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Peak

B.C

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Initial drill program completed June 2024

Tested two, southern areas along important structural setting for Cu-Au porphyry systems. Northern targets remain untested

Drilling encountered altered alkaline intrusive rocks – source for 2% copper mineralization on surface remains open

 

Excellent infrastructure

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Peak Central

Drilling identified megacrystic porphyritic rocks with intense sericite alteration.

 

Surface rock samples return grades of over 2.0% Cu. Rock chip sampling have returned 25 metres grading 0.44% Cu

 

Source of copper mineralization remains open

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Peak Central – IP Anomaly

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Drill holes at Peak Central intersected a series of mixed sediments including black graphitic shales, sandstones and polymictic conglomerates. The sedimentary package is intruded throughout by a series of porphyry dykes and the highly chargeable zone outlined by IP geophysics is likely due to graphitic sediments and zones with up to 5% pyrite. In addition, a deep resistive centre targeted in RC-PG-02 is interpreted to be caused by quartz-rich sandstones, conglomerates and late porphyry dykes.

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Peak North

Soil geochemistry outlines highly anomalous Cu, Ag values

Elevated geochemistry associated with interpreted intrusive related magnetic highs and lows

Area bounded to west by the Pinchi fault an important NW regional structure associated with Cu – Au deposits

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