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The welcome sign to Glacier Bay seen by the road entrance. Glacier Bay National Park and Preserve is a national park of the United States located in Southeast Alaska west of Juneau. President Calvin Coolidge proclaimed the area around Glacier Bay a national monument under the Antiquities Act on February 26, 1925. [4]
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Erosional landforms. As the glaciers expand, due to their accumulating weight of snow and ice they crush, abrade, and scour surfaces such as rocks and bedrock.The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys.
Ahern Glacier 5] 8,169 feet (2,490 m) Black and white photo of Grinnell Glacier, Glacier National Park, Montana. Photo by T. J. Hileman ca. 1938. Part of James Willard Schultz Photos and Personal Papers Collection, Montana State University.
A century later glacier retreat has opened a multi-armed bay more than 30 miles long. The tidewater glacier has divided into three independent glaciers, Yahtse, Tsaa and Guyot Glacier. Other examples of glaciers currently in the retreat phase are South Sawyer and Sawyer Glaciers in Alaska, retreating 2.1 and 2.3 km respectively from 1961 to 2005.
Portal:Oregon/DYK/1. Sign at entrance to Stub Stewart State Park...that L. L. "Stub" Stewart State Park (pictured) is the first new full-service state park in Oregon since 1972?
The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of tracking glacier change is comparing photographs of the glacier's position at different times. [2] The form of a glacier terminus is determined by many factors.
The sediment nearer the glacier typically is coarser than non-glacial sediment, ranging from boulders down to sand, but with little silt and clay since the water usually flows too fast to allow these fine particle to settle until it is a considerable distance from the glacier. [20]
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