Colibri Samples 4.64 g/t Au at the EP Project, Caborca Gold Belt, Sonora, Mexico

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Dieppe, New Brunswick--(Newsfile Corp. - August 22, 2024) - Colibri Resource Corporation (TSXV: CBI) (OTC Pink: CRUCF) ("Colibri" or the "Company") is pleased to report the results of geological mapping and outcrop sampling recently completed on the Plomo property at the EP gold project located in the Caborca Gold Belt, NW Sonora. Highlights include outcrop grab samples which returned values up to 2.99 grams per tonne ("g/t") Au which extend the footprint of surface mineralization at the San Perfecto target approximately 350 meters ("m") and samples from La Culebra target area that returned values up to 4.64 g/t Au occurring over a strike length of approximately 650 m.

Ian McGavney, President & CEO of Colibri commented: "The southwest part of the San Perfecto area is on the books as a priority drill target for Colibri. We are extremely pleased with the results of the recent mapping and sampling at San Perfecto which expanded the area of known mineralization and thereby the scope and potential of our drill target. The work at La Culebra has confirmed historical sampling and demonstrates discovery potential over a 650 m strike length which remains open. We are very encouraged by the common copper occurrences at La Culebra. Reporting these new results from our most advanced, highest priority target and from one of our earlier stage targets clearly demonstrates the significant discovery potential of the large EP property position"

San Perfecto Target

Work recently completed at the San Perfecto target area includes geological mapping and the collection and assay of 29 outcrop grab samples. Results include 14 samples which returned values greater that 0.1 g/t Au, including 9 samples greater than 0.5 g/t Au and 6 samples greater than 1.0 g/t Au, that define a cluster of mineralized outcrops which extend the footprint of known surface mineralization at San Perfecto approximately 350 m to the east-southeast. The footprint of mineralization at San Perfecto is now approximately 1,250 m by 700m and remains open to the southeast (see figure 1). The mineralization is hosted by moderately to strongly foliated and altered diorite. Alteration consists of strong silicification and sericite with disseminated and oxidized fine grained pyrite. Quartz micro-veinlets are locally recognized in the higher-grade samples. The diorite host rock and style of mineralization is continuous for approximately 1 km to the northeast at the San Perfecto target. The domain of foliated, altered, and mineralized diorite is coincident with a northeast magnetic low trend and overlies a strong apparent chargeability anomaly.