PROJECT SUMMARY
Prolific District: Situated in the Yerington Copper District, Nevada - a Tier-1 jurisdiction with world class deposits.
Prime Positioning: Two main targets located immediately North and South of the Pumpkin Hollow Deposit, leveraging district-scale geology.
High grade copper and gold at surface.
High-Grade Copper: Shear-hosted quartz sulfide mineralization returning values up to 7.38% Cu.
Structural Control: Mineralization hosted in 1-10-meter-wide shear zones.
Geophysical Signature: Coincides with a magnetic high anomaly similar to Pumpkin Hollow, suggesting a genetic link to the Yerington Jurassic Batholith.
Large-Scale Footprint: Identified 1,400m x 800m zone of Porphyry-style stockwork quartz sulfide mineralization.
Recent rock sampling: Identified high gold quartz veins up to 19.7 g/t Au.
Strong Vectors: Defined by hydrothermal alteration, iron oxidation, and Cu-Au geochemical anomalies in rock and soil.
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NORTH TARGET
Mineralization consists of massive quartz with pyrite and chalcopyrite.
Veins typically less than 50cm in width. In wider shear zones, it is 1-10m in width.
Shear zone rocks are altered to sericite-chlorite-pyrite and stained by limonite and malachite.
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HOLLOW SOUTH STOCKWORK
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Chlorite alteration is more pervasive than the Northern Target.
Historic workings are located on narrow quartz sulfide veins.
Porphyry type stockwork quartz sulfide vein mineralization was identified over an area of 800 x 1400 m.
HOLLOW SOUTH MINERALIZATION
Quartz veins 10-30 cm's in width.
With limonite after sulfide
Alteration selvages of sericite-illite
Narrow vein mineralization found throughout Yerington District.
Mesothermal intrusive related gold-silver-copper base metal mineralization.
Grab samples from Coyote workings returned high grade gold up to 19.7 g/t Au with anomalous Cu, Pb, Zn
Coyote workings have been reclaimed and it is difficult to determine vein thickness on the surface
In other exposures, veins are typically 0.5m wide
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