Renforth Resources Inc. announced that summer 2022 prospecting at Surimeau has successfully concluded with, amongst other findings, the extension of the known Lalonde surface battery metals mineralization to a strike length of 9 kms. on Renforth's wholly owned 330 sq km. property located south of Cadillac, Quebec and contiguous to the Canadian Malartic Mine. In the summer 2022 program Renforth continued to work to define the extent of surface/sub-surface polymetallic mineralization on the Surimeau District Property as evidenced by outcrop, drill results and geophysics.

To date this has resulted in the definition of the Victoria mineralized structure at approximately 20km in length and the Lalonde mineralized structure now measuring approximately 9km in length. A significant amount of ground remains untested, in part because Renforth has, to date, only used existing lumber roads and trails for access within the property. During this program Renforth's field crew, along with prospecting various targets, dug 8 different trenches between the Lalonde and Victoria polymetallic mineralized systems. In each trench some amount of mineralization was exposed, with the best mineralization (confirmed visually and with XRF) coming from Lalonde.

Interestingly, each trench exposed different portions of each mineralized system, helping to define the orientation of the mineralization, and in some cases making clear that the trench should be extended to capture the entire cross section of the mineralization. Renforth has discovered that at Victoria there is a second horizon of mineralization sitting to the north of the mineralized horizon uncovered during the Fall 2021 stripping at Victoria, the northern crosscut ended approximately 40m short of where it would have intersected the northern mineralization. Each trench is described below and shown on the location map.

Channels were cut in each trench and samples sent for assay; results will be released once available. Due to the success of this program Renforth is now planning additional stripping to cross-cut strike at Victoria in addition to a series of larger cross-cutting stripped trenches along strike at Lalonde in order to further define the extent of mineralization. At Victoria the cross-cutting trenches, which will start at the south and north side of the currently stripped area, will extend well into the sediments, hopefully capturing any additional mineralized horizons.

Lalonde Trenches: Trenches 1 through 5 were dug at Lalonde, approximately 3.7km north of the Victoria stripped area. Trench 5 represents an extension to the west of approximately 2km for the Lalonde mineralization. Trench 1: The first trench exposes about 5 meters of Pontiac sediments at the north end with occasional narrow beds of graphitic mudstone, mineralized with traces of chalcopyrite and pyrite stringers.

Ultramafics are found immediately south of the sediments with a narrow band of ab-shearing between the two units (approximately 50-60cm). The ultramafics have bands of calc-silicate alteration as well as bands of moderate to strong albitization with around 15-20% sulfide overall. South of the ultramafics is strongly amphibolized mafic volcanics (picrites).

Trench 2: As expected, the second trench exposes the same general lithological sequence as the first. The south end of the trench exposes very well mineralized calc-silicate altered ultramafics, followed by serpentinized ultramafics and another band of albitized and calc-silicate altered ultramafics. The first approximately 2m of the channel (at the south end) are extremely well mineralized with 5-25% sulfide disseminations and clots of pyrite, pyrrhotite and traces of sphalerite, pentlandite, chalcopyrite and bornite.

There is a narrow band of Pontiac sediments in the rough center of the trench, followed by another band of well mineralized calc-silicate and albitized ultramafics that is about 3m wide. The last 2 meters of the trench exposes Pontiac sediments. Trench 3: From south to north this trench exposes ultramafics with varying degrees albitization and up to 5-7% sulfide mineralization (pyrite-pyrrhotite), locally up to 15% sulfide, with traces of chalcopyrite, followed by Pontiac sediments to the end of the trench/channel, including occasional narrow beds of graphitic sediments.

Trench 4: This trench is 12 meters in length and trench exposes serpentinized ultramafics at the south end, with occasional bands of very strong biotitization to about 7m, followed by 2 meters of calc-silicate altered ultramafics with 10-15% sulfide. Sediments follow the ultramafics for about 3 meters to the end of the trench. Trench 5: This trench is about 22 meters in length and exposes serpentinized ultramafics at the very southern end, followed by 3 meters of graphitic mudstones and sediments with occasional narrow bands of albitized ultramafics, containing traces of chalcopyrite and up to 2% disseminated pyrite-pyrrhotite in the ultramafics.

A 3 meter wide albitized shear zone follows with 5-7% sulfide mineralization overall, with locally up to 30% sulfides, primarily sphalerite, pyrite and pyrrhotite. The next 6 meters (approx.) is albitized ultramafics with up to 2% disseminated pyrite-pyrrhotite, followed by serpentinized ultramafics at the north end of the trench. Surimeau Victoria North Trenches: Trenches 6-8 were dug at Victoria to expose the newly discovered northern band of mineralization at Victoria.

In the Fall 2021 Victoria stripping program, a length of 275m was stripped, exposing surface polymetallic mineralization, between fences of holes drilled in Spring 2021. Subsequently, the exposed mineralization was undercut with drilling in December 2021. Prior to this program the exploration at Victoria had been targeting the magnetic high, all the drilling and the stripped north crosscuts missed intersecting the northern mineralized band which was discovered during prospecting in Spring 2022 by Renforth's field crew.

Renforth is currently planning additional stripping at Victoria which will consist of a wide trench starting on the north and south sides of the stripped area, and driven to the north and the south, long enough to be well into what is assumed to be only host rock in an effort to not miss mineralization in future drilling. Little is known about what occurs between Victoria and Lalonde.