Dryden Gold Corp. (TSX-V: DRY) (OTCQB: DRYGF) is pleased to announce results from its first pass 3-hole exploration program at the Mud Lake Target Area in the Gold Rock Camp. Mud Lake is located 2 kilometers northeast of the main Gold Rock target area along the prolific Manitou-Dinorwic Deformation Zone. The objective of the step-out drilling at Mud Lake was to confirm the periodicity (or repetition) of the high-grade gold structures controlled by the MDdz along its 20-kilometer strike in the Gold Rock Camp. With this successful step-out, the Company will continue to develop addition targets in the Gold Rock Camp. Summary video link.
Highlights:
Trey Wasser, CEO of Dryden Gold commented, “One of our four major objectives in the 2025 exploration program was to validate our theory of periodicity of deposits in the Gold Rock Camp. Our early success at Mud Lake confirms that the geological setting could support multiple sub-parallel, gold-bearing structures. This type of structural repetition is the foundation of many high-performing gold camps and signals meaningful upside for ongoing exploration. In hockey terms, these Mud Lake results, combined with our success in expanding the Gold Rock target area, our early exploration success at Sherridon and Hyndman, would be considered a ‘haul’ scored by Dryden Gold in 2025.”
Mud Lake was first tested through the Company’s 2024 mapping campaign. Structural controls and surface expression at Mud Lake showed potential for similar mineralization to the Big Master and Elora Gold Systems in the Gold Rock target area. The mapping program from 2025 followed the mineralized trend further north where a sizable shear zone intersects favourable host rocks (Figure 1).
Figure 1: Geology map of Gold Rock and Mud Lake Target Areas
The geological interpretation for the expanded Mud Lake footprint is still on-going. Initial findings from the mapping and drill program show a flexure or bend in the mineralized trend. This geometry is common in shear zone systems and had been hypothesised by the geology team. The 2025 mapping confirmed this geometry where weather resistant quartz-feldspar porphyry (“QFP”) rocks outcropped hosting mineralization. The 2024 mapping program and 2025 drill holes targeted the southern portion of Mud Lake where narrow vein structures outcrop and have a very similar appearance to the Big Master system at Gold Rock. Samples from North Mud Lake indicate broader mineralization throughout the QFP (Figure 2). The geology team theorizes that the Pincher deformation zone may act like the Elora Shear at Gold Rock and host wider zones of mineralization. Unfortunately, like the Elora Shear, the Pincher deformation zone does not outcrop and will have to tested through drilling. The geology team will continue to analyze the data collected from the summer Mud Lake program to plan permitting and further testing at Mud Lake.
Figure 2: New results and geology of Mud Lake and North Mud Lake extension
Table 1: Mud Lake Drill Results
| Target Area | Drillhole | From | To | Length (m)* | Grade (g/t Au) | |
| Mud Lake | DML-25-001 | 272.00 | 297.10 | 25.10 | 0.33 | |
| 293.80 | 297.10 | 3.30 | 2.18 | |||
| Mud Lake | DML-25-002 | 76.50 | 77.00 | 0.50 | 43.10 | |
| 229.90 | 231.00 | 1.10 | 2.24 | |||
| Mud Lake | DML-25-003 | 69.00 | 73.04 | 4.04 | 0.83 | |
| Including | 71.21 | 73.04 | 1.83 | 1.63 | ||
| Mud Lake | 191.80 | 192.80 | 1.00 | 0.30 | ||
| DML-25-004 | 248.30 | 249.30 | 1.00 | 0.26 | ||
| 340.00 | 342.00 | 2.00 | 0.45 | |||
| *Reported intervals are drilled core lengths, true width is unknow; assay values are uncut | ||||||
Table 2: Highlight surface sample results North Mud Lake
| Sample # | Easting | Northing | Gold (g/t) | Description |
| 1291084 | 523442 | 5479509 | 93.00 | Quartz-ankerite vein within quartz-feldspar porphyry with disseminated pyrite. |
| 1290291 | 523438 | 5479523 | 19.80 | Quartz-ankerite breccia vein within quartz-feldspar porphyry & pyrite |
| 1290841 | 523443 | 5479548 | 15.00 | Altered quartz-feldspar porphyry with small quartz-ankerite veinlets with fine grained pyrite |
| 1291066 | 523661 | 5479265 | 2.77 | Strongly ankerite and sericite altered wall rock with disseminated pyrite and quartz-ankerite vein |
| 1291074 | 523501 | 5479509 | 1.17 | Strongly foliated mafic volcanic rock with intense ankerite alteration. Sample hosted quartz-ankerite veins wide with pyrite |
| 1291083 | 523469 | 5479449 | 1.10 | Representative quartz-feldspar porphyry host rock sample with veining and disseminated pyrite mineralization. |
| 1291069 | 523496 | 5479372 | 0.91 | Highly altered quartz-feldspar porphyry with quartz veining and pyrite mineralization |
| 1290852 | 523499 | 5479484 | 0.90 | Intense ankerite alteration with sericite alteration, minor quartz veinlets and disseminated pyrite |
