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Ms. Christine E. Johnston <br />1992 AHR Response <br />August 25, 1994 <br />Page 2 <br />3. The North Fork upper station is monitored for flow. This is the location of the USGS gaging station which <br />is also monitored for water quality. Early in the monitoring program, it was determined that only one Flow <br />station on the North Fork was necessary since the impact of the mine on river Flows would be negligible. <br />However, water quality is monitored at the lower monitoring station since there could be measurable effects <br />from mining operations. <br />4. Only one point was measured in late February, late May and late July at the Sylvester Gulch station <br />ranging in flow from 0.1 to 0 efs. Even though these measurements exhibit a decrease in Flow during the <br />spring snow melt, the runoff peak was probably missed between the February and May measurements <br />because of the operational problems with the Flume being clogged with debris and/or overtopping the <br />capacity of the flume. Comparison of daily Flows from acomparably-sized drainage at the Lick Creek <br />flume, indicates that the peak flow was earlier during the month of May. As a result, flows on Sylvester <br />Gulch appear to be appropriate for the season during which they were collected given the fact that the flows <br />could vary considerably from day to day during storm water runoff events or warm periods which would <br />increase Flow due to snow melt. The data from well GP-I indicates that the alluvial water table was at its <br />peak during the measurement made during May. This is also appropriate for the season of the year. <br />Subsequent comparison of this data should confirm this relationship. <br />5. Flow information will be incorporated with the surface water quality information found in Appendix D in <br />future AHRs. Flow information from the samples acquired from the sediment ponds is not easily acquired. <br />MCC monitors the total volume of discharges using flow gauges nn the discharge, but not the rate of <br />discharge. The amount of water discharging from the end of the pipe typically exceeds the staffs <br />capability to measure it. MCC will provide a Flow value in future AHRs based on a calculation derived <br />from the quotient of the volume discharged and the lima period that the gate was open. <br />SPRINGS: <br />Data from field parameters indicated that some values were outside the minimum and maximum range. <br />Samples sent to the laboratory require 20 l0 30 days to receive results and if a second sample were taken <br />at [hat point in time, it would not correlate [o the prescribed sampling window or other samples previously <br />obtained. As a result, MCC has applied for a revision to the plan to eliminate this second sampling <br />requirement. <br />MCC does not have an explanation as to why the minimum and maximum values were exceeded. <br />GROUNDWATER: <br />Page 8 of the AHR states "Some groundwater wells exhibited slightly changed conditions ...". The <br />paragraph goes on to say "Most notably, the 1992 data indicates:" and nine (9) bullet items are discussed. <br />These bullet items are the "changed conditions". <br />2. An error was made during data entry for water levels in well SOM 3g-H2. The hydrographs have been <br />corrected and attached for replacement in the 1992 and 1993 AHRs. <br />3. On a yearly basis, MCC will measure the total depth of each well. The measurements along with any <br />appropriate actions will be included in [he AHR. <br />