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Also on the Canadian side and entering the lower Stikine, like the Great Glacier, are the Mud and Flood Glaciers, which form the boundaries of the small Boundary Range, which is an eastern abutment of the range comprising the Stikine Icecap and marks the approximate boundary claimed by the United States prior to the Alaska Boundary Settlement ...
Matanuska Glacier is a valley glacier in the US state of Alaska. At 27 miles (43 km) long by 4 miles (6.4 km) wide, it is the largest glacier accessible by car in the United States. Its terminus feeds the Matanuska River. [2] It lies near the Glenn Highway about 100 miles (160 km) northeast of Anchorage in Glacier View. The glacier flows about ...
In the peaks of Glacier Bay are Alpine tundra, glaciers and ice fields. [29] Regions of the park closest to the Gulf of Alaska have a relatively mild climate with significant rainfall and comparatively low snowfall. Lower Glacier Bay is a transitional zone, and upper Glacier Bay is cold and snowy.
The glacier's activity is constant, and seeing 10-story-high icebergs calve into the water is unforgettable. College Fjord is a worthy grand finale. There are five tidewater glaciers in the fjord ...
Glacier View is located in the eastern part of Matanuska-Susitna Borough at (61.818532, -147.714741 It is bordered to the east by the Eureka Roadhouse CDP and to the west by the Chickaloon CDP. It is on the north side of the valley of the Matanuska River , along Alaska Route 1 , the Glenn Highway, which leads west 60 miles (97 km) to Palmer and ...
The Malaspina Glacier (Tlingit: Sít' Tlein) in southeastern Alaska is the largest piedmont glacier in the world. Situated at the head of the Alaska Panhandle, it is about 65 km (40 mi) wide and 45 km (28 mi) long, with an area of some 3,900 km 2 (1,500 sq mi), [1] approximately the same size as the state of Rhode Island.
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