Steven Dutch, Professor Emeritus, Natural and Applied Sciences, University of Wisconsin - Green Bay
In the map above the monument is in yellow and the Sioux Quartzite bluffs are in green.
Definitely one of the more inconspicuous national monuments. | |
The visitor center. The monument preserves outcrops of the Sioux Quartzite along with interbedded clay units that were quarried and carved for ceremonial purposes by the Indians. Indians are still permitted to quarry. | |
The quarries are located in the floor of a broad glacial meltwater channel. The bank of the channel is visible in the distance. Quartzite ledges line parts of the channel bank. | |
Sioux Quartzite outcrop | |
A short trail loop runs from the visitor center to the ledges and back. |
An old flooded quarry pit | |
Rubble from the pit | |
An active pit | |
An exposure of the pipestone, a clay-rich horizon in the quartzite. The pipestone is at the bottom of the outcrop marked by the lower green tablet. | |
Close-up of the pipestone. The quartzite dips a few degrees to the east, so as excavation continues, the pipestone gets deeper. Since all the quarrying was (and is, here) done by hand, the dip of the layers sets a strict limit on quarrying. |
The Sioux is the most extensive of a number of middle Precambrian quartzites of the upper Midwest. Other related units include the Baraboo, Waterloo and Barron quartzites of Wisconsin. All are very pure, generally pink to purple quartzites with abundant cross-bedding. | |
The quartzites are something of a mystery. How did such great thicknesses of pure quartz sand accumulate? How did the rocks get metamorphosed far from any active crustal disturbances? | |
Weathered boulder with cross-bedding | |
Cross-bedding | |
Cross-bedding | |
A boulder showing wind abrasion, pitting and polish. |
Looking southwest from the Visitor Center | |
Looking northeast to the Sioux Quartzite bluffs | |
Large erratics near the monument entrance |
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Created 18 April 2003, Last Update 06 June 2020