Renforth Resources Visually Observes Mineralization in Channel Cutting of Diorites and Felsites in Open Pit Footprint at Parbec Gold Deposit

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TORONTO, Ontario – TheNewswire - June 29, 2026 — Renforth Resources Inc. (CSE: RFR | OTC: RFHRF | FSE: 9RR) ("Renforth" or the "Company") is pleased to announce the completion of an initial channel cutting campaign with drone-assisted geological mapping in the open pit footprint for the Company’s wholly owned Parbec gold deposit on the Cadillac Break in Malartic, Quebec, contiguous to Canadian Malartic. HIGHLIGHTS 8 channels were cut with mineralization visually observed  Felsite and diorite, gold-bearing lithologies at Parbec, were uncovered during overburden removal and observed to occur to a greater extent than previously understood. Samples have been taken and submitted for assay.  Zoomed in Detail of Stripped Area in Parbec’s Open Pit Footprint with Channels in Orange STRIPPING AND CHANNEL SAMPLING PROGRAM DISCUSSION The area chipped at Parbec is approximately 350m by 125m.  Stripping within that envelope is roughly 250m by 100m. The sediments and diorites were exposed along the entire stripped length.  While our intention was to uncover the Cadillac Break along the length as well, we were unsuccessful due to excessive overburden thickness starting at the sedimentary contact with the break along the northern side of the trench. Washing the bedrock was stopped in order to permit initial sampling. The stripped area exposed is very interesting. Sediments intruded with diorite lenses are exposed along the length of the stripping and what we call ‘felsite’ horizons stretching for tens of metres subparallel to the break within the sediments.  These felsites are strongly silicified, intensely fractured up particularly in proximity to the break, hosting 2-6% fine disseminated pyrite with occasional small cubic pyrite crystals as well. Contacts with the sediments are clear and sharp. Drag folding with offsets of approximately one to three metres are noted with some boudinaging quartz veining. It is interesting that the felsites show continuity of tens of metres along their length, which was not clearly apparent in our drilling. In drilling they are often gold-bearing and only 1m or so in width, however on outcrop in some area’s true width approaches 15m at times. There are multiple felsite subparallel lenses within the stripped area.    We have also exposed diorites, which are mineralized in pri...

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