Renforth Resources Inc. update shareholders on successful recent nickel prospecting on the McCart Property, near Iroquois Falls Ontario and the unexpected, mineralized occurrences at the very end of the last drill hole on Victoria. The McCart claims lie atop a thick ultramafic sequence. The large, broad ridges expose komatiites, peridotites and dunites, and run approximately NE-SW. Pillowed basalts are exposed in the southeastern area of the property. The ridge in the northern part of the property contains numerous blasted pits and trenches in a broad area along and across the northern property boundary. Additional blasted trenches and pits were found in the southeastern corner of the property as well. Samples taken during the Fall 2023 Prospecting program consisted primarily of ultramafic and mafic units with very fine sulfide mineralization. Twenty-eight samples were taken during the program, of which 10 samples returned assay values greater than 1000ppm Ni. Five samples were in the range of 1700-2230ppm Ni, with 2230ppm Ni from Sample M007452 being the highest assay value of this program. The last hole drilled at Victoria was continued, in typical fashion, to the sedimentary contact at the bottom of the hole. As the three mineralized horizons had already been intersected, undercutting, and continuing the mineralization encountered in the prior, shallower, hole SUR-23-56 down dip,
there was little expectation of the end of this hole. Two additional mineralized occurrences were found at the end of hole SUR-23-57 in two forms. The first is within the typical blue/green ultramafics, which as deep as 373m down the hole included dark grey-black bands of graphite and magnetite which returned mineralized values in XRF testing. The second occurrence is a zone of very intense carbonate-plagioclase alteration and recrystallization from 296.6-300.15m, only seen once before in any of Renforth's drilling at Victoria in SUR-21-16, significantly east of this hole.