Interra Provides Rip Copper Molybdenum Project Exploration Update

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Vancouver, British Columbia--(Newsfile Corp. - April 26, 2024) - Interra Copper Corp. (CSE: IMCX) (OTCQB: IMIMF) (FSE: 3MX) ("Interra" or the "Company") is pleased to provide detail of the first phase exploration program at the Rip Copper Project (the "Project" or "Rip") in the Stikine region of British Columbia. The Rip Project is situated approximately 33 km northeast of Imperial Metals' past producing Huckleberry copper-molybdenum ("Cu-Mo") mine (see Figure 1), which is presently on care and maintenance. Imperial Metals Corporation is exploring Huckleberry and its surrounding claims for additional Cu-Mo resources.

In late 2023, the Company first announced its option agreement with ArcWest Exploration Inc. ("ArcWest") to acquire an 80% interest in ArcWest's Rip Cu-Mo project. Interra can earn the first tier of its interest in the project by completing staged exploration work totalling C$2.0 million and direct payment of C$100,000 and annual share payments over 4 years until end of 2027. Interra is currently funded for, and anticipates, it will meet and likely exceed its 2024 and 2025 obligations for the earn-in of C$300,000 and C$500,000 in expenditures respectively with the budget outlined in this 2 stage program. The initial program is staged into 2 work phases: 1) A geophysical program to define drill targets, commencing in late April and; 2) A diamond drilling program tentatively scheduled for Q3/Q4 of 2024.

The stage 1 exploration program consists of an airborne magnetic survey flown by Precision Geosurveys followed by a 3D-IP survey to be completed by DIAS Geophysical The 3D-IP survey is designed to further delineate and potentially expand upon a historical chargeability anomaly identified on the project by Kennco in the late 1970s, as shown in Figure 2.

Shallow percussion drilling of this chargeability anomaly by Kennco intersected porphyry copper style alteration and anomalous Cu-Mo mineralization over a broad area. A lone diamond drill hole intersected anomalous Cu (0.07%) and Mo (0.005%) over 74m in strongly quartz-sericite-pyrite ("QSP") altered volcanic rocks cut by late feldspar porphyry and mineralized quartz diorite dykes; the bottom 64m consists of intrusive clast-rich polymictic breccia cut by abundant pyrite, gypsum and quartz veins with local secondary biotite. QSP, intermediate argillic ("IA") and propylitic alteration predominate in the holes, suggesting that the Kennco holes only tested the upper levels of a shallowly eroded porphyry Cu-Mo system.