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<br />Spring 5-23 is located at the headwaters of the 006 Gulch, in an <br />ephemeral stream channel, This spring is upstream of mining and should <br />not be affected by mining. The EC plot indicated an increasing trend. <br />Spring 5-41 is located downstream of Spring 5-23 in the 006 Gulch stream <br />channel. It was located just downstream of the silted-in Temple Pond #2. <br />This spring was buried in spoils in 1998. <br />Spring 5-46 {a.k.a., the Olson Spring) is not a flowing spring, but a <br />three-foot diameter well placed in the alluvium of Dry Creek. Since a <br />well was drilled on the Olson ranch in September 1980, this "spring" has <br />not been put to use, although it is water-righted for stock use. The EC <br />plot indicates a decreasing trend. <br />Spring S-46 is a developed spring first monitoring during the 1979 <br />spring survey. This spring became part of the required monitoring <br />program in 2000. It is located immediately below the 005 Pond. The EC <br />plot indicates an increasing trend. <br />Spring 5-47 was first discovered by SCC personal in 1989 and was <br />monitored first in June 1990. It is a developed spring existing <br />alongside the mine entrance haul road just to the west of the Seneca II- <br />W Meteorological Station. This spring became part of the required <br />monitoring program in 2000. Its EC plot indicates a decreasing trend. <br />Spring 5-48, a.k.a. the Flanders Spring, is located just upstream of the <br />009 Pond. This spring became part of the required monitoring program in <br />2000. The EC plot indicates a increasing trend. <br />Spring 5-49 was located in the II-W South area just upstream of the <br />NPDES 016 pond. It was a developed spring that flows into a metal stock <br />tank. It was first sampled in August 1997. It was abandoned in August <br />2001 prior to being mined out. <br />~I <br />18 <br />