glacier, one of the largest glaciers remaining in the park, is the glacier most studied by the USGS. Edwards Mountain is to the right of Gunsight.
    lgphoto_141007_0205.jpg
  • Debris left by a melting glacier and the lateral moraine marking the edge of where the glacier was with the peak of Bearhat Mountain in the distance at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. rocky debris fields are created when a glacier melts and the rocks within it are no longer suspended in ice and fall to the ground.
    lgphoto_141007_0145.jpg
  • Sperry Glacier as viewed from Mount Clements is on the left side of the distant peak known as Gunsight Mountain, Glacier National Park, Montana, Tuesday, October 7, 2014. Sperry Glacier, one of the largest glaciers remaining in the park, is the glacier most studied by the USGS. Edwards Mountain is to the right of Gunsight.
    lgphoto_141007_0203.jpg
  • Scratches in rock at the location of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. glacier movement caused scratches in rock and is evidence that a glacier was there and in motion.
    lgphoto_141007_0119.jpg
  • Scratches in rock in a debris field at the location of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. glacier movement caused scratches in rock and is evidence that a glacier was there and in motion.
    lgphoto_141007_0154.jpg
  • Scratches in rock at the location of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. glacier movement caused scratches in rock and is evidence that a glacier was there and in motion.
    lgphoto_141007_0115.jpg
  • Scratches in rock at the location of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. glacier movement caused scratches in rock and is evidence that a glacier was there and in motion.
    lgphoto_141007_0120.jpg
  • A lateral moraine (top right) showing the edge of a glacier that disappeared from the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. Dan Fagre Ph.D. of the USGS and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0159.jpg
  • Daniel Fagre Ph.D., a research ecologist for the USGS in his office in the Global Change building in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. He described the effects of receding glaciers to mountain ecosystems. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0022.jpg
  • New York Times correspondent, Michael Wines, standing atop a lateral moraine of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. Sperry Glacier at the top of Gunsight Mountain is visible in the distance.
    lgphoto_141007_0174.jpg
  • Marbelized rock amongst debris left by a melting glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. rocky debris fields are created when a glacier melts and the rocks within it are no longer suspended in ice and fall to the ground.
    lgphoto_141007_0150.jpg
  • Scratches in rock at the location of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. glacier movement caused scratches in rock and is evidence that a glacier was there and in motion.
    lgphoto_141007_0117.jpg
  • Daniel Fagre Ph.D., a research ecologist for the USGS in his office in the Global Change building in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. He described the effects of receding glaciers to mountain ecosystems. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0008.jpg
  • Debris left by a melting glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. rocky debris fields are created when a glacier melts and the rocks within it are no longer suspended in ice and fall to the ground.
    lgphoto_141007_0141.jpg
  • Daniel Fagre Ph.D., a research ecologist for the USGS in his office in the Global Change building in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. He described the effects of receding glaciers to mountain ecosystems. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0038.jpg
  • Daniel Fagre Ph.D., a research ecologist for the USGS in his office in the Global Change building in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. He described the effects of receding glaciers to mountain ecosystems. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0035.jpg
  • Daniel Fagre Ph.D., a research ecologist for the USGS in his office in the Global Change building in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. He described the effects of receding glaciers to mountain ecosystems. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0015.jpg
  • Debris left by a melting glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. rocky debris fields are created when a glacier melts and the rocks within it are no longer suspended in ice and fall to the ground.
    lgphoto_141007_0144.jpg
  • A snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's.
    lgphoto_141007_0158.jpg
  • A shelf of books in the office of Daniel Fagre Ph.D., a research ecologist for the USGS in Glacier National Park, West Glacier, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0017.jpg
  • Marbelized rock amongst debris left by a melting glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. rocky debris fields are created when a glacier melts and the rocks within it are no longer suspended in ice and fall to the ground.
    lgphoto_141007_0151.jpg
  • A lateral moraine (center) showing the edge of a glacier that disappeared from the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. Dan Fagre Ph.D. of the USGS and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0100.jpg
  • A snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's.
    lgphoto_141007_0162.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0198.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0185.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0188.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0184.jpg
  • Family standing on the shore of Redrock Lake near the Continental Divide Trail in the Many Glacier area of Glacier National Park in NW Montana.
    lgphoto_120726_0248.jpg
  • View of Mount Reynolds from the lateral moraine left by a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0207.jpg
  • Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. The terminal moraine, a pile of gravel rocks created by the leading edge of a glacier that likely disappeared in the 1940's is visible just below the snowfield.
