The potential to find additional mineralization at and along strike of the Zinc Zone is considered excellent. Additional areas have been identified along a 20 km belt of prospective rocks west of the Zinc Zone. To date, the areas with greatest potential are outlined below:

• Zinc Zone: on-strike and down dip of the present Zinc Zone where zinc-silver mineralization continues outside the known area of the historic resource;

• FIII Rhyolite Showing: a felsic volcanic package located 0.7 km west of the Zinc Zone depleted in TiO2 and enriched in SiO2;

• Easy Lake Showing: Rockcliff’s staking crew identified a potential area with hydrothermally altered, pyritized, quartz sericite schist east of Easey Lake located ~ 6.0 km west of the Zinc Zone;

• Butler Creek Showing: extensive hydrothermally altered felsic rocks associated with shearing, pyrite, sericite and silica are located ~ 4.0 km west of the Zinc Zone;

• Moorehouse Lake Sediment Zn Anomalies: numerous lake sediment zinc anomalies in the Moorehouse Lake area located ~ 12.0 km west of the Zinc Zone;

• Easey Lake Conductor: A strong, extensive conductor northwest of Easey Lake identified by historic air and surface geophysics;

• Airborne Conductors: numerous untested airborne EM and Magnetometer anomalies identified by the OGS in 1987-88 located throughout the property;

• Felsic Rocks: limited historical reconnaissance mapping over small tracts of land in Rennie, Meath and Glasgow townships by Noranda (1984) and others outlined several areas with felsic volcanic rocks located up to 15 km west of the Zinc Zone.

Shihan Gold Potential

Additional areas on the property have been identified as structurally controlled gold-silver-copper mineralization. At least two auriferous zones located south of the Zinc Zone cross-cut stratigraphy and remain open in all directions. Drill results yielded intersections from anomalous up to 30 g/t gold over widths of up to 1.5 metres.