| 1290849 | 523499 | 5479484 | 0.86 | Quartz-ankerite vein with pyrite in the vein. |
| 1290847 | 523498 | 5479492 | 0.76 | Quartz-feldspar porphyry with minor veining and very fine-grained disseminated pyrite. |
| 1290839 | 523456 | 5479556 | 0.68 | Quartz-feldspar porphyry with quartz-ankerite breccia veining and pyrite mineralization. |
| 1290853 | 523499 | 5479484 | 0.68 | Intense sericite alteration with quartz-ankerite stringer veinlets and pyrite mineralization. |
| 1290817 | 523926 | 5480166 | 0.66 | Quartz vein with intense ankerite alteration on contacts with minor tourmaline and pyrite. |
| 1291088 | 523478 | 5479432 | 0.63 | Quartz-feldspar porphyry with quartz veining |
| 1291067 | 523661 | 5479265 | 0.63 | Sample of vein material with wall rock being strongly foliated. Sample is ankerite, chlorite, sericite altered with fine disseminated pyrite |
| 1291087 | 523442 | 5479509 | 0.63 | Quartz breccia with strong ankerite alteration and disseminated pyrite |
| 1291064 | 524067 | 5479342 | 0.57 | Sample of vein material with wall rock being strongly chlorite and sericite altered with sulphides |
| 1291075 | 523501 | 5479509 | 0.56 | Sample mostly quartz-ankerite vein with pyrite within a quartz-feldspar porphyry dyke |
| 1290842 | 523443 | 5479548 | 0.55 | Quartz-ankerite vein with minor strongly altered wall rock and rusty pyrite mineralization. |
| 1290290 | 523457 | 5479486 | 0.54 | Quartz-feldspar porphyry with quartz-ankerite breccia veins hosting pyrite. |
| Sample locations are in NAD 83 Zone 15 UTM coordinates | ||||
Marketing Update
Together with the team at the KE Report, Dryden Gold will be hosting a webinar on December 4, 2025, at 9:30am PT/12:30pm ET for a 2025 overview of our exploration program and some details about our upcoming key initiatives for the 2026 drill program. Registration is free, please click here to sign up.
Qualified Person
The technical disclosure in this news release has been reviewed and approved by Maura J. Kolb, M.Sc., P.Geo., President of Dryden Gold and a Qualified Person as defined by National Instrument 43-101 of the Canadian Securities Administrators.
Analytical Laboratory and QA/QC Procedures
The Company is drilling NQ size core. Samples are cut in half, with half going to the lab for analysis and half kept as a record. True thickness/widths of the mineralization are unknown, result intervals are reported as the drilled core lengths unless otherwise stated. All sampling completed by Dryden Gold Corp. within its exploration programs is subject to a Company standard of internal quality control and quality assurance (QA/QC) programs which include the insertion of certified reference materials, blank materials, and a level of duplicate analysis. Drill samples from the 2024 and 2025 program were sent to Activation Laboratories in Dryden Ontario, with sample preparation and analysis in Dryden, where they were processed for gold analysis by 50-gram fire assay with an atomic absorption finish and over limits determined by Fire Assay with a gravimetric finish. Select samples were analyzed using metallic screens. Activation Laboratories systems conform to requirements of ISO/IEC Standard 17025 guidelines and meets assay requirements outlined for NI 43-101.
Table 3: Drill Hole Information. All coordinates are in NAD83/Zone15N
| Hole Number | Easting | Northing | Elevation (m) | Azimuth (°) | Dip (°) | Actual Depth (m) | Core Size |
| DML-25-001 | 523,761 | 5,479,050 | 429 | 308 | -45 | 305 | NQ |
| DML-25-002 | 523,880 | 5,478,963 | 419 | 313 | -45 | 272 | NQ |
| DML-25-003 | 523,394 | 5,478,696 | 422 | 280 | -45 | 242 | NQ |
| DML-25-004 | 523,656 | 5,478,658 | 421 | 347 | -45 | 398 | NQ |
ABOUT DRYDEN GOLD CORP.
Dryden Gold Corp. is an exploration company focused on the discovery of high-grade gold mineralization listed on the TSX Venture Exchange and on the OTCQB marketplace. The Company has a strong management team and Board of Directors comprised of experienced individuals with a track record of building shareholder value through property acquisition and consolidation, exploration success, and mergers and acquisitions. Dryden Gold controls a 100% interest in a dominant strategic land position in the Dryden District of Northwestern Ontario. Dryden Gold’s property package includes historic gold mines but has seen limited modern exploration. The property hosts high-grade gold mineralization over 50km of potential strike length along the Manitou-Dinorwic deformation zone. The property has excellent infrastructure, enjoys collaborative relationships with First Nations communities and benefits from proximity to an experienced mining workforce.
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