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Lauren Grabelle

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Lauren Grabelle

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  • Mysterious ice circles on Swan River
    1128101457a.jpg
  • lgphoto_140119_088i.jpg
  • Sugar on the shore of Estes Lake
    lgphoto_130313_032i.jpg
  • North shore of Flathead Lake
    lgphoto_101227_0008.jpg
  • lgphoto_170228_0077.jpg
  • Dockstader Island Bridge under construction on the north shore of Flathead Lake
    lgphoto_141227_041i_neg.jpg
  • Dowden Health Media<br />
Monmouth Health & Life<br />
Gourment: Doris & Ed's
    DE5.jpg
  • Dowden Health Media<br />
Monmouth Health & Life<br />
Gourment: Doris & Ed's
    DE4.jpg
  • Sugar on the shore of Estes Lake
    lgphoto_130313_032i.jpg
  • North shore of Flathead Lake
    lgphoto_101227_0008.jpg
  • lgphoto_170228_0069.jpg
  • North shore of Flathead Lake
    lgphoto_101227_0008.jpg
  • lgphoto_160119_002i.jpg
  • Dockstader Island Bridge under construction on the north shore of Flathead Lake
    lgphoto_141227_041i_neg.jpg
  • Going to the Sun Mountain from HIdden Lake Trail
    lgphoto_120630_0236.jpg
  • 1993
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  • Ice Palace Bird (snow) from the series Listening To The Earth
    lgphoto_180130_006i.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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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 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
  • 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
  • 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 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
  • 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 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
  • 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
  • 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_0084.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
  • 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
  • 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
  • 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
  • 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 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