Baraboo_Quartzite

Baraboo Quartzite

Baraboo Quartzite

Precambrian geological formation in Wisconsin

Baraboo Quartzite is a Precambrian geological formation[1] of quartzite, found in the region of Baraboo, Wisconsin. While pure quartzite is usually white or gray, Baraboo Quartzite is typically dark purple to maroon in color, due to the presence of iron (hematite) and other impurities.[2] Baraboo Quartzite may display strata created by progressive deposition of layers of sand in the original sandstone from which the quartzite was formed (through metamorphism).[2] Specimens of Baraboo quartzite may also display ripple marks that appear visually similar to the patterns one might see in the sand at a beach. Ripples indicate that the sandstone from which the quartzite was metamorphosed was originally water-laid sediment.[2]

A Baraboo Quartzite sample, in breccia form. The brecciated purple portions are quartzite, and the matrix is white quartz
A sample of Baraboo Quartzite.

Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.

Uses

Quartzite is a decorative stone and may be used to cover walls, as roofing tiles, as flooring, and stairsteps. Crushed quartzite is sometimes used in road construction. Baraboo Quartzite is commonly mined for use as railroad ballast.

Occurrences

Formations of quartzite can be found throughout the Baraboo Hills in south-central Wisconsin. Many notable formations can be seen in Devil's Lake State Park.[3]

  • Devil's Doorway rock formation at Devil's Lake State Park
  • Chimney Rock
  • Boulder field on Eastern bluff at Devil's Lake

References

  1. [1]
    Hanson, G. F., Geology of the Barabou District, Wisconsin Archived February 22, 2014, at the Wayback Machine, The University of Wisconsin Extension, 1970, Information Circular 14
  2. [2]
    Montgomery, Keith. "Baraboo Quartzite". Archived from the original on 2010-09-20. Retrieved 2013-10-14.
  3. [3]
    Geology by Lightplane Geology.wisc.edu (1923-07-13). Retrieved on 2011-06-05.
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