Infinitum Copper Corp. report results from diamond drilling at its flagship project, La Adelita in Sonora and Sinaloa states, Mexico. Drill hole AD-22-0019 returned 32.25 metres (m) of 1.01% copper (Cu), 0.52 grams per tonne (g/t) gold (Au) and 39.69 g/t silver (Ag) or 1.74% copper equivalent (CuEq)1 starting at 36.65 m downhole in the Cerro Grande zone. Drill holes AD-22-0019 and AD-22-0020A were collared on the same pad, approximately 110 m
south of previously reported holes AD-22-0017 and 0018. At 32.25 m true width, the reported interval in drill hole AD-22-0019 is 58% wider than the comparative interval in hole AD-22-0018 to the north. In both areas, the highest grade copper-gold-silver mineralization is associated with semi-massive to massive magnetite and is still open along strike and to depth. Drill hole AD-22-0019 This hole cut a true width of 32.25 m of pervasive-garnet-magnetite skarn grading 1.01% Cu, 0.52 g/t Au and 39.69 g/t Ag or 1.74% of CuEq starting only 36.65 m down hole. The skarn alteration is dominated by grossularite-andradite garnet with 5% to 20% associated magnetite. Copper mineralization associated with the skarn consists of chalcocite, chalcopyrite and bornite disseminated in the matrix between crystalline garnet and in later quartz-calcite veinlets. Minor chrysocolla with native copper is also observed in patches and within fractures. A petrographic study of drill core from this program has identified electrum (a natural alloy of gold and silver) associated with magnetite and hematite. Drill hole AD-22-0020A This hole was drilled below hole AD-22-0019, at a steeper angle, looking for the down dip continuation of the mineralization intercepted by the previous hole. The mineralized zone was 19.30 meters true width, grading 0.54% Cu, 0.31 g/t Au and 23.28 g/t Ag for an average of 0.97% CuEq. The associated skarn alteration is very similar to the previous drill hole with pervasive grossularite-andradite garnet associated with high magnetite content. The copper minerals observed in order of abundance are chalcopyrite, bornite and chalcocite, with minor chrysocolla on fractures.