Slide 1: Dryden Gold Corp April 2025
TSXV: DRY | OTCQB: DRYGF WWW.DRYDENGOLD.COM APRIL 2025
Slide 2: Acknowledgements & Forward-Looking Statements
Acknowledgements & Forward-Looking Statements Dryden Gold Corp acknowledges all Indigenous Peoples and that it is operating on the traditional homelands of the Wabigoon Lake Ojibway Nation and Eagle Lake First Nation. Certain statements contained herein constitute “forward-looking statements” within
Slide 3: Key Value Drivers
Key Value Drivers Trey Maura Scott Anna Jason Christina Darin Stephen Wasser Kolb Kelly Hicken Jessup McCarthy Wagner Kenwood Experienced Management History of success in navigating M&A Technical team has extensive regional experience CEO President CFO VPX Director Director Advisor Advisor Director
Slide 4: Prolific Gold Region | Under Explored in the Dryden Gold District
Prolific Gold Region | Under Explored in the Dryden Gold District Archean Lode Gold Mine Camps Canada Central Canada Rice Lake Red Lake Rice Red Dryden Kirkland Winnipeg Ontario Lake Lake Timmins Lake Timmins Thunder Bay Kirkland Lake Gold Rock Quebec Minnesota Wisconsin 1km Toronto 2km USA Michigan
Slide 5: Prolific Gold Region | Dryden Gold District
Prolific Gold Region | Dryden Gold District Over 30+ Moz Au of historic production from the Birch- Uchi Greenstone Belts Under-explored Dryden Gold District despite district-wide high- grade gold occurrences Turn of the century historic high-grade mining in the Gold Rock Camp with little geo-focused
Slide 6: Dryden Gold District - Historical Gold Mining Region
Dryden Gold District - Historical Gold Mining Region Laurentian Mine ~75% of the historic mining in the district was from the Gold Rock camp N Mining at the turn of the century (1900’s) Historic mining was designed from surface expression Laurentian Laurentian Mine produced 20K tons of ore at 14 g/t
Slide 7: 2024 Exploration Timeline
2024 Exploration Timeline Gold Rock - Big Master & Gold Rock & Hyndman Sherridon Elora Phase 1-4 Drilling Field Mapping Field Mapping Fall Drill Program Program Program Program Dryden Gold Exploration Strategy Fall/Winter Relogging LiDAR Survey Phased Geological Phase 5 Drilling Modeling Program Pro
Slide 8: 2025 Exploration Strategy
2025 Exploration Strategy Gold Rock Gold Rock & Gold Rock, Mosher Cross River, Gold Expansion & Bay, Regional Hyndman Rock Extension Regional Targets Geophysics 3D Channel Detailed Drill Program Drill Program Inversion Sampling Mapping Dryden Gold Exploration Strategy Historic Core Phased Geological
Slide 9: Geoscience Systems Approach to Unlock Value
Geoscience Systems Approach to Unlock Value Understanding the What are the primary Supportive data controls on mineralization and secondary controls collection trends on mineralization? Oriented core in Higher grade (+10 Quartz vein 2023 and 2024 g/t) structurally orientations and Gold Rock drilling
Slide 10: Strategic Land Package
Strategic Land Package Over 702 km2 (70,250 hectares) consolidated by Dryden Gold Corp. Excellent infrastructure – Roads (Trans-Canada Hwy), power & labour 50 km covering regional gold bearing MDdz structure (Manitou-Dinorwic deformation zone) Limited exploration - only 33,200 meters of historic dri
Slide 11: District Scale | Near Surface High-Grade Gold Across the Property
District Scale| Near Surface High-Grade Gold Across the Property 2024 EXPLORATION FOCUS AT THE GOLD ROCK CAMP: Elora Gold System - Drill Highlights 15.17 g/t gold over 6.95 meters 10.59 g/t gold over 6.10 meters 7.47 g/t gold over 12.20 meters Big Master Gold System - Drill Highlights 3,497.0 g/t go
Slide 12: Dryden Area of the Western Wabigoon Subprovince
Dryden Area of the Western Wabigoon Subprovince • The Dryden area of the Wabigoon subprovince is primarily composed of 2745-2710 Ma mafic to felsic rocks. • Up to 10 km wide, 50 km long belts of 2710-2695 Ma turbiditic, volcaniclastic, alluvial, and chemical sedimentary rocks unconformably overlie t
Slide 13: Dryden Area of the Western Wabigoon Subprovince
Dryden Area of the Western Wabigoon Subprovince • The Mosher Bay-Washeibemaga deformation zone (MBWdz), Wabigoon deformation zone (Wdz) and Manitou-Dinorwic deformation zone (MDdz) represent regional, and possibly crustal scale, brittle-ductile deformation zones that are E- and NE-trending, respecti
Slide 14: Regional Map – Rock Library
