LMAO I like this part on page 4 that describes it http://www.dnr.wa.gov/Publications/ger_ofr2004-5_iaml_greatexcelsior.pdf OPENINGS For purposes of clarity, we use the same nomenclature for the underground mine asMoen (1969) and Stoess and Slater (1935). The ore body lies on the west bank of Wells Creek. Slopes in the mine area vary from 50 degrees to vertical. Figures 3 and 4 provide an excellent depiction of the relationship of the various openings to each other.We found the Lower tunnel portal at elevation 1700 feet, approximately 150 feet vertically above Wells Creek. It is completely caved and overgrown. A 1974 letter to G. McKelvey, Homestake Mining Co., quotes claim holder Douglas McFarland as reporting the Lower tunnel to be full of water at the time (R. C. Parker, consultant, written commun., 1974, DGER mine files). A 10-foot-deep gully extends downslope immediately opposite the portal site, indicating that significant quantities of water have discharged in the past. The Lower tunnel was reported caved in 1986 (USFS file). The Blacksmith tunnel portal at elevation 1878 feet is open but unstable (Fig. 5). It lies immediately under the east shoulder of a rudimentary road leading south, approximately 300 yards from the Mill Level tunnel. The Mill Level tunnel is obvious as one approaches the historic mine area, since the portal has been extended beneath colluvium and retimbered circa 1986. It leans to the south, and supporting timbers appear deteriorated.