Bcm Resources Corporation · TSXV:B

Bcm Resources — Investor Presentation (December 2024)

25 slides from Bcm Resources's investor presentation, Dec 6, 2024

  1. Slide 1: Thompson Knolls - New Copper-Gold-Molybdenum Discovery in the Great Basin, Western Utah

    Sergei Diakov, Ph.D. and Richard R. Redfern, M.Sc. Thompson Knolls - New Copper-Gold-Molybdenum Discovery in the Great Basin, Western Utah December 6, 2024 1

  2. Slide 2: Cautionary Notes & Forward-Looking Statements

    Cautionary Notes & Forward-Looking Statements • This presentation contains certain information that may be deemed “forward-looking statements,” or "forward-looking information” (as defined under applicable securities laws), with respect to BCM Resources Corp. (the “Company” or “BCM Resources,” or “B

  3. Slide 3: Thompson Knolls: General Introduction

    Thompson Knolls: General Introduction • BCM Resources Corporation (Symbol "B", TSX- Venture Exchange), (the “Company,”, “BCM,” “BCM Resources,” “B”) is a diversified Canadian mineral exploration company focused on the continued exploration of its flagship Thompson Knolls (TK) Porphyry Cu-Au-Ag-Mo pr

  4. Slide 4: Geographic Location

    Geographic Location • Thompson Knolls is located in Utah’s Millard County, 25 miles east of the Nevada- Utah border, 2-3 miles south of Highway 6/50 – the “Loneliest Road in America” TK TK TK 4

  5. Slide 5: Regional Geology

    Regional Geology • The TK Property lies west of the Confusion Range known for numerous outcropping gold- bearing jasperoids, including at the King’s Canyon gold deposit ~5 miles (8 km) to NE of TK • The Property ground is covered by post-mineral fanglomerates composed of products of weathered destru

  6. Slide 6: TK Regional Geology

    TK Regional Geology D D’ TK Project Legend TK Project location Gold-silver occurrences Base metal occurrences Copper occurrences 6

  7. Slide 7: BCM's TK Landholdings

    BCM’s TK Landholdings Legend Recently claimed BLM ground Company claims on BLM land Company leases on SITLA land Highway I50 from Ely to Delta Existing unpaved roads The TK Property comprises 225 BLM claims and 2 parcels of Utah State leased lands totaling 5,540 acres (2,242 ha) 7

  8. Slide 8: Exploration History

    Exploration History • Exploration history started with a U.S. Geological Survey aeromagnetic survey conducted in 1972. The survey outlined a prominent magnetic “high” anomaly at TK, which led to the later formulation of a porphyry copper deposit model for this target area • From 1989 to 1996, Crown

  9. Slide 9: TKP Geophysical / Geological Data Integration

    TKP Geophysical / Geological Data Integration • BCM technical team compiled all historical geophysical data into 3D geophysical model • Combined geophysical and geological drilling data with surface geology were used as base model for directing targeted drilling in highly mineralized parts of the TK

  10. Slide 10: Thompson Knolls Project Current Status

    Thompson Knolls Project Current Status • “B” is on the hunt for an “Elephant-size” porphyry copper deposit in Utah, and TK is essentially a blind target • The TKP Porphyry/Skarn system is buried under Fanglomerate cover of varying thickness • “B” applied for and received a 10-year Plan of Operation

  11. Slide 11: TK Phase 1, -2 and -3 Drillhole Locations

    TK Phase 1, -2 and -3 Drillhole Locations TK14 Magnetic anomaly area 1 N Magnetic anomaly area 2 Drillholes completed in Phase 3 drillholes* Magnetic anomaly TKP property Phases 1 and 2 areas 1 and 2 boundary Note: * TK11 and TK13 remain undrilled, TK12 is only partially drilled 11

  12. Slide 12: Longitudinal Section Line DG

    Longitudinal Section Line DG Note TK6, TK14, TK7 and TK4 are projected to cross-section 12

