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Kenorland Commences 2025 Winter Drill Program at the Chebistuan Project, Quebec

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Vancouver, British Columbia--(Newsfile Corp. - February 18, 2025) - Kenorland Minerals Ltd. (TSXV: KLD) (OTCQX: KLDCF) (FSE: 3WQ0) ("Kenorland" or the "Company") is pleased to announce the commencement of the Winter 2025 drill program at the Chebistuan Project (the "Project"), located in the northern Abitibi greenstone belt of Quebec, and held under an exploration agreement with Newmont Corporation ("Newmont").

Q1 2025 Winter Exploration Program

The Winter 2025 exploration program and budget have been approved by Newmont, which will include up to 3,500m of drilling across 9 drill holes at the Deux Orignaux target area. This second phase of drilling, follow-up to the initial program completed in early 2023, will test lateral and down-dip extents of the mineralised syenite intersected in drill hole 23DODD005, which returned 157.20m at 0.41 g/t Au including 20.61m at 0.97 g/t Au (see press release dated June 27, 2023). The program will also test additional targets, identified as potential syenite plugs based on geophysical characteristics. Kenorland remains operator of the Project, and drilling activities are expected to conclude early March.

Figure 1. Plan map of Deux Orignaux drilling highlights (previously reported) and planned drill hole locations

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Deux Orignaux Target Area

The Deux Orignaux target area is a grassroots prospect under an earn-in agreement with Newmont. Systematic, property wide geochemical surveys completed in 2020 covering the original 159,690 hectare project and detailed till geochemical surveys in 2021 defined the target area containing anomalous gold and multi-element geochemistry, and gold grains in glacial overburden. The defined target area was followed up with a detailed airborne magnetics survey, and an induced polarization (IP) survey in 2022 ahead of drill targeting.

The mineralised intrusion at Deux Orignaux, defined by coincident resistivity, chargeability, and magnetic anomalies, was intersected along the regional contact between a clastic sedimentary basin (Opemiska Group) and volcanic rocks, marked by a first order basin bounding structure and Timiskaming type polymictic conglomerates. The intrusion is mineralised throughout with minor disseminated pyrite and trace sphalerite associated with pervasive potassic and albite alteration (Kspar-albite-quartz-hematite-carbonate-sericite alteration assemblage).

Figure 2. Cross section of 2023 Deux Orignaux drilling (geology and previously reported assays, looking east)