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

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Vancouver, British Columbia--(Newsfile Corp. - March 17, 2025) - Kenorland Minerals Ltd. (TSXV: KLD) (OTCQX: KLDCF) (FSE: 3WQ0) ("Kenorland" or the "Company") is pleased to announce the commencement of the maiden diamond drill program at the Hunter Project, located in the southern Abitibi greenstone belt of Quebec and held under an option agreement with Centerra Gold Inc. ("Centerra").

2025 Winter Exploration Program

The Winter 2025 exploration campaign and budget have been approved by Centerra for the maiden drill program at the Hunter Project. The program will include up to 4,300m of diamond drilling as an initial test of the targets identified through systematic exploration carried out since 2021. Two phases of drill-for-till sonic drilling in 2022 and 2024 identified a large multielement Au-Cu-Mo-Ag-W-Bi geochemical anomaly, both in glacial till and bedrock sampling over a 3.5 by 2.0 kilometre footprint, where bedrock alteration remains fully concealed beneath thick overburden. Kenorland remains operator of the Project, with drilling activities expected to conclude in early April.

Figure 1. Plan map of target area with planned drill hole locations

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Priority Target Area

Systematic, property-wide exploration at the Hunter Project included a VTEM survey flown in 2021, followed by a drill-for-till sonic program completed in 2022. Priority target areas identified for follow-up were advanced through the completion of a high-resolution airborne magnetics survey in 2023, and a detailed sonic drill program and induced polarisation ("IP") survey in 2024 ahead of drill targeting.

Underlying geology of the target area includes stratigraphy dominated by felsic volcanic rocks, which are intruded by multiple felsic-intermediate porphyritic intrusive rock phases. These intrusive phases are focused within an interpreted north-south trending structural corridor coeval with the syn-volcanic Poularies Batholith. Widespread silica-epidote-sericite±K-feldspar alteration within both volcanic and intrusive rocks is associated with variable quartz, quartz-sulphide, and sulphide veining. Sulphide mineralisation includes pyrite with lesser chalcopyrite and molybdenite, occurring as fine-grained disseminations to vein controlled blebs and stringers. Mineralisation within the target area is interpreted to be intrusion related, which may be syn-volcanic (disseminated sulphide to VMS type mineral systems), or related to younger magmatism similar to the Duparquet gold deposit 6.5 kilometres to the south, located along the Destor-Porcupine Fault Zone.