Fidelity Minerals Corp. announced results from confirmatory sampling of nine (9) rock and outcrop exposures at the highly prospective Core Las Huaquillas precious and base metal property in northern Peru, and for which Fidelity holds a 44.5% interest and holds an option to acquire an additional 5.5%. The confirmatory sampling was completed as part of a site visit by Luc Pigeon B.Sc., M.Sc., P.Geo (the "Author"), a Qualified Person in the context of National Instrument 43-101 who is authoring a new NI 43-101 technical report on the Project as announced by the Company on October 7, 2021. The best result obtained was a sample collected from quartz veins exposed at the entrance of one of the underground working portals within the Los Socavones zone that returned a result of 9.653 g/t Au, 126 g/t Ag and 1.08 % Pb. The CLH Project features extensive historical exploration completed by Sulliden Exploration Inc. ("Sulliden") and others through 1999. This work included soil sampling, geophysics and over 5,700m of diamond drilling (26 drill holes), and the excavation of approx. 1,200m of underground development on three levels in the Los Socavones Zone. This work defined five (5) mineralised zones, consisting of four (4) mineralisation types including epithermal Au-Ag (Los Socavones), and porphyry Cu style mineralization (Cementerio and San Antonio) at the Project. The confirmatory sampling was completed by the Author as part of a site visit required to support the writing of the new NI 43-101 technical report. This included limited verification of geologic mapping, alteration, and geochemical sampling completed by Sulliden in 1999. The Author collected a total of nine (9) grab samples: three (3) north of the San Antonio zone, four (4) along road cuts within the Los Socavones and SanAntonio zones, and two (2) from exposed veins at the entrance portal of two (2) underground workings within the Los Socavones zone. The Author had previously visited the Cementario zone in 2011 and verified the geology and alteration at that time for another issuer. The Author confirms the following: Significant alteration occurs within both the Cementerio and San Antonio zones. Furthermore, the location of the diorite and alteration mapped by the Author concurs with the historical geological mapping; Two (2) underground working portal locations were measured using a hand-held GPS with a reported accuracy of 2m. The PSAD56 portal locations reported in the historical maps and reports are accurate with their transformed WGS84 X, Y values falling within the GPS error radius. This confirms that the locations reported by Sulliden were of excellent quality and must have been acquired by a sub- metre accuracy differential GPS or surveyed using benchmarks and a total station; Grab samples C001437 and C001438 collected from quartz veins exposed at two (2) underground working portals within the Los Socavones zone returned 1.062 g/t Au and 9.653 g/t Au respectively; Sample C001438 is also characterized by 126 g/t Ag and 1.08% Pb; Sample C001437 is composed of dark grey quartz with 6%-7% disseminated and veinlet pyrite; A minor amount of iron oxides are also present; Sample C001438 is composed of a milky quartz matrix cross-cut by grey quartz veinlets; and the rock contains approximately 6% disseminated pyrite and up 15% fracture- and vug-controlled iron oxides.