Holes WC-22 and 23 were drilled due south instead of due east to intersect the sulphide breccia dike
discovered in hole WC-13, as well as other easterly trending mineralized structures that would have been missed by east-directed holes.
Of particular note is a previously unknown sulphide-matrix breccia dike
beginning at 125 meters that averages 1.
The area surrounding the mineral properties has breccia zones, breccia dikes
and quartz veins, which stretches to the southeast and is said to contain not only gold but significant quantities of silver as well.
The mineralization occurs in dacites and dacite porphyries intruding a fine grain granite and is associated with breccia dikes
, crackle breccias and stockwork veining.