Forza Lithium Corp. announce the company has completed its latest fieldwork program on its Jeannette Lithium Property ("the Property") for the 2023 season. The Property is located approximately 105 km east of the town of Red Lake, Ontario, and 80 km northeast of Ear Falls, Ontario.

The 9-day field program was carried out by a crew of three in early August by mobilizing a boat to provide access to the northern portion of the property as well as along logging roads which traverse the Property. During the 2022 field program 113 grab and channel samples were collected returning values up to 244 ppm Li, which was obtained from a sample of biotite gneiss with coarse feldspar-quartz dykelets. 45 grab samples were collected during the June and July field programs, which returned values up to 290ppm Li and 688ppm Rb.

The value of 290 ppm Li was obtained from biotite gneiss proximal to the sample which had earlier returned 244 ppm Li. The value of 688 ppm Rb was obtained from pegmatite on the south shore of Tarpley Lake in the northeastern part of the Property. An additional 44 grab samples were collected during the August 2023 program.

These returned up to 309 ppm Li and up to 497 ppm Rb. The value of 309 ppm Li was obtained from biotite gneiss proximal to samples which had earlier returned 244 and 290 ppm Li. The value of 497 ppm Rb was obtained from pegmatite approximately 2 km south of Tarpley Lake in the eastern part of the Property.

Frederick W. Breaks, Ph.D., P.Geo., was asked after the July 2023 program to review sample results to date and provide a summary of his findings. Mr. Breaks carried out a review of 157 samples collected on the Jeanette Property from 2022 - July 2023. August sampling returned the Rb value of 497 ppm approximately 2 km south of Tarpley Lake along the above-mentioned topographical/magnetic lineament, adding support to the `lineament control' hypothesis.

Elevated rubidium concentrations in rare element pegmatite systems are indicative of a higher degree of chemical evolution of the system and therefore prospectivity for lithium mineralization. The following description of the regional geology is adapted from the NI 43-101 Independent Technical Report on the Jeannette Lithium Property (Camier 2022): The Property is located in the east-central portion of the Allison Lake Batholith within the Uchi Subprovince of the Superior Province of the Canadian Shield. The Uchi Subprovince is an east- trending granite-greenstone domain between 50 and 70 kilometers in width, extending approximately 700 kilometers from Lake Winnipeg in the west to the James Bay Lowlands.

The Allison Lake Batholith is the known fertile, peraluminous granite in northwestern Ontario (Breaks et al. 2003). Rare-element (Li, Cs, Rb, Tl, Be, Ta, Nb, Ga and Ge) pegmatite mineralization associated with S-type, peraluminous granite plutons is distributed over a wide expanse of the Superior Province of northeastern and northwestern Ontario.

Rare element pegmatite mineralization occurs along a 350 km strike length of the Uchi-English River Subprovince boundary, from the Sandy Creek beryl pegmatite near Ear Falls to the Lilypad Lake complex-type pegmatite in the Fort Hope area, with 3 areas of known mineralization in between at Jubilee Lake, Root Lake and East Pashkokogan Lake (Breaks et al. 2003). John Londry, P. Geo, an independent qualified person as defined in National Instrument 43-101, has reviewed, and approved the technical contents of this news release on behalf of the Company.

The Company nor the Q.P. have not completed sufficient work to verify the historical information on the property comprising the Jeanette Project, particularly regarding historical exploration, neighbouring companies, and government geological work. Grab samples are selected samples and not necessarily representative of the mineralization hosted on the property.