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National Geologic Map Database
Geologic Unit: Freedom
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Map showing publication footprint
  • Usage in publication:
    • Freedom formation
  • Modifications:
    • Named
  • Dominant lithology:
    • Dolomite
    • Iron-formation
  • AAPG geologic province:
    • Wisconsin arch
Publication:

Weidman, Samuel, 1904, The Baraboo iron-bearing district of Wisconsin: Wisconsin Geological and Natural History Survey Bulletin, no. 13, 190 p.


Summary:

Freedom formation described in south-central WI. Upper part consists 500 ft of dolomite. Lower part is 450 to 500 ft of iron ore, ferruginous slates, ferruginous dolomite and ferruginous chert. Appears to grade into underlying Seeley slate and to lie unconformably below Potsdam sandstone. Does not outcrop. Found only by exploration southwest of North Freedom. Is known to cover 5 or 6 sq mi in secs. 2, 3, 9, 10, 11, 15, 16, and 20 of town of Freedom. Assigned to Precambrian.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Freedom Formation
  • Modifications:
    • Overview
  • Dominant lithology:
    • Hematite
    • Dolomite
    • Chert
  • AAPG geologic province:
    • Wisconsin arch
Publication:

Clayton, Lee, and Attig, J.W., 1990, Geology of Sauk County, Wisconsin; With a section about the Precambrian geology by B.A. Brown and an appendix naming the Rountree Formation by J.C. Knox, D.S. Leigh, and T.A. Frolking: Wisconsin Geological and Natural History Survey Information Circular, IC 67, 68 p., (incl. geologic map, scale 1:100,000)


Summary:

Freedom Formation known only from descriptions of mines and iron-exploration cores made early 1900's. No outcrops known, though cross section by Weidman (1904) shows exposure in railroad cut at Illinois Mine. Lower unit consists of hard and soft hematite, layered hematite and chert, granular hematite and chert, and mixed chert and carbonate with quartz, clay minerals, and iron silicates. Upper part of the formation consists largely of dolomite. Interbedded phyllite in lower part indicates that contact with the Seeley is gradational.

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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