Miata Metals Corp. (TSX-V: MMET) (FSE: 8NQ) (OTCQX: MMETF) is pleased to announce additional drill results from its ongoing, 25,000 m diamond drilling program at its Sela Creek Gold Project in Suriname.
The 2026 drill program continues to advance Miata’s interpretation of Sela Creek as a large, structurally controlled gold system with multiple centres of gold mineralization. At Jons Trend, the deepest test of the mineralized zone completed to date successfully extended five known vein zones by 50 meters down-dip to a vertical depth of 250 m. The Company also discovered an additional zone below the formerly modeled gold mineralization. All of these vein zones remain open at depth. The drill hole returned a broad intercept across several vein zones of 63 m at 1.44 g/t Au. At Big Berg, continued step-out drilling returned both broad and higher-grade intercepts, 400 m to the southwest along strike from Jons Trend. Geological data continues to point towards the continuation of Jons Trend and Big Berg, in a single mineralized corridor of 1,300 m strike length.
Highlights:
“JT-016 represents one of the most important holes drilled at Sela Creek to date,” said Dr. Jacob Verbaas, CEO of Miata Metals. “It successfully extended five known mineralized vein zones, identified a new deeper zone below our existing geological model, and returned a broad intercept of 63 m at 1.44 g/t Au. The hole increased the down dip extent by 50 m and the true vertical depth of the system to 250 m. The result demonstrates that the system continues to grow vertically and remains open for further expansion.”
“Big Berg also continues to deliver encouraging results and is increasingly demonstrating characteristics similar to Jons Trend, including repeating mineralized zones and strong continuity. Together, these results strengthen our view that Sela Creek hosts an expansive mineralized corridor with multiple centres of gold mineralization and significant room for continued growth.”

Figure 1. Plan view of Jons Trend and Big Berg with geological sections (Figures 2 to 3) lines indicated.
Jons Trend Drilling:
26DDH-JT-016 was designed to test the deepest portion of the Jons Trend system evaluated to date and extend gold mineralization to depth. The results are highlighted by a broad mineralized interval interpreted to represent the deeper projection of two thick vein zones that coalesce into a continuous mineralized intercept at depth:
The broad intercept is interpreted to represent the down-dip convergence of multiple mineralized vein zones that were previously modeled as separate structures higher in the system. This observation supports the emerging geological model that individual mineralized zones and sub-parallel high-strain shear structures, may merge into broader mineralized envelopes at depth.
Drilling also intersected a newly identified deeper vein zone below the previous geological model:
This lower intercept occurs beyond the previous geological model and represents a new zone of mineralization at depth. In total, DDH-JT-016 is interpreted to have extended five existing vein zones down-dip and identified one new deeper zone, reinforcing the continuity and scale potential of Jons Trend. The mineralized zones remain open at depth, with ongoing drilling designed to further test the depth, continuity and potential strike extensions of Jons Trend.

Figure 2. Cross section of central Jons Trend (A-A’ on Figure 1) showing 26DDH-JT-016 and the modeled vein zones. All vein zones remain open to depth.
Big Berg Drilling:
Big Berg continues to establish itself as a growing second centre of mineralization within the Sela Creek system. At Big Berg, holes 26DDH-BB009 and 26DDH-BB010 were drilled as approximately 20 m step-outs from previously reported holes BB-003 and BB-004. The holes were designed to test continuity along strike and down dip of the known mineralized vein zones.
Hole 26DDH-BB-009 intersected:
Hole 26DDH-BB010 intersected:

