• 1,566 ha in size
• Great logging road access
• 7km north of the town of Pemberton
• 100% owned with no further encumbrance
• Comprehensive surface exploration completed previously including mapping, soil sampling, regional airborne magnetic survey, and historical diamond drilling

Regional Geology

The Owl Creek Project is located within a prospective geologically belt that hosts many Miocene intrusion related porphyry style deposits. This belt is part of a subduction zone that stretches from northern California through Oregon into British Columbia. Some of the major deposits in this belt include:

• Mt. Margaret in southwestern Washington State: Historical geological resources of 523.0 MT at 0.36% Cu, 0.011% Mo, and 0.24gpt Au (CIM Special Volume 37, 1986)
• New Prosperity in south-central BC: Total Measured and Indicated Resources at 0.15% Cu cutoff grade with 1,109 MT at 0.24% Cu and 0.007% Mo

Highlights

• 4 zones were identified previously: A, B, C, & D zones
  • Grab samples by zone:
    • A: 0.15% to 1.99% Cu
    • B: 0.12% to 0.80% Cu
    • C: 0.23% to 0.47% Cu
    • D: newly identified diorite identified by soil and geophysical surveys

• Mapping and sampling only completed in selected area (lack of a project wide sampling and mapping program)

Exploration Potential

• The four identified copper‑bearing zones span more than 5 km along strike and may represent interconnected segments of a larger, continuous mineralized system.
• Airborne magnetic data have delineated multiple high‑priority targets slated for follow‑up in the next phase of work.
• Previous programs did not assay for additional elements such as gold or silver, creating a clear opportunity to conduct multi‑element assays—particularly for copper and gold mineralization.