Kirk Main Zone (West Ridge) - approx. 15 minor and 2 major quartz-sulphide showings are exposed as quartz-carbonate fissure veins adjacent to salmon coloured K feldspar dykes in a 200 X 400 m area. The quartz-carbonate veins contain pyrite-chalcopyrite-galena-sphalerite-tetrahedrite- bismuth tellurides. Skarn mineralization is hosted by marble (dolomitic) which is partly brecciated and is in close proximity to quartz-carbonate fissure veins. The skarn minerals consist of magnetite-pyrite-chalcopyrite-azurite -epidote -garnet-pyroxene-chlorite-feldspar-lizardite -carbonate. IP geophysics over the Kirk Main Zone identified eight parallel chargeability anomalies, suggesting layering or crudely stratiform mineralization. A strong mag high in the north portion of the Kirk Main Zone correlates with increased magnetite along the main conductor axis (located 50 m. west of and parallel to the baseline), however gold values in soil geochemistry increase in the south portion of the Kirk Main where a prominent mag low reflects increased alteration (i.e. saussauritized country rock). The south west area has a 0.8 m wide quartz-sulphide vein which returned an assay value of 22. 4 g/t Au (0.653 opt Au). In the north end a 0.5 m wide quartz-sulphide vein assayed 40.9 g/t Au (1.193 opt Au).