Green, Jeffrey AAlexander Jr., E. CalvinAlexander, Scott CLuhmann, Andrew JRunkel, Anthony CPeters, Andrew J2017-03-242017-03-242017https://hdl.handle.net/11299/185358One dye trace in 2007, one dye trace in 2008, and three dye traces in 2010 in Winona County, Minnesota near the town of Rushford. Traces were run to characterize surface-groundwater interactions and to delineate springsheds in the area. Characterizing sinking streams and their connection to springs is important as these springs are critical water sources for trout streams in southeastern Minnesota. A collaborative effort between the Minnesota Department of Natural Resources and the University of Minnesota.Southeastern Minnesota’s karst lands support numerous trout streams. These trout streams are formed by springs discharging from Paleozoic bedrock. Dye tracing has been the tool of choice for mapping the springsheds (karst groundwater basins) that feed these springs. Previous work was focused on the Galena limestone karst. In order to accelerate springshed mapping, a two-year study was funded by the Minnesota Environment and Natural Resources Trust Fund as recommended by the Legislative-Citizen Commission on Minnesota Resources (LCCMR). Across southeastern Minnesota, numerous springs discharge from the Cambrian St. Lawrence formation. The St. Lawrence is considered to be a confining unit under the Minnesota well code. A dye trace was initiated when a stream sink was discovered in the upper St. Lawrence Formation. The sampling points included springs, stream crossings, and a municipal well that may be at risk for surface contamination. Dye was recovered at one spring in less than two weeks and at two other springs in less than three weeks. This translates into travel times of 200-300 meters/day. The springs all discharge from the lower St. Lawrence Formation. The St. Lawrence contains beds of dolostone; the dye trace demonstrates that there is a karst conduit flow component in this formation. This is evidence that these springs are significantly more susceptible to degradation than previously thought.endyetracingtracespringkarsthydrogeologyspringshedsinkholesinking streamdisappearing streamstream sinkgroundwaterconduit flowpseudokarstSt. LawrenceLone RockTunnel CityCambrianWinona CountyRushfordReport