Baraboo Quartzite
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]
Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.
Uses
[edit | edit source]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
[edit | edit source]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]
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Devil's Doorway rock formation at Devil's Lake State Park -
Chimney Rock
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Boulder field on Eastern bluff at Devil's Lake
References
[edit | edit source]- ^ 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
- ^ a b c Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ Geology by Lightplane Geology.wisc.edu (1923-07-13). Retrieved on 2011-06-05.