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Draina_e A extends southeast from thz fan ~rortal. Old-°Z•o~~ th fir <br />• tlu-ives along the north facing slope, and the drainage bottom and sides appear <br />stable. The bottom of the drainage is a broad, heavily vegetated floodplain <br />with braided channels. East~,~~ard (upgradient~ the channels consolidate, and <br />an area exists along the base of the north facing hillside which appears stable <br />and drained ~~~ell enough to pro~-ide a good found, tion for Topsoil storage. A <br />spring exists at the southeast corner of Drainage A. <br />3.3 Svh~ester C=ulch South of Fan Portal <br />About 500 feet south of the fan portal, on the east side of Sylvester <br />Gulch, old-growth aspen and fir indicate a stable regime for construction of a <br />• staging area. The old landslide within the old-grot~-th fir appears to be Hell <br />settled and stable. Smooth contours and good bedrock control above signify <br />slope stability along the eastern side of Sylvester Gulch between Drainage A <br />and the nest drainage to the south. <br />3.4 Drainage B <br />About 2,000 feet south of Drainage A another unnamed drainage, <br />referred to as Drainage B in Figure 1.0, drains into Sylvester Gulch from the <br />east. The confluence area is a grassy pasture that appears stable for <br />construction, provided thatrunoffis controlled. There are several springs near <br /> 5 <br /> <br />is <br />«. <br />:~t.: <br />