Regional Map – Rock Library Clastic Sediments -Conglomerate High Mag Mafic Volcanic Mafic Intrusion - Gabbro Mafic Volcanics Intermediate Intrusion-Diorite Pillow Basalt Amygdaloidal Basalt Felsic Intrusion Felsic Volcanics Ultra Mafic Intrusive TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 14
Slide 15: Mineralization – Rock Library
Mineralization – Rock Library Hyndman Mineralization in Aplite Dyke Elora Structure Mineralized Sheared Mafic Volcanics Hyndman Mineralization in Diorite Big Master Structure Sherridon Vein hosted in Mafic Volcanics Mineralization in Pyroxenite Dyke TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 15
Slide 16: Similarities to Red Lake
Similarities to Red Lake Dryden Gold Corp. Gold Rock Area Geology Similar geological setting, rock types, and dykes with regional folding. Confirmed - through mapping, geophysics and drilling. Near surface high-grade free gold in an Archean setting. Confirmed - added new high-grade shoots with shall
Slide 17: Similarities to Timmins
Similarities to Timmins Dryden Gold Corp. Manitou Dinorwic deformation zone (MDdz) Western Wabigoon Timmins (Abitibi Sub-Province) Mafic to intermediate successions of metamorphosed volcanic and sedimentary rocks that were intruded by tonalitic to granitic plutons Crustal-scale deformation zones wit
Slide 18: Mineralization Timing, Age & Metamorphism
Mineralization Timing, Age & Metamorphism The Western Wabigoon contains Meso- to Neoarchean rocks (2775-2680 Ma) Age dating was completed from syn-D2 gold bearing quartz carbonate veins at Gold Rock (Kenwest) and Goldlund and yielded three distinct populations, corresponding to three weighted avera
Slide 19: D1 Structural Synthesis – Western Wabigoon Subprovince
D1 Structural Synthesis – Western Wabigoon Subprovince • D1 is marked by the development of an ENE to E-trending vertical to subvertical foliation (SMM-1) that is best preserved in sedimentary and intrusive rocks of the Manitou group in proximity to the MBWdz. • The presence of an E-trending S1 foli
Slide 20: D2 Structural Synthesis – Western Wabigoon Subprovince
D2 Structural Synthesis – Western Wabigoon Subprovince • D2 is characterized by ductile deformation along the Wdz, WBWdz and MDdz. • In the MDdz, D2 resulted in the regional development of a NE-trending penetrative to anastomosing S2 foliation that crenulates earlier structural fabrics (bedding and
Slide 21: Gold Rock Camp | Geology & Targets
Gold Rock Camp | Geology & Targets Created 3D magnetic inversion from all known data (geology, geophysics, mapping, sampling, etc.) Created a 3D geological model with accompanying targets from unexplained anomalies These targets are areas where it is theorized there is either alteration or mineraliz
Slide 22: Gold Rock | Near Surface High-Grade Gold
Gold Rock | Near Surface High-Grade Gold MDdz Brownfield opportunity within the Gold Rock Camp Majority of historic drilling focused on Gold Rock Camp Historic high-grade intercepts on two gold systems 502 Targets Confirmed 75% of all historic mining occurred in Gold Rock Camp 1.5 km Strike Length P
Slide 23: Spring 2023-2024 Drilling
Spring 2023-2024 Drilling Expanded mineralized footprint of gold system Confirmed orientation, structural controls and expanded Elora high-grade zone and BM2 historically delineated high-grade zone KW-24-008: 15.17 g/t gold over 6.95 meters, including 43.81 g/t gold over 1.42 meters and 92.10 g/t go
Slide 24: Fall 2024 Drill Program – Expand on the Elora Gold System
Fall 2024 Drill Program Expand on the Elora Gold System Historic Elora-Jubilee Mine KW-25-001 KW-25-002 Laurentian Gold Mine Elora Gold System hosted high-grade Laurentian Gold Mine with average grade of 14 g/t gold and mined to only 140 meters Figure 1 Long Section TSXV: DRY | OTCQB: DRYGF DRYDENGO
Slide 25: Fall 2024 Drill Program – Test the Big Master Gold System
Fall 2024 Drill Program Test the Big Master Gold System TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 25
Slide 26: Elora Drill Core Preliminary Structural Analysis
Elora Drill Core Preliminary Structural Analysis 3D planar structural disks in Leapfrog. Elora mineralized trend shown in grey. Average orientation of all Potential structural domains: contact & foliation ● Regional S2 = 033/80 (n = 197) measurements: ● Northerly fabric = 014/71 (n = 75) 030/77 (n =
Slide 27: Big Master Drill Core Preliminary Structural Analysis