  13. Slide 13: Selected Images of Mineralized Core

    Selected Images of Mineralized Core Photo 1. Drill hole TK6 at 3,420 ft (1,042.4 m) depth. Sulfide-rich skarn in 230 ft (70.1 m) interval of the core from “Eureka” skarn zone Photo 2. Drill hole TK6 a 30 ft (9.1 m) interval from 3,400 to 3,430 ft (1,036.3-1,045.5 m) that assayed 0.97% Cu, 0.14 g/t A

  14. Slide 14: Selected Images of Mineralized Core

    Selected Images of Mineralized Core Photo 3. TK8 drill hole interval from Photo 4. TK8 drill hole 10-ft (3 m) interval 2,180 to 2,190 ft (664.5-667.5 m) with from 2,220 to 2,230 ft (676.7-679.7 m) intense sulfide-magnetite brecciated detail with massive sulfide-magnetite- marble skarn that assayed 1

  15. Slide 15: Research Prelude

    Research Prelude • In Summer 2023, BCM, together with Crescat Capital, became a part of the CASERM program at Colorado School of Mines (CSM) • CASERM researchers: Dr. Mathias Burisch Hassel (CSM Associate Professor) and Chad Abarbanel (CSM MS Student) were assigned to review the TK core • In April 2

  16. Slide 16: Core Re-Logging Summary

    Core Re-Logging Summary • The new logging data imply discontinuous skarn packages that are intersected in drill holes TK6, TK8, TK9 and TK14 as well as at the very bottom of TK5 • Intersected skarn intervals are represented mainly by distal skarn mineral assemblages of pyroxene and serpentine, where

  17. Slide 17: Schematic Geological Model of the Thompson Knolls Porphyry/Skarn System

    Schematic Geological Model of the Thompson Knolls Porphyry/Skarn System 17

  18. Slide 18: Research Results

    Research Results • The geometry and mineralogy of skarn alteration intersected to date indicate that the Copper core of the Skarn and Porphyry system remains outside the area of recent exploration drilling • Relatively high Cu grades associated with this intermediate-distal skarn is encouraging beca

  19. Slide 19: Our Interpretation

    ECM Resources Corp. Our Interpretation rt q- es —_ ~ I \/ sim one See 2 |. fn if < $ tks G7 .@ |} 2\ J ri & TKS and (ae 47g tt 1 ! ting ! ! K7 ; tv Magnetic anomaly Area 2 TK3A Magnetic anomaly — rx 2) eS r=) r=) 6 Area 1 TK1 TK2 & @ TK4 ~ E TK17 @ 0 miles ah. Legend TK Mag a 7] Base metal ratio iso

  20. Slide 20: Conclusions & Recommendations

    Conclusions & Recommendations • The fluid migration pathways deduced from these observations could be from the SW to the NE, or from both the SW and N • The most obvious scenario is that the fluids came from SW from the geophysical anomalous Area 2, hence this area deserves primary attention for fol

  21. Slide 21: Future Drilling Plans

    Future Drilling Plans • Company’s vector path to the core of the TK mineralized system continues to be refined with each phase of drilling. After Phase 3 with more drilling data available we are now able to apply a more scientific approach in our exploration program • BCM focus will turn to drilling

  22. Slide 22: Planned Drillholes Under Plan of Operations: Proposed Holes in Area 2

    Planned Drillholes Under Plan of Operations: Proposed Holes in Area 2 N TK6 TK5 TK14 TK9 TK8 TK3a TK10 TK3 Area 1 TK15 TK11 TK1 TK16 TK7 TK2 TK17 TK4 TK12 TK13 Legend Company claims on BLM land DK14 DK DK13 1 Company leases on SITLA land DK Previously drilled holes 8 DK12 Area 3 Area 2 DK10 Drill ho

  23. Slide 23: Future Exploration

    Future Exploration • With the successful outcome of the proposed Phase 4 drill program delivering economic intercepts in both skarn and porphyry mineralization, our focus will be directed at the western anomalous Area 2 with additional drill testing its southern extension • Anticipated economic inte

  24. Slide 24: For further information to this presentation please contact

    For further information to this presentation please contact: Sergei Diakov Phone: (760) 803-0506 Email: sdiakov@gmail.com or sdiakov@bcmresources.com 24

  25. Slide 25: END

    BCM Resources Corp END

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