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• Most of the culverts and outlet sediment control structures along Road "J" are in need of <br /> maintenance, due to erosion and siltation from the recent heavy rains. <br /> • The southern-most corner segment of former Road "K", which was reclaimed and seeded last fall <br /> appears to be stable, and seeded grasses have recently germinated. <br /> Hydrologic Balance <br /> Sediment Ponds 005, 006, 016, 016A, and 017 were inspected, and appeared to be functioning properly, with <br /> disturbed area runoff properly directed into the ponds. Sediment Ponds 009 and 015, in the Sage Creek <br /> watershed were not inspected. Stock ponds in the 005, 006, and 007 watersheds were observed; all held water <br /> close to pond capacity and embankments appeared stable. Stock Ponds T-26 and T-27 in the upper 016 <br /> watershed could not be accessed. Previously documented mine area springs and seeps were actively flowing; <br /> no previously un-documented springs were noted. The following observations regarding ponds and springs <br /> were recorded: <br /> • The sediment ponds observed were all discharging clear flow. <br /> • A significant quantity of sediment, including riprap washed down from eroded permanent channels had <br /> been deposited in Pond 016A. <br /> • Movement along the toe of the"Pond 16 Slide", which previously damaged Road "J"adjacent to the <br /> pond, has impacted the riprap channel between Ponds 016 and 016A. Ground movement, and possibly <br /> also heavy flow during the recent runoff event has resulted in constriction of the channel and <br /> displacement and mounding of the riprap. Channel repair will be warranted in association with the <br /> slide remediation plan to be developed this year. <br /> • The riprapped inlet to Stock Pond T-20 was eroded along a 25 segment, and repairs are <br /> warranted. <br /> Backfilling and Grading <br /> Slides and Damage <br /> There are three areas of significant slope instability that warrant advisement from geotechnical consultants with <br /> regard to development of remediaton plans, to be submitted this year. These locations are the-"Pond 016"and <br /> adjacent"Shrub Plot" slides, which have been detailed in recent inspection reports, and a slide that was repaired <br /> several years ago on a slope south of the upper segment of 006 Gulch. These slides are delineated on the 2009 <br /> R&G map, and the operator has contracted the services of a geotechnical consultant to develop remediation <br /> plans. Geotechnical investigations for these slides were initiated last summer, to continue through this spring, <br /> with remediation plans to be developed and completed following completion of the investigation. The slides in <br /> the lower 016 watershed are described in previous inspection reports and in the Hydrologic Balance section of <br /> this report(new movement evident along the toe of the"Pond 016" slide this year). The repaired slide in the <br /> upper 006 Gulch watershed has reinitiated movement this spring, exhibiting a new scarp up to 80 yards in length <br /> and two feet high along the upper slope, with a parallel toe bulge below. Detailed remedialtion plans for these <br /> slide locations will need to be submitted by July 30, 2009. <br /> There are a number of additional cracks and minor scarps on steep reclaimed spoil and highwall slopes <br /> that have developed or re-opened this spring, and will require repair. Most of these various locations are <br /> properly delineated on the 2009 R&G map. One settling crack not indicated on the map was observed <br /> (from a distance)along the former highwall in the upper 017 watershed. <br /> Hillslope Erosion <br /> A significant number of hillslope erosional features were observed during this and the previous inspection, most <br /> of which are properly marked for repair on the 2009 R&G Map. The following hillslope rills and gullies were not <br /> marked on the map, but will require stabilization: <br /> • Numerous rills paralleling the TRM channel north of the aspen test plots; hand cut water bars may be <br /> appropriate to direct flow into the channel. A hillslope gully 12"-14" deep enters this channel from the <br /> south, approximately 150' upstream from upper end of TRM segment. <br /> 4 <br />