Renforth Resources Inc. delivered to shareholders the results from 21 holes drilled over a strike length of 2.2 kms at Victoria West, with each hole delivering mineralization and the four deeper holes demonstrating an increase in grade. The results reported on include the two 2021 drill programs and the results from resampling of the 2.5 holes drilled in 2020 in the intervals presented below. Surimeau is a wholly owned 260 km square property in the Pontiac, south of the Cadillac Break and contiguous to the Canadian Malartic Mine. There are 5 areas of known polymetallic mineralization on the property, including the Huston target, 18kms NW of Victoria West, where Renforth recently reported a grab sample assaying 1.9% Ni, 1.38% Cu, 1170ppm Co and 4 g/t Ag and several gold showings. Surimeau District Property hosts first exploration for nickel, copper, cobalt - 3 of the primary metals required for batteries and, in particular, Electric Vehicles. While still at a very early stage, the extent of the findings and the magnitude of additional potential within the 260 km square property, its known targets and unexplored prospective ground warranting further exploration, Surimeau presents new path for Renforth Resources in metals that are forecast to be in high demand as the EV and energy storage market grows. Victoria West, the first target to be drilled by Renforth, has a current mineralized strike length, comprised of Renforth's drilling and surface sampling, along with prior drilling and surface sampling by Lac Minerals and other historic operators, of 5km, co-incident with a mag high anomaly clearly visible on government geophysics, which continues to the east for 15kms, where it ends on the Surimeau property at the Colonie target, which hosts polymetallic mineralization. It is the opinion of management and consulting geoscientists that Renforth's results are sufficient to support historic results, confirming the strike length of Victoria West. To the east, within the 20km magnetic trend, the ground seems to be, upon brief field inspection, of low relief with little outcrop and unexplored, with no historic documentation available. The results of this drill program, including the measurement of magnetic susceptibility while logging core, demonstrate that the government survey is registering the magnetic signature of the nickel and cobalt bearing ultramafic body at Victoria West. Renforth's future plans include investigation of the 14km of magnetic anomaly between Victoria West and Colonie in order to determine whether the mineralized ultramafic mineralization occurring with the magnetic anomaly over a 5 km portion of the anomaly continues the length of the anomaly. Drilling has taken place at Victoria West in 3 different phases; October 2020 - a total of 2.5 holes were drilled in 194m using a track mounted drill which broke down 32m down the 3rd hole, ending the program. Each hole returned visible sulphides. March/April 2021 - a total of 15 holes were drilled in 3456m over a strike length of 2.2km, these holes were drilled south in pairs, designed to cross the north-south "width" of the east- west striking magnetic ultramafic body, targeted with the government aeromagnetic survey. June 2021 - a total of 4 holes were drilled in 773.2m, using the pads cleared for the prior drill program. These holes were each drilled north, at a steeper angle than the prior drilling, designed to undercut visually interesting results from the March/April drill program. Victoria West Assay Highlights: Presented below is a highlight table for the 4,423.2m drilled at Victoria West. The intervals given are as measured in the core box, true width is not known at this time. Intervals in blue denote long measured lengths, intervals in red denote higher grade results, provided to aid in a quick review. The mineralized body at Victoria West is currently interpreted to be an ultramafic intrusive body, carrying consistent nickel and cobalt mineralization, within which there are areas of higher grade. In the drilling the shoulders of the ultramafic, or the hanging and footwalls, demonstrate copper and zinc mineralization, including occasional zones of "mixing". The interpreted structure is currently considered consistent along the drilled strike, with variation in the width of the shoulder zones. Interestingly, the recently concluded stripping at Victoria West encountered much more copper and zinc on surface than was seen in the drilling, currently this is considered to be due to the variable presence of the ultramafic nickel/cobalt body and the magmatic copper/zinc body, consistent with "Outokumpu style" model that suggests two different mineralized bodies juxtaposed in one location due to the circumstances of the mineralizing event.