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Geological Formation

Baraboo Range

Hill and Mountain Ranges

The Baraboo Range is a horseshoe-shaped ridge of Precambrian quartzite in south central Wisconsin, its rock formed from sediment deposited in a shallow sea some 1.7 billion years ago before being metamorphosed, folded into a syncline and uplifted, then left standing as far younger surrounding rock eroded away around it over an immense span of geologic time. The range extends about 25 miles across Columbia and Sauk counties, with the city of Baraboo sitting in its central valley, and its eastern half was overridden by the last continental ice sheet while its unglaciated western half marks the edge of Wisconsin's Driftless Area. It was designated a National Natural Landmark in 1980.

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Caused By

Weathering, Processes

Wikidata P31 formation-type mapped to formative process Weathering via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Baraboo Range

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Baraboo Range
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Baraboo Range
Sources
1. Wikidata: Baraboo Range
  • Wikidata Q2147674, class allow-list match (w-wdresolver-0926)
  • Wikidata P1435 heritage-designation or P3425 Natura 2000 claim on the formation's own item (w-bbfill-earth2-0926)
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Baraboo Range (Wikipedia)
In Group: Mountain Ranges and Hill Ranges, Lead sentence
Quote, In Group: Mountain Ranges and Hill Ranges, Lead sentence
The Baraboo Range is a mountain range in Columbia County and Sauk County, Wisconsin.
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