Interra Copper Corp. announce initial Drilling Results from the Cathedral Area at its 20,600 hectare Thane Property, located on traditional territory of the Takla and Tsay Keh Dene First Nations in North-Central B.C. Results are from drill holes TH21-1, TH21-2 and TH21-5, which tested the northern portion of the Cathedral Zone?s IP chargeability anomaly. All three holes intersected indicator low grade copper-gold and moderate grades of molybdenum mineralization. Mineralization styles intersected within the drill holes consists of disseminated, vein and localized semi-massive copper mineralization at shallow to moderate depths within the Cathedral Zone. Localized quartz-chalcopyrite-molybdenum fractures and vein mineralization has also been intersected within the drilling campaign. Drilling within the Cathedral Zone was focused on the following; To test a 600 square meter IP chargeability high (up to 45 mV/V with a background of 5) within a highly K-spar and albite altered and resistive diorite to monzonite host; coincident surface copper-gold outcrop mineralization within magnetic high and low areas and localized increased copper -gold -arsenic soil analysis on four east-west trending and 2 north south trending IP/soil lines. A plan map and cross section of these holes with drill results are included below. See figure 3 for plan view of relevant drill holes, and figures 4 and 5 for section view of the drill holes illustrating the mineralized intercepts. Interra?s goals at the Cathedral Area in 2021 included; confirming and expanding copper and gold mineralization at depth from previous surface exploration programs; testing sub-surface chargeability and resistive high targeted areas observed within the 2019 and 2020 IP programs; and drilling angled holes across interpreted porphyry related alteration and associated mineralization and structural zones. The results to date have confirmed; porphyry related K-spar and albite alteration and structurally controlled quartz-sulphide vein style mineralization is observed at depth at Cathedral; Copper-gold and molybdenum mineralization is coincident with sub-surface high chargeability and K-spar-albite-quartz altered highly resistive areas observed within the 2019 and 2020 IP programs; sulphides of pyrite, chalcopyrite and localized chalcocite and bornite occur as quartz-sulphide veins and fractures and disseminations, proximal to intrusive contacts, shear structures and within localized magnetite veins and breccias; copper and gold mineralization at depth is at reduced grades to samples collected from the surface, which may be due to secondary supergene enrichment of the surface samples; mineralization and associated alteration within the reported intervals above are hosted within the Thane Creek diorite and the Duckling Creek monzonite to syenite intrusive phases of the Hogem Batholith; both sulphides and magnetite are noted to occur within areas of high chargeability and equally within areas of magnetic high and magnetite destructive low areas and mineralization within Thane and Duckling Creek suites of rocks may be related to late Mesilinka granitic intrusive phases. Results from the remaining drill holes within the Cathedral Area are pending and will be released later this month and next.