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1911 map showing extent of the Driftless Area as well as the Driftless region in Minnesota and Iowa Typical terrain of the Driftless Area as viewed from Wildcat Mountain State Park in Vernon County, Wisconsin Glacial map of the Great Lakes region; the dark area near left center was not covered by drift. Areas with diagonal hatching were ...
Glacial Lake Wisconsin 20,000 years ago with modern counties for geographical context. Glacial Lake Wisconsin was a prehistoric proglacial lake that existed from approximately 18,000 to 14,000 years ago, at the end of the last ice age , in the central part of present-day Wisconsin in the United States .
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 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]
One dramatic example is Wildcat Mountain State Park. The Baraboo Range anchors the eastern edge where the Wisconsin River turns and runs through the area to the Mississippi River. The Baraboo Range is a monadnock in Sauk and Columbia Counties and a National Natural Landmark formed 1.6 billion years ago featuring Devil's Lake, an endorheic lake.
Contains unusual steep sandstone bluffs that formed as islands in Glacial Lake Wisconsin. [42] Mirror Lake State Park: Sauk: 2,179 882 1962 Mirror Lake Surrounds a reservoir whose wooded shores and 50-foot (15 m) cliffs often keep the water mirror-smooth. [43] The Seth Peterson Cottage designed by Frank Lloyd Wright is on the NRHP. Natural ...
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[3]: 40–75 The Early Wisconsin was the bigger of the two and extended farther west and south. It retreated an unknown distance before halting. During this period of quiet, the glacial deposits were eroded and weathered. This first Wisconsin period erased all the Illinoian glacial topography that its glaciers extended over. [3]
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