Figure 3. Cross sectional view of Big Berg (B-B’ on Figure 1) showing 26DDH-BB-009 and 010. Big Berg displays similar geological characteristics to Jons Trend.
Together, these holes demonstrate the range of mineralization styles developing at Big Berg. 26DDH-BB-009 highlights the potential for wider zones of gold mineralization and is characterized by folded veins and host-rock sulphides, while 26DDH-BB-010 demonstrates higher-grade mineralization over concentrated intervals associated with shear-hosted veining. Both holes display strong banded alteration, including silica, biotite, ± white mica and chlorite, consistent with the mineralization style observed at Jons Trend.
2026 drilling at Big Berg has intersected nine discrete mineralized zones in ten holes, supporting the interpretation of a robust and expanding mineralized system with significant potential for further growth. Miata continues to evaluate the potential connection between Big Berg and Jons Trend, with results to date supporting Big Berg as a growing parallel centre of mineralization within the same broader gold-bearing structural corridor.
To date in 2026, Miata has completed approximately 10,300 m of drilling across several targets at Sela Creek, including Jons Trend, Big Berg, Puma West, Puma East, Stranger, Cambior, and Golden Hand. Results remain pending for several recently completed holes.
Importantly, grades and widths have been maintained as the system expands vertically, providing increasing confidence in the continuity and scale potential of Jons Trend.
Table 1.Latest Gold Assay Results
| Hole Id | From (m) | To (m) | Intercept (m) | Au (g/t) | Target | true width (m) |
| 26DDH-JT-016 | 16.5 | 21 | 4.5 | 1.07 | Jons Trend | sap |
| and | 57 | 57.78 | 0.78 | 0.65 | 0.6 | |
| and | 111 | 117 | 6 | 0.75 | 4.9 | |
| and | 129 | 130 | 1 | 0.54 | 0.9 | |
| and | 134 | 136.4 | 2.4 | 0.67 | 2.3 | |
| and | 149 | 161.1 | 12.1 | 0.69 | 11.4 | |
| including | 155 | 156 | 1 | 2.09 | 0.9 | |
| and | 167 | 230 | 63 | 1.44 | 54.6 | |
| including | 169 | 170 | 1 | 2.69 | 0.9 | |
| including | 173 | 177 | 4 | 1.85 | 3.5 | |
| including | 184 | 188 | 4 | 4.41 | 3.5 | |
| including | 198 | 199 | 1 | 5.78 | 1.0 | |
| including | 205.39 | 214 | 8.61 | 2.48 | 8.3 | |
| including | 217.2 | 220 | 2.8 | 3.49 | 2.7 | |
| including | 228 | 230 | 2 | 2.94 | 1.9 | |
| and | 248.5 | 249.41 | 0.91 | 3.43 | 0.9 | |
| and | 254 | 256 | 2 | 0.58 | 1.9 | |
| and | 265 | 270.29 | 5.29 | 1.56 | 5.1 | |
| and | 278.21 | 281 | 2.79 | 0.60 | 2.7 | |
| 26DDH-JT-017 | 58.53 | 60 | 1.47 | 3.75 | Jons Trend | 1.2 |
| and | 170 | 171.5 | 1.5 | 0.58 | 0.8 | |
| and | 173 | 174.34 | 1.34 | 0.56 | 0.7 | |
| and | 183 | 184.5 | 1.5 | 0.59 | 0.8 | |
| and | 189 | 190.5 | 1.5 | 0.57 | 0.8 | |
| and | 193.5 | 197 | 3.5 | 1.15 | 2.2 | |
| including | 193.5 | 195.35 | 1.85 | 1.95 | 1.2 | |
| and | 206.32 | 207.5 | 1.18 | 0.69 | 0.8 | |
| and | 274 | 276 | 2 | 0.62 | 1.3 | |
| 26DDH-JT-018 | 24.55 | 25.55 | 1 | 0.60 | Jons Trend | 0.5 |
| and | 57.3 | 63.5 | 6.2 | 0.50 | 3.1 | |
| and | 105.3 | 109.6 | 4.3 | 0.62 | 2.5 | |
| including | 106.3 | 107.3 | 1 | 1.36 | 0.6 | |
| and | 140.5 | 143.5 | 3 | 0.51 | 1.9 | |
| and | 183.5 | 185 | 1.5 | 0.50 | 1.0 | |
| 26DDH-BB-009 | 35.5 | 40.5 | 5 | 0.82 | Big Berg | 4.7 |
| and | 83.5 | 85 | 1.5 | 0.67 | 1.4 | |
| and | 104.3 | 111.5 | 7.2 | 1.13 | 7.0 | |
| including | 107.1 | 108.1 | 1 | 3.53 | 1.0 | |
| and | 118 | 123.15 | 5.15 | 0.95 | 5.0 | |
| including | 120 | 121 | 1 | 3.05 | 1.0 | |
| and | 129.55 | 131 | 1.45 | 1.67 | 1.3 | |
| and | 149.5 | 182.5 | 33 | 1.03 | 29.9 | |
| including | 151 | 154.3 | 3.3 | 1.07 | 3.0 | |
| including | 163.5 | 171.5 | 8 | 2.91 | 7.3 | |
| 26DDH-BB-010 | 71 | 80.25 | 9.25 | 3.10 | Big Berg | 5.9 |
| including | 72.65 | 79 | 6.35 | 4.17 | 4.1 |
Table 2. Updated Collar Information.
| Hole ID | Easting* | Northing | Elevation (m) | Azimuth** | Dip | Length (m) |
| 26DDH-JT-016 | 754,832 | 418,085 | 106 | 348 | -55 | 300.17 |
| 26DDH-JT-017 | 755,245 | 417,751 | 113 | 353 | -48 | 278.62 |
| 26DDH-JT-018 | 755,257 | 417,897 | 114 | 350 | -65 | 210.30 |
| 26DDH-BB-009 | 755,693 | 417,504 | 112 | 355 | -53 | 188.60 |
| 26DDH-BB-010 | 755,620 | 417,511 | 112 | 355 | -48 | 177.42 |
All drill information is available through this link.
QAQC
Drill core samples are analyzed for gold at FILAB Suriname, a commercial certified laboratory under ISO 9001:2015. Samples are crushed and pulverized to 85% passing 88 µm prior to analysis using a 50 g fire assay (50 g aliquot) with an Atomic Absorption finish. For samples that return assay values over 5.0 grams per tonne gold, another cut was taken from the original pulp and fire assayed with a gravimetric finish. Samples with coarse visible gold or returning an assay value over 10.0 g/t gold, metallic screen analysis is conducted on the coarse reject material. Miata Metals inserts certified reference standards, as well as blanks and ¼ core duplicates, in the sample sequence for quality control and assurance.
QP Statement
The scientific and technical information in this news release has been reviewed and approved by Dr. Jacob Verbaas, P.Geo., a director of the Company and Qualified Person as defined under the definitions of National Instrument 43-101 – Standards of Disclosure for Mineral Projects.
About Miata Metals Corp.
Miata Metals Corp. (TSX-V: MMET) is a Canadian mineral exploration company listed on the TSX Venture Exchange, as well as the OTCQX (OTCQX: MMETF) and Frankfurt (FSE: 8NQ) Exchanges. The Company is focused on the acquisition, exploration, and development of mineral properties. The Company holds a 70% interest in the ~215 km2Sela Creek Gold Project with an option to acquire a full 100% interest in the Project, and a 70% beneficial interest in the Nassau Gold Project with an option to acquire 100%. Both exploration properties are located in the greenstone belt of Suriname.
On Behalf of the Board
Dr. Jacob (Jaap) Verbaas, P.Geo | CEO and Director
For Further Information, please contact:
Nikki McEachnie
Director of Investor Relations
nikki@miatametals.com
1-778-486-1500
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