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Lauren Grabelle

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Lauren Grabelle

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  • 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
  • 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
  • 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
  • Big horn sheep standing in a handicap parking space at Logan Pass Visitor Center in Glacier National Park
    lgphoto_120726_0409.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
  • 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
  • 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
  • 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
  • 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
  • Rear view of a male big horn sheep on Going To the Sun Road at Logan Pass in Glacier National Park
    lgphoto_120726_0440.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
  • 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
  • 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_0094.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
  • 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
  • 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
  • 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
  • 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
  • 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
  • Amish couples from Lancaster County Pennsylvania hiking Hidden Lake trail and Logan Pass at Glacier National Park
    lgphoto_120727_0730.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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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 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 mountains and clouds looking east from Logan Pass and Hidden Lake Trail
    lgphoto_120727_0482.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 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • Amish couples from Lancaster County Pennsylvania hiking Hidden Lake trail and Logan Pass at Glacier National Park
    lgphoto_120727_0735.jpg
  • Abstract view of Hidden Lake from the Hidden Lake overlook in Glacier National Park
    lgphoto_120727_0633.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
  • Two mountain goat grazing above Hidden Lake in Glacier National Park
    lgphoto_120727_0653.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
  • lgphoto_120727_0619.jpg
  • lgphoto_120727_0716.jpg
  • lgphoto_120727_0616.jpg
  • View of Going to the Sun Road and The Loop
    lgphoto_120630_0141.jpg
  • - HIdden Lake Trail
    lgphoto_120630_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
  • 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
  • lgphoto_120727_0664.jpg
  • lgphoto_120727_0489.jpg
  • Mountain goat standing on a rocky outcropping around a snow field on Hidden Lake Trail in Glacier National Park
    lgphoto_120727_0686.jpg
  • lgphoto_120727_0642.jpg
  • Going to the Sun Mountain from HIdden Lake Trail
    lgphoto_120630_0240.jpg
  • Going to the Sun Mountain from HIdden Lake Trail
    lgphoto_120630_0236.jpg
  • Abstract of melting snow and ski tracks on HIdden Lake Trail
    lgphoto_120630_0227.jpg
  • - HIdden Lake Trail
    lgphoto_120630_0274.jpg
  • Abstract of melting snow on HIdden Lake Trail
    lgphoto_120630_0220.jpg
  • lgphoto_120726_0439.jpg
  • - HIdden Lake Trail
    lgphoto_120630_0243.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
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