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Baraboo Range in winter Looking east down the range on Wisconsin Highway 78. The Baraboo Range is a mountain range in Columbia County and Sauk County, Wisconsin. Geologically, it is a syncline fold consisting of highly eroded Precambrian metamorphic rock. It is about 25 miles (40 km) long and varies from 5 to 10 miles (16 km) in width.
Keating's report on the 1823 Long expedition included a "Map of the country embracing the route of the expedition of 1823 commanded by Major S.H. Long". The name Ocooch is placed on this map approximately where the Baraboo Hills are located. Hachures extend the range to the north and northwest, but the implication is that the name Ocooch ...
Devil's Lake State Park is a state park located in the Baraboo Range in eastern Sauk County, just south of Baraboo, Wisconsin.It is around thirty-five miles northwest of Madison, and is on the western edge of the last ice-sheet deposited during the Wisconsin glaciation. [2]
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.
Point of Rocks is a geologically significant outcropping located along U.S. Route 12 (US 12) in the Town of Baraboo in Sauk County, Wisconsin, United States, southwest of the city of Baraboo. The formation is made up of Baraboo Quartzite and is part of the Baraboo Range ; it dates from the Precambrian and is roughly 1.7 billion years old.
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Blue Mound State Park is a state park in Wisconsin, United States, located atop the largest hill in the southern half of the state, near the village of Blue Mounds.The 1,153-acre (467 ha) park features a pair of observation towers affording views of the Wisconsin River valley and Baraboo Range to the north, the mounds, buttes, and rolling forests of the Driftless Area to the south and west ...
The park is on the edge of the Baraboo Range in an unglaciated Driftless Area of south-central Wisconsin. Outcrops of quartzite, hardened sand deposited about 1.6 billion years ago jut out of the tops of these hills. The arch and rock shelter have been weathered out of one such outcropping. The top of the arch is 35 feet (11 m) above the ground.