    lgphoto_141007_0089.jpg
  • Exterior of the United States Geological Survey's Global Change building in Glacier National Park, West Glacier, Montana, on Tuesday, October 7, 2014.
    lgphoto_141007_0002.jpg
  • A view of the valley and Upper McDonald Creek as seen from Going to the Sun Road in Glacier National Park, Montana, Tuesday, October 7, 2014. This u-shaped valley was created by a glacier from the ice age that ended 12,000 years ago.
    lgphoto_141007_0075.jpg
  • Cracked mud that turned into rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. this rock formed 1/2 a billion or more years ago and is part of the rock that makes up the mountains of Glacier National Park.
    lgphoto_141007_0210.jpg
  • The remaining snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's. In the distance is the Garden Wall.
    lgphoto_141007_0200.jpg
  • A lateral moraine (foreground) showing the edge of a glacier that disappeared from the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. In the distance are the peaks of the mountains above St. Mary Lake.
    lgphoto_141007_0199.jpg
  • Late blooming aster in the debris left by a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall and that without the water available from melting ice in the late summer a lot of grasses will dry up and be less nutritious.
    lgphoto_141007_0160.jpg
  • A view of the valley and Going to the Sun Road in Glacier National Park, Montana, Tuesday, October 7, 2014. This u-shaped valley was created by a glacier from the ice age that ended 12,000 years ago.
    lgphoto_141007_0081.jpg
  • View of Bird Woman Falls (center bottom) and the snow field that feeds it as seen from Going to the Sun Road in Glacier National Park, Montana, Tuesday, October 7, 2014. The cirque above the falls used to contain a small glacier but no longer has one.
    lgphoto_141007_0073.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0170.jpg
  • View of Going to the Sun Road below the Garden Wall in Glacier National Park, Montana, Tuesday, October 7, 2014. Going to the Sun Road which goes to Logan Pass and crosses the continental divide is the only road that crosses Glacier National Park and was completed in 1932.
    lgphoto_141007_0068.jpg
  • A view from Going to the Sun Road looking down onto a patch of larch pines in autumn, in Glacier National Park, Montana, Tuesday, October 7, 2014. Going to the Sun Road which goes to Logan Pass and crosses the continental divide is the only road that crosses Glacier National Park and was completed in 1932.
    lgphoto_141007_0064.jpg
  • Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's.
    lgphoto_141007_0232.jpg
  • New York Times correspondent, Michael Wines, standing atop a lateral moraine of a former glacier at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014.
    lgphoto_141007_0172.jpg
  • A lateral moraine (foreground) showing the edge of a glacier that disappeared from the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. In the distance are the peaks of the mountains above St. Mary Lake.
    lgphoto_141007_0130.jpg
  • Research ecologist, Daniel Fagre Ph.D., on Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0085.jpg
  • Entrance sign to Glacier National Park in West Glacier, Montana, on Tuesday, October 7, 2014.
    lgphoto_141007_0001.jpg
  • Wolverine tracks in the snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. According to Dan Fagre Ph.D. wolverine are snow-dependent carnivores and snow is no longer lasting in the Logan Pass area.
    lgphoto_141007_0164.jpg
  • A view of the valley and Upper McDonald Creek as seen from Going to the Sun Road in Glacier National Park, Montana, Tuesday, October 7, 2014. This u-shaped valley was created by a glacier from the ice age that ended 12,000 years ago.
    lgphoto_141007_0251.jpg
  • Snow poles on Hidden Lake Trail at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Snow poles are stuck in the ground at the end of season to mark the location of the trails for snow clearing in early summer and show what a snow dominated area Glacier National Park is and that there will be vast changes in the park's ecosystem as the snow continues to diminish.
    lgphoto_141007_0244.jpg
  • A snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's.
    lgphoto_141007_0161.jpg
  • A snowfield at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS this is the location of a glacier from the little ice age that ended in 1850 and probably disappeared in the 1940's.
    lgphoto_141007_0156.jpg
  • Research ecologist, Daniel Fagre Ph.D., on Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0098.jpg
  • Research ecologist, Daniel Fagre Ph.D., on Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0094.jpg
  • Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. The terminal moraine, a pile of gravel rocks created by the leading edge of a glacier that likely disappeared in the 1940's is visible in the middle distance going across the image.
    lgphoto_141007_0093.jpg
  • Research ecologist, Daniel Fagre Ph.D., on Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0090.jpg
  • Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. The terminal moraine, a pile of gravel rocks created by the leading edge of a glacier that likely disappeared in the 1940's is visible just below the snowfield.
