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The Baraboo Range is a syncline located in Columbia and Sauk Counties, Wisconsin. It consists 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. The Wisconsin River, previously traveling in a north to south direction, turns to the east just north of the range before making its turn to the west towards the Upper Mississippi River. 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.

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  • Baraboo Range (en)
  • Monts Baraboo (fr)
  • Baraboo Range (nl)
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  • The Baraboo Range is a syncline located in Columbia and Sauk Counties, Wisconsin. It consists 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. The Wisconsin River, previously traveling in a north to south direction, turns to the east just north of the range before making its turn to the west towards the Upper Mississippi River. 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. (en)
  • Les monts Baraboo (Baraboo Range) est un synclinal situé dans le sud de l'état américain du Wisconsin, dans les comtés de Sauk et de Columbia. Ils se composent de roches métamorphiques précambriennes fortement érodées. La chaine est longue d'environ 40 km pour largeur variant de 8 à 16 km. La rivière Wisconsin, qui coulait jusqu'alors du nord au sud, tourne vers l'est juste au nord de la chaîne avant de bifurquer vers l'ouest en direction du Mississippi. L'extrémité orientale de la chaîne a subi la glaciation du Wisconsin, tandis que la moitié ouest non pas et, par conséquent, marque la limite orientale de la (en) (la « zone sans dérive »). (fr)
  • Baraboo Range is een gebergte van het type inselberg gesitueerd in Sauk County en Columbia County in de Amerikaanse staat Wisconsin. Het bestaat uit zeer geërodeerd metamorf gesteente uit het Precambrium. Het gebergte is ongeveer 40 kilometer lang en varieert van 8 tot 16 kilometer in de breedte. De rivier Wisconsin, die voordien van noord naar zuid liep, draait naar het oosten even ten noorden van de Baraboo Range om na de Range naar het westen af te buigen alvorens in de uit te monden. Het oostelijke einde van het gebergte was met ijs bedekt tijdens de ijstijd in Wisconsin en markeerde de oostelijke grens van het , terwijl de westelijke helft niet bedekt was. (nl)
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  • Baraboo Range (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/BarabooRangeFall2010WIS33.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/BarabooRangeWIS78.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/BarabooRangeWinter.jpg
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