Golden Dome Project

Golden Dome Project

Golden Dome claims
Oxidized silica outcrop, characteristic of high-sulfidation epithermal alteration

Regional Context

The Golden Dome Project lies within the Antelope Valley Volcanic Center of northern California, a region known for epithermal gold systems associated with volcanic activity along the ancestral Cascade arc. This setting has proven highly prospective for gold-silver mineralization, with similar alteration and mineral assemblages found in productive high-sulfidation deposits across the western United States.

Geology and Mineralization

Gold occurs in a vuggy silica-alunite-pyrite vein system, with ore minerals including pyrite and enargite, accompanied by secondary copper oxides. Mineralization is primarily hosted in altered volcanic rocks with strong silica and alunite alteration halos, suggesting a well-preserved epithermal environment. The presence of both gold and silver indicates a polymetallic system with potential for broader resource development
Antelope Valley volcanic terrain near the Golden Dome alteration zone

Regional Context

Geology and Mineralization

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Historical Information and Exploration Context

The mineral properties comprising the portfolio have been the subject of extensive historical exploration, development work, and, in several cases, past commercial production or advanced-stage evaluations with the intent to commence mining. The historical exploration results, sampling, drilling, resource estimates, feasibility studies.

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