Steven Dutch, Professor Emeritus, Natural and Applied Sciences, Universityof Wisconsin - Green Bay
What better place to see the middle Precambrian Sioux Quartzite than siouxfalls, South Dakota? Excellent exposures are preserved in Falls Park.
Below: general views of the park | |
Weathered joints in the quartzite. | |
Left and below: the upper falls area. | |
Left and below: the circular marks are probably percussion marks created when fast-moving water slammed large rocks into the quartzite. | |
Left and below: This sort of fluting and polishing looks a lot like wind abrasion, but here it is clearly due to running water. | |
Left and below: Lower Falls Area | |
Left and below: In pioneer days the falls were tapped for water power, as similar falls were in many places, but unlike the wholesale industrial vandalism that destroyed St. Anthony Falls on the Mississippi, here only a part of the water was diverted and the falls were left largely undamaged. Ruins of the mills are preserved in the park. | |
Left: part of a sluice that once carried water to the mills. | |
Left and below: Views of outcrop face | |
Cross-bedding in Sioux Quartzite | |
Ripple marks in Sioux Quartzite | |
Railroad cut in Sioux Quartzite adjacent to Falls Park. | |
Looking north across the broad valley of the Big Sioux River. The Big Sioux River cut downward through soft Pleistocene and Cretaceous deposits until it encountered the resistant Sioux Quartzite. |
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Created 14 July 2003, Last Update 06 June 2020