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The geology of Wisconsin includes Precambrian crystalline basement rock over three billion years old. A widespread marine environment during the Paleozoic flooded the region, depositing sedimentary rocks which cover most of the center and south of the state.
As of the 2020 census, Wisconsin had a population of 5,893,718, and ranked 27th in the United States in population density. [9] [10] The center of population is located in Green Lake County, in the city of Markesan. [11] Wisconsin is divided into 72 counties, and has 190 cities, 407 villages, and 1250 towns. [12]
Where the Wisconsin River turns west to join the Mississippi, the area to the south, including the whole of Grant County as well as most of Lafayette County, are part of the Driftless Area. The rugged terrain comprising most of the Driftless Area is distinct from the rest of Wisconsin, and is known locally as the Coulee Region. The steep ridges ...
Kettle Moraine is a large moraine in the state of Wisconsin, United States. It stretches from Walworth County in the south to Kewaunee County in the north. It has also been referred to as the Kettle Range and, in geological texts, as the Kettle Interlobate Moraine .
Pages in category "Geology of Wisconsin" The following 19 pages are in this category, out of 19 total. This list may not reflect recent changes. ...
[8]: 1 Penokean-age rocks in the northern Wisconsin and the Upper Peninsula of Michigan contain areas of low-pressure, low- to high-temperature metamorphism. [ 8 ] : 3 The folding and metamorphism increased in intensity to the south and southeast, [ 8 ] : 1 and produced the isolated gneissic 1,755-million-year-old [ 2 ] : 342 Watersmeet Domes ...
The Wisconsin glaciation extended from about 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred about 25,000–21,000 years ago during the last glacial maximum, also known as the Late Wisconsin in North America. The Last Glacial Period caused a much lower global ...
The viewing of the rock formations by water is a tourist attraction in the area. The nearby city of Wisconsin Dells is the center of summer tourist activity, much of it in the form of the theme parks unrelated to the river features. The Dells of the Wisconsin River is owned by the Wisconsin Department of Natural Resources.