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Lauren Grabelle

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Lauren Grabelle

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  • Autumn smoke
    lgphoto_141023_008i.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
  • 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
  • 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
  • Hidden Lake Trail runs along the edge of a lateral moraine at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. The Garden Wall is in the distance.
    lgphoto_141007_0226.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_0222.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
  • 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
  • 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
  • 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_0179.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
  • 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
  • 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_0134.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
  • 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_0085.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
  • Entrance sign to Glacier National Park in West Glacier, Montana, on Tuesday, October 7, 2014.
    lgphoto_141007_0001.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
  • Frost on bare tree branches with mountains behind
    lgphoto_121007_0079.jpg
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  • 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 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
  • 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
  • Sugar on a trail with signs of autums
    lgphoto_130903_004i.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
  • 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
  • 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
  • Daniel Fagre Ph.D. walks along Hidden Lake Trail which runs along the edge of a lateral moraine at Logan Pass, Glacier National Park, Montana , Tuesday, October 7, 2014. The Garden Wall is in the distance.
    lgphoto_141007_0225.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
  • 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
  • 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
  • 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 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 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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_0166.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
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  • 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
  • lgphoto_151103_081i.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
  • 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 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
  • 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
  • lgphoto_171112_061i.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
  • 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 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
  • 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_0223.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
  • 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_0213.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
  • 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
  • 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
  • Wolverine(R) and possibly mountain lion(L) 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_0167.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_0165.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 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
  • 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
  • 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
  • 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
  • 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
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  • lgphoto_161001_0190.jpg
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  • 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
  • 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
  • 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 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
  • 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
  • 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
  • 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
  • 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_0215.jpg
  • A view of the valley below from 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_0190.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
  • Sugar on a trail with signs of autums
    lgphoto_130903_004i.jpg
  • lgphoto_171011_002i-2.jpg
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  • Listening To The Earth
    lgphoto_171005_008i.jpg
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