Northwire Canada EditionSunday, July 12, 2026
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GLDN 0.055 +0.0% BRON 0.040 +0.0% BTO 5.43 −0.7% ESK 0.365 −2.7% AUMN 0.275 +0.0% GGX 0.040 +0.0% S 0.155 +29.2% NNX 0.035 +0.0% ABX 51.90 −0.6% TTS 2.40 −4.0% FCI 0.400 −9.1% GR 0.075 +0.0% AII 23.38 +12.4% TUNG 1.72 +1.8% LGO 1.01 −2.9% EMM 0.080 +0.0% GLDN 0.055 +0.0% BRON 0.040 +0.0% BTO 5.43 −0.7% ESK 0.365 −2.7% AUMN 0.275 +0.0% GGX 0.040 +0.0% S 0.155 +29.2% NNX 0.035 +0.0% ABX 51.90 −0.6% TTS 2.40 −4.0% FCI 0.400 −9.1% GR 0.075 +0.0% AII 23.38 +12.4% TUNG 1.72 +1.8% LGO 1.01 −2.9% EMM 0.080 +0.0%
Drill Results Routine +

Powermax Minerals Identifies Priority Rare Earth Element Targets at the Hopkins REE Project, Ontario

PMAX · Price

Executive Summary

  • Powermax Minerals received a desktop study for its Hopkins REE Project in northeastern Ontario, integrating geological, geophysical, and geochemical datasets to prioritize future exploration targets.
  • The study ranks Block A as Priority #1, with target area A1 identified as the highest-priority zone for immediate field validation, including rock sampling, structural mapping, and soil geochemistry.
  • Management outlines a phased exploration program encompassing airborne surveys, ground mapping, targeted sampling, and potential trenching or drilling, contingent on funding, permitting, and seasonal conditions.

Key Details

  • Project Location & Tenure: Hopkins REE Project, Cochrane District, NE Ontario (~45 km NNE of Kapuskasing, Porcupine Mining Division). Comprises 13 mineral claims totaling ~6,145 hectares across two blocks (Block A: ~5,479 ha/11 claims; Block B: ~666 ha/2 claims).
  • Study Methodology: Prepared by Shahab Tavakoli, P.Geo. Integrated whole-rock geochemical data, regional airborne magnetic/radiometric surveys (Ontario Geological Survey), gravity data, and historical exploration data for the Clay-Howells alkalic intrusive complex.
  • Priority Targets Identified:
  • Block A (Priority #1): Contains five target areas (A1–A5). Area A1 (north bank of Kapuskasing River) is the highest-ranked hotspot, recommended for detailed rock sampling, structural mapping, and soil geochemistry. Areas A2–A5 are high-prospectivity cells overlapping major magnetic tilt derivative (TDR) lineaments, recommended for prospecting, mapping, and ground verification.
  • Block B (Priority #2): Contains two target zones (B1–B2) along the intrusive margin with ENE-trending structures supporting localized REE potential. Recommended for targeted mapping, prospecting, and sampling.
  • Geological & Geophysical Model: REE prospectivity is margin- and structure-controlled, driven by late-stage carbonatitic and metasomatic processes. The Weight-of-Evidence (WofE) model highlights prospectivity where anomalous TREO values coincide with elevated Th/K, elevated U/K, variable Th/U, high gravity responses, and positive magnetic tilt derivative extrema.
  • Mineralization Styles: Two principal styles identified: (1) intrusion-hosted, magnetite-bearing, K-rich syenite system; and (2) contact-hosted, Th-rich metasomatic system along the intrusive-paragneiss boundary.
  • Recommended Exploration Program: Phased program subject to funding/permitting/seasonality, including airborne magnetic/VLF/radiometric surveys, geological mapping/prospecting over targets A1–A5 and B1–B2, targeted rock sampling, soil geochemistry over Area A1, ground verification of anomalies, and potential follow-up trenching or drill testing.
  • Data Verification Status: Study relies on publicly available historical datasets; interpretations are preliminary and subject to confirmation through future fieldwork. No current mineral resource or reserve estimate exists.
  • Qualified Person: Afzaal Pirzada, P.Geo., Director of the Company, reviewed and approved the technical information per NI 43-101.

Notable Quotes

  • Paul Gorman, CEO: "The Hopkins REE desktop study provides Powermax with a clear and technically supported exploration framework. The identification of multiple priority targets, particularly Area A1 within Block A, gives the Company a focused path forward for field validation. The integration of magnetic, radiometric, gravity and geochemical datasets has highlighted structurally controlled zones that we believe warrant systematic follow-up for rare earth element mineralization."
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