Location
Nevada
Ownership
100%
Project Stage
Advanced Exploration & Resource Definition
Metals
Gold & Silver
Property Size
100% control over a 1,729.73ha
Deposit Type
Volcanic-hosted epithermal precious metal deposit
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Geology
The Comstock District sits on the eastern side of the Virginia Range, an area shaped by multiple waves of volcanic activity over millions of years. Older sedimentary and metamorphic rocks form the deep foundation, while younger volcanic layers, mainly andesites and rhyolites, built up over time to create the host rocks we see today. These volcanic units, together with the large faults cutting through them, created the ideal conditions for silver and gold–bearing fluids to move through the rock and form mineralized zones.
The silver-gold deposits at Comstock are classic low-sulfidation epithermal systems, the same style responsible for many of the world’s most profitable precious-metal camps. Mineralization occurs in networks of quartz-rich veins, stockworks, and breccias developed along major fault zones, particularly the Comstock fault, the district’s main structural control. Historically, extremely rich “bonanza” zones were found where veins intersected or flexed, producing some of the highest-grade gold and silver ever mined in the American West. Today, areas like the Occidental-Brunswick Lode continue to show the same favourable structural features, with multiple sub-parallel vein systems that offer strong potential for new discoveries.
