SEEPS AND SPRINGS AT A PLATTEVILLE “OBSERVATORY” ON THE RIVER BLUFFS BJ Bonin Independent Contract Geologist, 284 Macalester Street, St. Paul, MN, 55105 USA
[email protected] Greg Brick Department of Earth Sciences, University of Minnesota, Minneapolis, MN, 55455 USA
[email protected] Julia Steenberg Minnesota Geological Survey, 2609 Territorial Road, St. Paul, MN, 55114 USA
[email protected] Abstract teville–Glenwood Shale contact. Overall, the hydro- Residential building construction along the Mississip- stratigraphic attributes of this site are consistent with pi River bluffs in the 1970s created a unique enclosed how the Platteville has been recently characterized in the outcrop of the Late Ordovician Platteville Formation TCM area in a fractured bluff edge setting (Anderson et at Lilydale, Minnesota. This outcrop was examined in al., 2011). early 2013 after a newly-formed spring flooded an el- evator shaft the previous year, drawing attention to the The enclosed outcrop features many seep- and spring- foundation conditions. related mineral deposits. Most notable were the iron- stained flowstone and microgours near the seeps and The Lexington Riverside property is a six story condo- springs along fractures in the limestone, and calcite rafts minium complex constructed within the top of the bluff. on the surfaces of the pools. At some damp locations a A two-level underground parking garage was built into fungal ecosystem has developed. Gypsum beards have the bluff. Bedrock was mechanically excavated to ac- grown in dry portions of the cavern. commodate the construction of the building, creating This man-made cavern, and others nearby, present an unweathered rock surface.