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Autumn in the Driftless Area of Cross Plains, Wisconsin. The Driftless Area, also known as Bluff Country and the Paleozoic Plateau, is a topographical and cultural region in the Midwestern United States [1] that comprises southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and the extreme northwestern corner of Illinois.
High Cliff State Park is a 1,187-acre (480 ha) Wisconsin state park near Sherwood, Wisconsin.It is the only state-owned recreation area located on Lake Winnebago. [2] The park got its name from cliffs of the Niagara Escarpment, a land formation east of the shore of Lake Winnebago that stretches north through northeast Wisconsin, Upper Michigan, and Ontario to Niagara Falls and New York State.
Ocooch Mountains are a place name for the Western Upland area of Wisconsin also known as the Driftless Region, meaning un-glaciated, lacking glacial drift or the Paleozoic Plateau, referring to a geologic era, Greek for "ancient life". The lack of glaciated terrain accounts for high hills, bluffs, and ridges.
State Trail. Estimated Users. Busiest Month. Glacial Drumlin State Trail East. 239,219. October (28,370) Military Ridge State Trail. 206,300. July (37,000) Badger ...
The state park also includes the 500-foot-high (150 m) quartzite bluffs surrounding the lake, and 11 miles (18 km) of the Ice Age Trail. [54] Interstate State Park consists of two adjacent state parks on the Minnesota–Wisconsin border. The Wisconsin side covers 1,330 acres (5.4 km 2), and the Minnesota side covers 298 acres (1.21 km 2).
Great River State Trail: 1985 Onalaska-Marshland La Crosse, Trempeleau: DNR Yes Rail Trail 24 Great Sauk State Trail: 2017 Sauk City - Sumpter Sauk, Juneau County Yes Rail Trail 5 Green Circle State Trail: 1992 Stevens Point area (local) Portage: County No Local Trail 31 Hank Aaron State Trail: 1996 Milwaukee-West Allis Milwaukee: DNR No Rail ...
Escarpment face of a cuesta, broken by a fault, overlooking Trenton, Cloudland Canyon State Park, and Lookout Mountain in the U.S. state of Georgia. An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations.
The cliffs along the escarpment are primarily formed by the early Silurian Mayville Dolostone; the rocks that make up the escarpment were deposited within the Michigan Basin. Continued subsidence of this basin during deposition meant that many of the rock layers in eastern Wisconsin have been tilted towards the east. [2]