Big Master Drill Core Preliminary Structural Analysis 3D planar structural disks in Leapfrog. Big Master mineralized trend shown in grey. Average orientation of all Potential structural domains: contact & foliation ● Regional S2 = 037/85 (n = 283) measurements: ● Northerly fabric = 013/81 (n = 83) 0
Slide 28: MDdz at Big Master (Gold Rock)
MDdz at Big Master (Gold Rock) Zammit (2020) 28
Slide 29: MDdz at Big Master (Gold Rock) - Veining
MDdz at Big Master (Gold Rock) - Veining • Based on cross-cutting relationships and composition, three generations of NNE- to NE-trending quartz to quartz-carbonate veins are identified. 1. Vka is NE-trending, steeply-dipping, and solely composed of milky quartz. These veins are isoclinally folded a
Slide 30: Geochemistry
Geochemistry Whole Rock analysis on select samples from Geochemical analysis (4-acid digest) from Phase 1-4 Phase 1-4 drill programs drill programs displaying PCA analysis Principal Component 1 (PC1) Positive Correlation: Au, Ag, As, Cd, Pb, Sb, Zn The presence of quartz- carbonate veins within high
Slide 31: Petrography
Petrography Logged ID Texture Essential Mineralogy Protolith Listwanite: hosts an assemblage of carbonate Banded sulphide rich schistose, no textural relicts minerals (magnesite, ankerite and dolomite), quartz>dolomite/ankerite>pyrite volcaniclastic/sedimentary basalt found silica and/or fuchsite (C
Slide 32: Ongoing Re-Logging Program
Ongoing Re-Logging Program Approximately 20,000 meters of historic drill core was selectively sampled & securely stored (Gold Rock, Cross River, Sherridon, etc.) Re-logging will improve our understanding of grade- thickness continuity The 2018 relogging program at Great Bear was instrumental in the
Slide 33: Summer 2024 Field Program
Summer 2024 Field Program Field mapping program preferentially focused on Hyndman, Gold Rock, and Sherridon areas of the property Highlight - 2023 reconnaissance program returned 4/5 samples on Hyndman over 10.00 g/t gold Use geophysical anomalies and structural interpretation as a guide for priorit
Slide 34: Gold Rock Property
Gold Rock Property This area is hosted by mafic flows of the Pincher Group that were intruded by syn-deformational felsic dykes The sinistral transpressive Manitou Dinorwic deformation zone (MDdz) is the main control on mineralization with gold primarily hosted in fracture- filling quartz veins rela
Slide 35: Gold Rock Property – Mosher Bay Mapping Interpretation
Gold Rock Property – Mosher Bay Mapping Interpretation Persephone Vein - The vein is straight-edged, sheeted to brecciated quartz-carbonate vein, hosted in a very discrete ankerite-chlorite altered shear zone. • The structure cuts across weakly ankerized, mostly unstrained conglomerate. The average
Slide 36: Gold Rock Property – Mud Lake Mapping Interpretation
Gold Rock Property – Mud Lake Mapping Interpretation • Mapping/sampling was successful at extending the Last Chance trend to the north significantly (~450 m), demonstrating an impressive degree of continuity for this trend which mirrors what we see south of Mud Lake. The trend remains open to the no
Slide 37: Hyndman Property – 3D Inversion Study
Hyndman Property – 3D Inversion Study The property is located between the Revell Lakes batholith to the southwest and the Basket Lake batholith to the northeast. It is underlain by foliated and deformed mafic to intermediate volcanic rocks. Felsic porphyry and granitic intrusions occur within the vo
Slide 38: Hyndman 2024 – New Geological Map
Hyndman 2024 – New Geological Map Mafic metavolcanic rocks often display pillow selvages, however they are elongated, deformed, and often garnet- bearing in the eastern portions of the traverses, relative to the more characteristic pillow metabasalts in the western claims. These garnet-rich selvages
Slide 39: Hyndman 2024 Field Results
Hyndman 2024 Field Results The gold showings hosted within the mapped diorite are situated within narrow shear zones that cut through the intrusion with mineralization associated with aplite dykes. Intrusions can act as ridged bodies in comparison with the more ductile surrounding mafic volcanic and
Slide 40: Sherridon Property
Sherridon Property The area consists of a thick Early Precambrian mafic metavolcanic sequence followed by intermediate to felsic flows and related tuffs. This sequence is in turn overlain by a sedimentary sequence and is intruded by mafic to felsic stocks and sills. Mineralization in the area consis
Slide 41: Sherridon Property – New Geological Map
