The Snow Property, in part, was previously held under option by Snowfield from 1997 until 2008 but was relinquished due to a Province of British Columbia government of the day moratorium on exploration in the area for several years followed by a further exploration permit moratorium arising from Aboriginal Land Claim Negotiations between the Province of British Columbia and the Hawiih of the First Nations with respect to the Clayoquot Land Use Decision Area adjacent to the area where the Snow Property is located.

These issues have since been resolved and exploration in the area resumes under the normal protocols.

Under its previous option tenure of the Snow Property, the Company expended a total of $290,334 on programs
of exploration on the Property.

The Snow property is situated between the Taylor and Kennedy rivers west of Sproat Lake on Vancouver Island, approx. 45 kilometers west of the town of Port Alberni. The Sutton Creek logging road on the south side of the Taylor River provides two-wheel drive access to the centre of the property.

The dominant structures of the Snow property are steeply-dipping, northwesterly-striking extensional faults. These structures appear to have controlled the emplacement of the felsic dykes along with quartz sulphide veins and veinlets which may be related to the felsic dykes hosted in Karmutzen volcanics. Gold mineralization within the Snow property is associated with pyrite, galena, sphalerite and chalcopyrite in quartz or quartz-carbonated veins. Vein textures are indicative of open space filling. A petrographic study indicated the presence of carbonate and epidote with the quartz gangue and native gold as thread-like veinlets and inclusions in the chalcopyrite and galena.

These veins range in thickness from less than one centimeter to several tens of centimeters and usually occur as sub-parallel sets up to several meters wide along northwesterly striking faults. At least three such vein sets are known within the Property area.