    lgphoto_141007_0088.jpg
  • View of Going to the Sun Road passing below the Garden Wall in Glacier National Park, Montana, Tuesday, October 7, 2014. Going to the Sun Road which goes to Logan Pass and crosses the continental divide is the only road that crosses Glacier National Park and was completed in 1932.
    lgphoto_141007_0066.jpg
  • A tunnel on Going to the Sun Road in Glacier National Park, Montana, in autumn on Tuesday, October 7, 2014. Going to the Sun Road which goes to Logan Pass and crosses the continental divide is the only road that crosses Glacier National Park and was completed in 1932.
    lgphoto_141007_0059.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0202.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0171.jpg
  • A view of the valley and Upper McDonald Creek (center right) as seen from Going to the Sun Road in Glacier National Park, Montana, Tuesday, October 7, 2014. This u-shaped valley was created by a glacier from the ice age that ended 12,000 years ago.
    lgphoto_141007_0248.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0179.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0121.jpg
  • Research ecologist, Daniel Fagre Ph.D., on Hidden Lake Trail heading towards Mount Clements at Logan Pass in Glacier National Park, Montana, Tuesday, October 7, 2014. Fagre and his staff are working on the climate change in mountain ecosystems project which includes looking at what has happened in Glacier National Park since the little ice age ended in 1850.
    lgphoto_141007_0084.jpg
  • Exterior of the United States Geological Survey's Global Change building in Glacier National Park, West Glacier, Montana, on Tuesday, October 7, 2014.
    lgphoto_141007_0042.jpg
  • Hidden Lake Trail is cut through the side of a lateral moraine at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Snow poles are stuck in the ground at the end of season to mark the location of the trails for snow clearing in early summer and show what a snow dominated area Glacier National Park is and that there will be vast changes in the park's ecosystem as the snow continues to diminish.
    lgphoto_141007_0231.jpg
  • A small stream in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0113.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0103.jpg
  • Early morning flight out of Glacier National Airport heading over Hungry Horse Reservoir with views of the Bob Marshall and Great Bear Wilderness and Glacier National Park
    lgphoto_100716_0005.jpg
  • Early morning flight out of Glacier National Airport heading over Hungry Horse Reservoir with views of the Bob Marshall and Great Bear Wilderness and Glacier National Park
    lgphoto_100716_0006.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0177.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0123.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0133.jpg
  • Abstract of surface of Lake Sherburne in Glacier National Park
    lgphoto_120726_0159.jpg
  • A mother and a daughter holding a heart-shaped rock found on a trail in Glacier National Park
    lgphoto_120726_0319.jpg
  • A family taking in the view on the Continental Divide Trail in Glacier National Park
    lgphoto_120726_0242.jpg
  • West Glacier Motel sign at night
    lgphoto_120726_0466.jpg
  • Mother and daughter holding holding hands while hiking in Glacier National Park
    lgphoto_120726_0177.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0208.jpg
  • Dan Fagre Ph.D., a research ecologist with the USGS at the base of Mount Clements at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. Fagre is using repeat photography to document disappearing glaciers using photos taken in the 1880’s (first exploration of this area by people with cameras) and since, and comparing them with the present day images he takes in the exact locations of the historic images to study and document the rate at which glaciers are disappearing.
    lgphoto_141007_0125.jpg
  • View of Glacier National Park from outside the park near East Glacier
    lgphoto_101113_0238.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0139.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0136.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0134.jpg
  • A view from Hidden Lake Trail towards the Garden Wall at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS clumps of sub-alpine fir have gotten thicker and taller in this area due to warming temperatures and changes in snow melt.
    lgphoto_141007_0238.jpg
  • A view from the valley below the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS clumps of sub-alpine fir have gotten thicker and taller in this area due to warming temperatures and changes in snow melt.
    lgphoto_141007_0224.jpg
  • A small stream in the grass in the valley below the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall and that without the water available from melting ice in the late summer a lot of grasses will dry up and be less nutritious.
    lgphoto_141007_0233.jpg
  • Grass in the valley below the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall and that without the water available from melting ice in the late summer a lot of grasses will dry up and be less nutritious.
    lgphoto_141007_0220.jpg
  • A small waterfall in the rock at the base of a snowfield at Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0102.jpg
  • A small waterfall in the rock at the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall.
    lgphoto_141007_0229.jpg
  • Grass in the valley below the base of Mount Clements at Logan Pass, Glacier National Park, Montana, Tuesday, October 7, 2014. According to Dan Fagre Ph.D. of the USGS receding glaciers in the park means that streams dry up in late summer and fall and that without the water available from melting ice in the late summer a lot of grasses will dry up and be less nutritious.
    lgphoto_141007_0219.jpg
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