Essex Resources talks fall 2025 exploration at Rabbitt

Executive Summary

• Essex Resources Corp. reports significant exploration progress at its Rabbitt copper-silver-lead-zinc property in Southern British Columbia, specifically defining a northwestern extension of a partial ring of mineral showings.
• Induced polarization (IP) and total metal ion (TMI) soil surveys identified a prospective chargeability high and resistivity low west-northwest of the Thynne showing, consistent with subhorizontal, mineralized plates dipping southwestward.
• The exploration program traced the ring of mineral showings for approximately 1,500 meters northwestward, with geophysical data suggesting the presence of up to six stacked sulphide lenses.

Key Details

• Property Location: Rabbitt property, Similkameen mining division, Southern British Columbia.
• Exploration Program: Comprehensive program conducted in fall 2025, including induced polarization geophysics and total metal ion (TMI) soil geochemical surveys.
• Geochemical Survey Results:
  • 560 TMI soil samples and 16 rock samples collected.
  • Defined an extension of the partial ring of mineral showings around the northern slope of Rabbitt Mountain.
  • Ring traced for approximately 1,500 meters (5,126 feet) northwestward from the Thynne showing across the northern slope to near the northern property boundary.
  • Identified four areas of elevated soil gold associated with three areas of enriched soil copper.
• Induced Polarization (IP) Survey Results:
  • Survey covered an area of approximately one square kilometer, extending northwesterly from the Red Bird showing through the Shamrock and Thynne showings to about 750 meters northwest of the Thynne showing.
  • Chargeability ranges: 3.4 to 20.9 millivolts per volt.
  • Resistivity ranges: 176.8 to 980.1 ohm-metres. Key Anomaly: A prospective area centered about 400 meters (1,312 feet) west-northwest of the Thynne showing.
    • Chargeability as high as 17 millivolts per volt.
    • Coincides with a resistivity low (fewer than 230 ohm-metres).
    • Flanked by elevated soil-copper, zinc, and gold concentrations.
  • Geological Interpretation:
    • The resistivity low core extends ~400 meters southeasterly and ~150 meters along the northwestern boundary.
    • Anomaly orientation (northwest-southeast) is consistent with the subcrop of a subhorizontal, mineralized plate dipping southwestward.
    • Sharp anomaly boundary on the northeastern side suggests potential surface hosting; diffuse southwestern boundary suggests fading detection due to increased burial.
    • Pseudo-sections indicate the possibility of as many as six stacked sulphide lenses contributing to the resistivity low.
• QA/QC: Samples analyzed at Peter E. MSA Labs (Langley, B.C.) using induced coupled plasma techniques. No QA/QC issues detected.
• Qualified Person: Chris Dyakowski, PGeo, Director of the company.

Notable Quotes

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