•1,400 x 675 m area of elevated apparent conductivity that is probably attributable to disseminated sulfides. This feature occurs 300-400 m below the surface and occurs at the west end of the southern conductivity ‘Tusk’.
•Occurs on the southwest limb of the Silver Cup Anticline and is associated with a conductive feature (fault) that extends back into the Elephant.
•Also associated with numerous small gossans, iron seeps that suggest the presence of pyrite and other valuable metals in the subsurface.