Kutcho Copper Provides Updates on Project Enhancements at its High-Grade Copper-Zinc Project

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Vancouver, British Columbia--(Newsfile Corp. - March 24, 2025) - Kutcho Copper Corp. (TSXV: KC) (OTCQX: KCCFF) ("Kutcho Copper" or the "Company") is pleased to provide positive updates on metallurgical and geological understanding, and looks forward to the next steps planned for 2025 at its feasibility stage, high-grade copper-zinc development project located in north-western British Columbia.

Vince Sorace, President & CEO of Kutcho Copper stated: "Kutcho Copper finished 2024 with several fundamental accomplishments, and we anticipate that 2025 will be another year of progress for the Company. We are uniquely positioned with a feasibility-stage, high-grade, low-cost copper-zinc development project located in a Tier 1 jurisdiction that has potential for significant exploration upside and continued engineering optimization. We will continue to explore and expand on opportunities for the Kutcho project on our path towards a construction decision.

Since completion of the 2021 Feasibility Study ("FS"), Kutcho Copper has been attending to improvement recommendations and risk reduction studies documented in the FS. Kutcho Copper is pleased to report a number of additional milestones from its optimization program, including:

  • Oxide Ore

A simple oxide model was included in the 2021 Mineral Reserve; one of the recommendations was a detailed review of the extent and intensity of oxide mineralization. Oxidation of mineralization can lead to poorer recoveries of metals to concentrates and operational complexity. Understanding degree of oxidation and precise location of it, is important for project performance.

Since 2021, detailed logging of existing core photographs from the Main deposit was completed using a six-point scale for the degree of weathering. Results of this detailed logging indicate that the indurated massive sulphide mineralization at shallow depths has minimal weathering which is generally limited to oxidation along late faults and fractures. In practical terms, it appears that the massive sulphide mineralization was protected from weathering due to its generally massive nature. Surface water infiltration, which causes weathering, preferentially travelled down through the rock along faults and planes in north dipping, fissile hanging wall schists parallel and above the sulphide horizon.

A cut through the weathering profile overlying sulphide mineralization is displayed on Figure 1, here approximately 1 m of moderately weathered material overlies weakly weathered zinc sulphide of the Main deposit, confirming the new detailed modelling, this is a significant reduction from the average oxide thickness of 20 m predicted in the 2021 oxide model.