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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 ...
Wollersheim Winery grew rapidly and garnered national media attention with the introduction of its Prairie Fumé wine in 1989. [1] In 1990, Wollersheim Winery bought Cedar Creek Winery, located in the Hilgen and Wittenberg Woolen Mill in Cedarburg, Wisconsin. The sister wineries share family ownership and a winemaker, but the two brands are ...
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.
An American Viticultural Area (AVA) is a designated appellation for American wine in the United States distinguishable by geographic, geologic, and climatic features, with boundaries defined by the Alcohol and Tobacco Tax and Trade Bureau (TTB) of the United States Department of the Treasury. [1]
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.
A new hotel is planning to open in Wisconsin Dells next summer, and according to a press release, it "will lean into the state's heritage in a big way, from architecture and interior design to ...
Madeline Heim is a Report for America corps reporter who writes about environmental issues in the Mississippi River watershed and across Wisconsin. Contact her at 920-996-7266 or mheim@gannett.com .
The eastern end of the range was glaciated during the Wisconsinian glaciation, while the western half was not, and consequently, marks the eastern boundary of Wisconsin's Driftless Area. The city of Baraboo is in the center of the valley. The range was designated a National Natural Landmark in 1980. [1]