The Destiny Property

The Destiny Project is located approximately 75 km northeast of the city of Val d’Or in the prolific Abitibi Greenstone Belt where more than 180 million ounces of gold have been produced historically along major structural breaks within the assemblage of Archean-age volcanic, sedimentary and intrusive rocks. The Destiny Project lies along the approximately 400 km long Chicobi Deformation Zone, a major structural break which is largely underexplored in the Abitibi Greenstone Belt. The 5,013 ha project includes the DAC deposit, one of several gold zones along an approximately 6 km long segment of the Despinassy Shear Zone within the Chicobi Deformation Zone.

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The Empirical Project

The 10,518 Ha Empirical Gold-Copper-Molybdenum project is located in southeastern British Columbia, 12 km south of the town of Lillooet.

The project was initially explored for molybdenum in veins and was not systematically explored for porphyry style mineralization or gold.  

Approximately 1,600m of historic diamond drilling was completed in the 80’s to a maximum depth of 230m with 6 of the 15 holes returning anomalous gold values including 21m of 3.67g/t Au.

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The Tyber Project

The 928 Ha Tyber gold-copper-silver project is located in southeast Vancouver Island 18 km Southwest of Parksville.

Historic rock samples taken from the property between 1916 and 1986 assayed up to 2.328 oz/t Au (from historic adit dump), 16% Cu and 305.5 oz/t Ag (1916 BC Mines Annual Report; Minfile 092F236).

Two historical adits on the Tyber Project, believed to be targeting mineralized quartz veins within local shear zones, extend approximately 14 m and 47 m in length (1981 Assessment Report 09432).

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The Gretna Green Project

The 1,331 Ha Gretna Green gold-copper-silver project is located approximately 24 km Southwest of Port Alberni and 1.3 km North of Henderson Lake.

Historical reports show that a selected sample assayed 48.00 grams per tonne gold, 51.43 grams per tonne silver and 17.8 percent copper (Minister of Mines Annual Report 1921; Minfile 092F24). Locally, a skarn zone with chalcopyrite ore occurs in limestone cliffs near a contact with dioritic rock.

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