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rutting has occurred but does not significantly affect drainage or cause erosional issues at <br /> this time. Periodic grading should easily restore the road surface. The road was travelled to <br /> a point near permanent Pond B. <br /> Hydrologic Balance <br /> Permanent Pond F (at right) was dry. <br /> The embankment appeared normal with <br /> no sign of borrows or damage of any <br /> kind. This pond is an excellent addition <br /> to the post-mining landscape, providing <br /> a seasonal source of water for livestock <br /> and wildlife. The sediment baffle is no <br /> longer necessary and the operator <br /> should consider removing it from the <br /> pond prior to final bond release. <br /> Pond D held a moderate amount of <br /> water but was not discharging. <br /> Traditionally, this pond seems to contain rwpa_* : <br /> water on a year-round basis. A natural <br /> spring exists in the headwaters of the <br /> Pond D watershed on the steep slope <br /> that rises to the west. The spring was Liiii <br /> visited and found wet and active. Mostflow percolates into the subsurface a <br /> short distance from this spring. It <br /> appears to be an important source of <br /> water to local wildlife. Mining appears to <br /> have had no long-term affect on this <br /> spring. <br /> Spoil well SP-01 remains un-reclaimed at this time. <br /> The well was found capped and locked (shown below <br /> right). The permanent drainage in the pre-1986 <br /> reclaimed area (below left) shows minimal downcutting, <br /> strongly suggesting long-term stability over the last 20- <br /> 25 years. <br /> 4 <br />