Robinson Dike Gold Leak Project

Located in Central Idaho, USA, within the prolific Idaho Batholith, a well-known host of shear-zone-related gold systems.
Option to acquire 100% ownership of the historical Robinson Dike and Gold Leaf Deposits, featuring strong historic grades and extensive underground workings.
Historical drill-indicated reserve (non-NI 43-101 compliant) includes:
- 153,000 tons averaging 2.33 g/t Au and 4.8 g/t Ag.
- o 191,000 tons averaging 2.06 g/t Au.
Historical feasibility study (1984) outlined robust open-pit economics, with 1.1:1 strip ratio, ~85% gold recovery, and first-year payback at $350/oz gold.
Gold occurs in oxidized, silicified granite—a style amenable to heap-leach extraction, with cyanide consumption <1 lb/ton and rapid recovery.
Only ~700 ft of the 4,000 ft shear zone has been drilled; ~90% of the property remains unexplored.

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Regional Context

The Robinson Dike and Gold Leaf Deposits lie within the Idaho Batholith, a region renowned for its numerous gold-bearing shear zones and long mining history. The property sits near the historic mining community of Dixie, Idaho, benefitting from direct road access, nearby airstrips, and strong local support for responsible mineral development.

Geology and Mineralization

Gold mineralization is hosted within oxidized and silicified granite, characterized by fine disseminated gold along a shear zone traced for more than 4,000 feet in strike length. Historical work outlined near-surface oxide mineralization with simple metallurgy and excellent heap-leach recoveries.

Metallurgical testing by K.D. Engineering, Degerstrom Laboratories, and the University of Idaho confirmed the ore’s strong leach response, high gold recovery, and low reagent demand. The gold system remains open along strike and at depth, representing significant expansion potential.