The Southwest Zone - mineralization is located in the SW part of the BX 1-2 claim, where a porphyritic monzonite/andesite contact coincides with NNE and ENE trending fault zones in a 300 by 700 meter area. Previous work by Redwood Resources in 1987 identified a 49 foot wide zone that assayed 11.19% Cu, 5.44 opt Ag and 0.115 opt Au and occurs in a quartz breccia gangue. This exposure features stockwork and sheeted quartz-magnetite-chalcopyrite with K feldspar/sericite envelopes with minor albite-anhydrite-barite-pink calcite alteration. There is a prominent strong jarosite gossan covering the SW Zone. In 1996, Guardian Resources performed IP geophysics that showed a Y shaped conductor centered on L 1+00 S. Pyrite-magnetite-chalcopyrite-sphalerite-galena sulphide mineralization occurs in quartz veins, quartz breccia and as skarn assemblages along a NNE trending fault zone that appears to splay N and NNW at L 1+00 S. Soil geochemical surveys indicates that in a 100 X 200 m area, anomalous values are >500 ppm Cu, > 200 ppb Au, >1,000 ppm Zn, >200 ppm Pb. The strongly coincident IP geophysics and soil geochemistry will make the SW Zone a primary drill target.