Sherridon Property – New Geological Map The property comprises mainly mafic greenschist facies metavolcanic rocks including massive basalts, pillowed basalts and amphibolite facies coarse grained metavolcanics and porphyritic metabasalts. Interbedded with the pillowed flows are massive to coarse-gra
Slide 42: Dryden Gold’s Resource Pipeline
Dryden Gold’s Resource Pipeline 2025 Exploration Emphasis on Gold Rock Camp Targets. Several Regional targets are Identified and Follow up stages will continue in 2025. Regional Drill Ready Mineral Conceptual Early-stage Identified Follow Up Resource (Camp) Target Target Target Target Target Target
Slide 43: District Scale | Near Surface High-Grade Gold Across the Property
District Scale| Near Surface High-Grade Gold Across the Property Gold Rock Camp Drill Highlights Hyndman Field Samples 30.72 g/t gold over 5.70 meters 34.8 g/t gold grab sample 2024 15.17 g/t gold over 6.95 meters 13.0 g/t gold grab sample 2023 15.4 g/t gold over 6.1 meters 12.3 g/t gold grab sample
Slide 44: 2025 Drill Program Objectives
2025 Drill Program Objectives Expand on the high-grade zone in the Elora Gold System Test new targets along strike and at depth at Gold Rock Test Highly Prospective Regional Targets TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 44 * Permits submitted but pending approval
Slide 45: Elora Permit
Elora Permit TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 45
Slide 46: Sherridon Permit
Sherridon Permit TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 46
Slide 47: Exploration Budget 2025 | Use of Proceeds – 5.8 M
Exploration Budget 2025 | Use of Proceeds – 5.8 M Item Property Cost ($CAD) LiDAR All properties $100,000 Till/Soil All properties Early Geochemical $700,000 Stage Survey 14% Geophysics 3D Priority Regional Targets $250,000 Inversion Sherridon, Gold Rock expanded, other Gold Rock Mapping & Priority
Slide 48: Till Planning
Till Planning TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 48
Slide 49: Contact
TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM Contact: Trey Wasser CEO & Director +1 (940) 368-8337 twasser@drydengold.com Maura Kolb President & QP +1 (807) 632-2368 mjkolb@drydengold.com
Slide 50: Appendix
Appendix Digging deeper into our story.
Slide 51: Gold Rock – Deformational History
Gold Rock – Deformational History • Orogenic gold occurrences in the Dryden area largely occur within ~ 5-10 km of the major E- and NE-trending deformation zones. • The Kenwest prospect is hosted by mafic volcanic flows of the Pincher Lake group that were intruded by syn- deformational felsic dikes
Slide 52: Gold Rock - Mineralization
Gold Rock - Mineralization • Gold is primarily hosted in NE-trending fracture-filling quartz veins that are interpreted to relate to brittle-ductile deformation occurring during sinistral transpression along the MDdz. • Ore mineralogy includes carbonate and sulphide minerals, chlorite, sericite, and
Slide 53: The Manitou Lakes Area
The Manitou Lakes Area • The Manitou Lakes area is a ~ 400 km2 area located at the intersection of the MBWdz and MDdz and is bounded to the northwest by the 2740-2720 Ma Atikwa-Lawrence batholith and to the southeast by the syn-to-late orogenic 2705-2695 Ma Taylor Lake and Scattergood Stocks • The M
Slide 54: What We’ve Learned
What We’ve Learned S1 S2/F2 S3 D1 020/80 (average S1 72→053 foliation) (F2 Fold Axis Plunge/Trend) F2 isocinally folded limbs at 060/85 and S2 fabric no D3 vein 237/82 D2 S2: 034/84 (F2 axial Apparent F2 dip on plane // to main S2 S3 planes: 74 E foliation) S2 associated with sinistral-sense shear (
Slide 55: Gold Rock Camp | Historic Bulk Sample Highlights
Gold Rock Camp | Historic Bulk Sample Highlights HIGHLIGHTS TABLE Single gravity separation recovered: 88.6% Bulk cyanidation test recovery for the composite: 99.4% Weighted average grade from total of 17 chip samples, over 13.6 linear meters: 40.2 g/t Au Individual chip samples: 0.05 g/t Au - 1,07
Slide 56: Core Facility
Core Facility Dryden Core Facility Gold Rock TSXV: DRY | OTCQB: DRYGF DRYDENGOLD.COM 56
Slide 57: What We’ve Learned
What We’ve Learned Ore mineralogy includes carbonate and sulphide minerals, chlorite and sericite within native gold- bearing quartz veins in disseminated zones proximal to vein margins D3 is associated with late brittle-ductile deformation that occurs with narrow (~ <5 cm) extensional quartz veins