Miata Intersects 43.0 m at 2.42 g/t Au, Including 4.0 m at 17.11 g/t Au at Jons Trend and Confirms Continuity with Big Berg at Sela Creek, Suriname

Results from four holes drilled in between Jons Trend and Big Berg confirm that these discoveries are connected and are part of a larger mineralized system. Spanning approximately 1.5 km in length, the combined zones remain open along strike and at depth, and Miata will continue to drill to establish further continuity and define the corridor’s limits.

Gold in each of the targets throughout the system is hosted in a moderately southwest-dipping, southeast-trending folded metasedimentary package that displays shear zones along fold limbs and hinges with pervasive silica, sericite, and biotite alteration. These zones host repeating extensional quartz vein arrays associated with sulfide mineralization dominated by pyrite and pyrrhotite. The mineralized system remains open along the tested WNW–ESE axis in both directions and at depth.

The latest Jons Trend results comprise holes 26DDH-JT-024 and 26DDH-JT-025, drilled in the southeastern and northwestern parts of the trend, respectively. 26DDH-JT-025 was a 130 m step-out from 26DDH-JT-023 (released September 29, 2026, returning 35.25 m at 3.41 g/t Au), and confirmed the continuation of a broad, high-grade vein zone. The hole returned two broad mineralized intervals:

JT-024 returned several narrower intervals, including 3.0 m at 1.28 g/t Au from 115.2 m, 3.0 m at 1.61 g/t Au from 203.0 m and 10.99 m at 0.75 g/t Au from 229.5 m. The results show structurally controlled repeating vein array that is continuous and open at depth and along strike.

26DDH-GH-001 tested a mineralized vein zone parallel to and approximately 500 m east of Jons Trend. Four holes, 26DDH-GH-002 through GH-005, tested the central corridor between Jons Trend and Big Berg. All holes intersected multiple mineralized vein zones. Bedrock results include:

Near-surface saprolite results include 14.0 m at 1.09 g/t Au in 26DDH-GH-002, 20.1 m at 1.19 g/t Au in GH-004 and 9.5 m at 0.80 g/t Au in 26DDH-GH-005. Similar to mineralization at Jons Trend and Big Berg, these holes show mineralization hosted in moderately southwest-dipping quartz vein arrays that are associated with pervasive silica, sericite, and biotite alteration and pyrite plus pyrrhotite. As well as confirming a new vein zone in the intervening corridor, these drilling results clearly link the Big Berg and Jons Trend discoveries.

Results from 26DDH-BB-014 through BB-020 returned mineralized intervals to the west and northwest of existing drilling at Big Berg. Highlights include two broad intervals in 26DDH-BB-015 (13.0 m at 1.64 g/t Au from 60.0 m and 14.1 m at 2.23 g/t Au from 80.5 m), as well as 18.45 m at 1.37 g/t Au from 223.8 m in 26DDH-BB-017. The results show mineralization in multiple holes and at different depths, expanding the known mineralized footprint of Big Berg by approximately 150 m in both west and northwest directions. The next planned Big Berg drilling phase is designed to further infill between Jons Trend and Big Berg and to test the southeastern extension of known mineralization.

Drillholes BB-020, GH-002, JT-024, and JT-025 were crushed at the preparation lab on Sela Creek. The Sela Creek preparation lab uses heavy-duty jaw-crushers to reduce regular half core samples to a fine crush, whereby at least 75% of the sample can pass a 2.2 mm screen. The uniformly crushed sample is then put through a riffle-splitter; resulting in a ca. 300-500 g sample, to be shipped to the Filab in Paramaribo for further sample preparation (pulverizing) followed by analysis, and the remaining reject is kept in dry storage for future quality control or duplicate testing. The Company inserts regular crush duplicates to ensure the split sample is representative of the entire section of drill core. The remainder of the samples were fully processed at FiLAB Suriname, a commercial certified laboratory under ISO 9001:2015. At FiLAB, 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 (AA) finish. For samples that return assay values over 5.0 grams per tonne (g/t) Au, 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 Au, metallic screen analysis is conducted on the coarse reject material. Miata Metals inserts certified reference standards, as well as blanks and crushed core duplicates, in the sample sequence for quality control and assurance. All samples passed QAQC.

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.

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 km2 Sela Creek Gold Project with an option to acquire a full 100% interest, 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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