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Brule Glacial Spillway is a Wisconsin Department of Natural Resources-designated State Natural Area that encompasses the valley of the upper reaches of the Bois Brule River. This valley was carved by the outlet of Glacial Lake Duluth , which occupied what is now the western portion of Lake Superior , during the retreat of the Superior lobe of ...
The state park system in Wisconsin includes both state parks and state recreation areas. Wisconsin currently has 51 state park units, covering more than 60,570 acres (245.1 km 2) in state parks and state recreation areas.
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The Ice Age National Scientific Reserve is an affiliated area of the National Park System of the United States comprising nine sites in Wisconsin that preserve geological evidence of glaciation. To protect the scientific and scenic value of the landforms, the U.S. Congress authorized the creation of a cooperative reserve in 1964.
The state park encompasses 9,217 acres (3,730 ha), [3] making it the largest in Wisconsin. [4] The state park is known for its 500-foot-high (150 m) quartzite bluffs along the 360-acre (150 ha) Devil's Lake , which was created by a glacier depositing terminal moraines that plugged the north and south ends of the gap in the bluffs during the ...
The Ice Age Trail is a National Scenic Trail stretching 1,200 miles (1,900 km) in the state of Wisconsin in the United States. [1] [2] The trail is administered by the National Park Service, [3] and is constructed and maintained by private and public agencies including the Ice Age Trail Alliance, a non-profit and member-volunteer based organization with local chapters. [4]
The peak of a glacial horn will often outlast the arêtes on its flanks. [1] As the rock around it erodes, the horn gains in prominence. Eventually, a glacial horn will have near vertical faces on all sides. [citation needed] In the Alps, "horn" is also the name of very exposed peaks with slope inclinations of 45-60° (e.g. Kitzbüheler Horn).
Till plains are large flat or gently sloping areas of land on which glacial till has been deposited from a melted glacier. In some areas, these depositions can be up to hundreds of feet thick. The morphology of the till plain is generally reflective of the topography of the bedrock below the glacier. Another term for till plain is ground moraine.
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