10 Water Resources in Karst Terranes of the Midwestern U.S.
Thursday, 2 April 2009
1:00 PM - 5:00 PM
SINKS AND RISES OF THE SOUTH BRANCH ROOT RIVER, FILLMORE CO., MN
Paper number: 10-4
Program: Symposia Sessions
Time: 2:10 PM – 2:30 PM
Authors
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Scott C. AlexanderUniversity of Minnesota, Minneapolis, MN
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Andrew J. LuhmannUniversity of Minnesota, Minneapolis, MN
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Cale T. AngerUniversity of Minnesota, Minneapolis, MN
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Jeffrey A. GreenMinnesota Department of Natural Resources, Rochester, MN
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Andrew J. PetersMinnesota Department of Natural Resources, Rochester, MN
Abstract
A series of dye traces over the last 3+ decades have demonstrated that much of the water that sinks from the SBRR resurges in three major spring systems, Seven, Crayfish (MN23:A0080), and Saxifrage (MN23:A0113) Springs. These springs form the head of the perennial flow along a ~0.25 mile reach of the SBRR. The SBRR is a warm water stream above Mystery I, a coldwater stream below Seven Springs and typically dry inbetween.
Mohring (1983) found that water sinking at MN23:B0110 traced both to Seven and to Moth (MN23:A0002) and Grabau (MN23:A003) Springs. Moth and Grabau Springs are the source springs for Forestville Creek, a coldwater stream north of the SBRR in Forestville Twp. Moth and Grabau rise at ~1115 ft from the lower Ordovician Cummingsville Fm. An 18 Nov 2008 dye trace from sink MN23:B0061 found that the dye resurged in Crayfish, Seven and Saxifrage and in Moth and Grabau Springs confirming Mohring's results. Moth and Grabau are about 3.5 miles from B61.
The Sinks of the SBRR feed at least 3 identified springsheds and at least 5 major spring groups that are the source springs for 2 trout streams in 2 different watersheds. In a complex, stage-dependent fashion, Moth and Grabau are pirating flow from the SBRR into Forestville Creek.