Wealth Minerals Ltd. discovered two additional semi-massive sulphide horizons exposed along the Cascade Creek deactivated logging road, on the Lardeau-Goldsmith claim block at the north end of its Kootenay Project, located south of Revelstoke, British Columbia . The disseminated and semi- massive sulphide zones are steeply dipping and may be a fold repetition, or two parallel horizons . Both gossanous outcrops contain mostly pyrite-pyrrhotite with minor chalcopyrite and sphalerite. The Goldsmith discovery, like the Lost Ledge discovery, was made while geologists were investigating the extension of an electromagnetic ("EM") conductive feature. The sulphide mineralization at Goldsmith is also associated with a copper-zinc-nickel soil anomaly (historical) along strike of the conductor. Additional stronger conductors were identified by the 2022 VTEM survey farther upstream and will be field evaluated next spring. In addition, the southeast extension of the newly discovered sulphide horizon above Lost Ledge creek canyon was mapped and sampled at the bottom of the canyon, where the zone is several metres thick. Field work confirms that the zone links up to the copper soil anomaly on the main grid, which in turn is associated with the 2.5 km long Ni-Cu-Zn and magnetic anomaly at the main showing. The Kootenay nickel-copper-zinc-gold property in southeastern British Columbia (the "Kootenay Project") comprises two separate claim blocks including the Lardeau-Goldsmith claim block, covering 6,951 hectares, and the Ledgend claim block covering 1,728 hectares . The claims cover precious and base-metal prospective lower Paleozoic greenstone and phyllite units within the Index Formation of the Lardeau Group, which hosts Besshi-type volcanogenic massive sulphide ("VMS") deposits north of Revelstoke, including the past-producing Goldstream Cu-Zn mine. On August 17, 2022, the Company announced the results of recent geophysical studies ("Studies"), including the analysis of a completed VTEM survey that covered the north end of theLedgend property, as well as the entire Lardeau-Goldsmith block located 20 km to the north. On the Ledgend property, two significant, highly conductive electromagnetic ("EM") anomalies occur on the eastern edge of the geophysical survey grid and on strike with Ni-Cu-Zn soil and magnetic anomalies to the south. The strong conductors, with conductivity-thicknesses ("CTs") of >300 siemens, were interpreted by geophysicist Martin St. Pierre to be shallow (Northeast target) and outcropping (Lost Ledge target) massive sulphides. The Lost Ledge target turned out to be a previously undocumented outcrop of semi-massive sulphide that extends for 30 metres along strike along the canyon rim and is up to 6-metres thick and open along strike to the southeast. Pyrite, pyrrhotite, chalcopyrite, and sphalerite were visually identified in the outcrops. Follow-up channel-chip sampling utilizing an angle grinder collected an additional 10 samples; assay results are pending. The geophysical modeling indicates that this layer gets either more massive (higher sulphide content), and/or thicker as it plunges shallowly to the north under cover. Additionally, Vector Geological Solutions geologists found the down-strike, southeast continuation of the horizon into Lost Ledge creek and collected three chip samples across the layering (Figure 3). At the creek, the total true width is about 10m, with the upper 6-7m section comprising disseminated pyrite±chalcopyrite and the lower 2m comprising semi-massive pyrite-
pyrrhotite-chalcopyrite±bornite.