Results 201 to 210 of about 1,597 (261)

Aeolian accumulation rate within the kettle holes on Skeiðarársandur (S Iceland) under climate warming conditions. [PDF]

Sci Rep
Szafraniec JE.
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... Flora of Glacier National Park, Montana

, 1921
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Succession of Lichens in Front of Retreating Glaciers in Sweden and Norway. [PDF]

Ecol Evol
Halda JP, Košnar J, Lukešová A.
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Pictorial map. Glacier National Park. Waterton Lakes National Park.

, 2014
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Estimation of Glaciers change in the Glacier Bay National Park, Alaska

Estimation of Glaciers change in the Glacier Bay National Park, Alaska
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PROMOTIONAL IMAGERY OF GLACIER NATIONAL PARK*

Geographical Review, 1997
The Great Northern Railway vigorously encouraged visitation to Glacier National Park between 1911 and 1930.
WILLIAM WYCKOFF, LARY M. DILSAVER
exaly   +2 more sources

Grinnell Glacier, Glacier National Park, Montana

Geological Society of America Bulletin, 1939
Stratification due to the annual accumulation of snow is well exhibited in Grinnell Glacier. Layers of snow in the narrow firn zone at the head of the glacier are wedge-shaped and have a steep initial tilt toward the glacier front. Weight of overlying layers forces the earlier-formed layers to rotate so that after travelling a relatively short distance
G. R. GIBSON, J. L. DYSON
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Recession of glaciers in Glacier National Park, Montana

Eos, Transactions American Geophysical Union, 1940
Recent detailed mapping by the National Park Service of several glaciers in Glacier National Park, Montana, has yielded much information about the volume‐shrinkage of these glaciers since the area was mapped by the United States Geological Survey in 1900–02.
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Herpetofauna of Glacier National Park

Northwestern Naturalist, 1997
The current distribution of amphibians and reptiles in Glacier National Park, Montana was documented from museum records and field surveys conducted in 1990 to 1992. Eight species were recorded at 141 sites at elevations from 1000 m to 2300 m. Rana luteiventris was the most common amphibian, occurring parkwide to elevations of 1800 m.
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