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Autumn in the Driftless Area of Cross Plains, Wisconsin 43°30′N 91°00′W / 43.5°N 91°W / 43. 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 ...
However, the Dells itself was never covered by glacial ice sheets – it was part of the large Driftless Area that was bypassed by the ice. The melting of the glacier formed Glacial Lake Wisconsin, a lake about the size of Great Salt Lake in Utah and as deep as 150 feet (45 m). The lake was held back by an ice dam of the remaining glacier.
Pages in category "Driftless Area" The following 110 pages are in this category, out of 110 total. ... Dells of the Wisconsin River; Driftless; Driftless Area ...
The geographical regions of Wisconsin [1]. The Western Upland is a geographical region covering much of the western half of the U.S. state of Wisconsin.It stretches from southern Polk County, Wisconsin in the north to the state border with Illinois in the south, and from Rock County in the east to the Mississippi River in the west.
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.
The Wisconsin River dissects the plain here, creating the Wisconsin Dells. East of the river, moraines and small kettle lakes are interspersed throughout the plain. Forests and wetlands mark the northeastern section of the region. For the most part, the Central Plain is a rural area of farmland and forests. Population is sparse.
Dells of the Wisconsin River, May 2002. The lower, westward-flowing portion of the river, between the Baraboo Hills and the Mississippi, is probably the oldest section. Passing through the Driftless Area, it was never covered by a glacier. The western, lower end of the river is narrower than its upstream valley, leading to the suggestion that ...
Professor Lawrence Martin created a schema for dividing Wisconsin into geographical regions in his work "The Physical Geography of Wisconsin". [1] [2] Western Upland; Eastern Ridges and Lowlands; Central Plain; Northern Highland; Lake Superior Lowland; Three of these geographical provinces are uplands and two are lowlands.
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