CONFUSION hILLS

Geology

The Confusion Hills Project encompasses an extensive alteration system exhibiting characteristics of both high-sulfidation and intermediate-stability hydrothermal regimes. The high-sulfidation assemblage is marked by advanced argillic alteration and vuggy silica, while the more neutral-stable alteration phase is typified by illite-muscovite assemblages associated with veining and silicified hydrothermal breccias.

The occurrence of gusano textures, pyrophyllite, and elevated molybdenum geochemistry suggests proximity to a porphyry system. Preliminary geochemical sampling returned significant gold, silver, and trace element concentrations, indicating that the Confusion Hills prospect hosts mineralization. The area is considered a high-priority exploration target for both low- and high-sulfidation epithermal mineralization, with potential for a shallow porphyry system.

Detailed lithological mapping by Dr. Rachel Harrison has delineated a newly recognized lithocap extending across approximately 1.6 km × 0.5 km. The core of the lithocap is characterized by vuggy quartz with alunite, transitioning outward to massive pyrophyllite zones that grade into white mica-rich domains.

The identification of gusano textures within the volcanic sequence indicates the dissolution of primary volcanic fabrics, a process driven by extensive replacement by advanced argillic alteration minerals. Soil geochemical analyses reveal a strong spatial correlation between gold anomalism and zones of advanced argillic alteration, with a pronounced molybdenum anomaly defined to the south of the project area, further supporting the hypothesis of a Proximal porphyry system.

Recent magnetic study and IP surveys, show a high mag zone to the SE of the claim as well as a high chargeability anomaly open as well to the southeast.

Planned follow up geophysics on their way. Preliminary drilling targets have been set.