Eagle Plains Resources Partner Earthwise Minerals Intercepts Mineralization in all Holes at the Iron Range Precious Metals Project, BC.

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CRANBROOK, BC / ACCESS Newswire / June 16, 2026 / Eagle Plains Resources Ltd. (TSXV:EPL) (OTCQB:EGPLF) ("EPL" or "Eagle Plains") is pleased to announce that partner Earthwise Minerals Corp. (CSE:WISE) (FSE:966) (OTCQB:EWISF) ("Earthwise" or "WISE") has completed the diamond drilling program at Eagle Plains' 100% owned Iron Range Project, SE British Columbia. Earthwise holds the exclusive option to acquire up to an 80% interest in the Iron Range Project. The 20,021 ha Iron Range Project is considered by management of both Eagle Plains and Earthwise to hold excellent potential for the presence of structurally controlled gold-silver mineralization, iron-oxide copper-gold ("IOCG") and Sullivan-style lead-zinc-silver sedimentary-exhalative ("sedex") mineralization. The property is owned 100% by Eagle Plains, with part of the property subject to an underlying 1.0% Net Smelter Royalty held by a third party. The drill program was managed by Terralogic Exploration Inc. and diamond drilling was contracted to QB Drilling. The 2026 drill program was designed to infill historical mineralized intercepts and assess continuity of mineralization along trend at the Talon Zone structure, where 2010 drilling by Eagle Plains intersected 2 intervals of strong and continuous mineralization including 14.0m grading 5.1g/t gold, 1.86% lead, 2.1% Zinc, 75.3g/t silver and 7.1m grading 8.13g/t gold, 2.84% lead, 3.07% zinc, 86.6g/t silver (DDH IR10010). See Iron Range Drill Plan Map here Hole ID Easting* Northing* Elev. (m) Az. (°) Incl. (°) Length (m) IR26053 543397 5445640 1371 270 -56 410 IR26054 543398 5445641 1371 295 -61 383 IR26055 543216 5445651 1369 223 -67 389 TOTAL 1182 *Collar locations projected in NAD83 UTM Zone 11N DDH IR26053 was designed to cross-cut the Talon Zone structure, infilling historical holes IR11011 and IR11015 (125m spacing at target depth). The hole was collared in the middle Aldridge Formation, intercepting the regionally significant lower-middle Aldridge Formation Contact (LMC) at approximately 120m depth. The Talon Zone structure, intercepted between 280-396m, is defined by strong silica-feldspar alteration associated with dense, chaotic quartz-feldspar-ankerite veins. Polymetallic mineralization (pyrrhotite-pyrite-sphalerite-galena-arsenopyrite-sulfosalts) was noted throughout the structural zone within veins, as fracture infill and forming localized ...

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