Mr. Gurminder Sangha reports

FE BATTERY METALS INTERSECTS UP TO 1.43% LITHIUM OXIDE IN THE BASEMENT ROCKS AT THE AUGUSTUS LITHIUM PROPERTY

FE Battery Metals Corp. has released significant findings from its continuing exploration efforts at the Augustus lithium property in Quebec. The company's latest studies have revealed remarkable lithium oxide (Li2O) concentrations in the basement rocks situated in proximity to the pegmatite wallrocks, with values ranging from 0.3 per cent to an exceptional 1.43 per cent Li2O (see an attached table).

The Augustus lithium property is located just 33 kilometres north of Val d'Or, Que., and sits directly adjacent to Canada's largest lithium mine, the North American lithium mine (NAL). The company's exploration efforts at ALP have revealed widespread lithium-bearing pegmatites on surface, and drill efforts show they remain open at depth and along a strike length of 5.5 km.

To date, the company has completed 14,448.59 metres of diamond drilling across 79 NQ-size holes, and analytical investigative efforts have been focused on the pegmatite bodies, but with this significant find the company intends to further explore the potential of economic lithium oxide concentrations that have also been revealed in the host rocks of the pegmatite bodies.

Key highlights (see an attached table for details):

• The basement rocks returning the highest lithium concentrations are identified as biotite schist and amphibolites, with the majority of these samples in close proximity to their contact points with pegmatite bodies.
• A correlation is observed with higher lithium, cesium and rubidium concentrations and elevated nickel and chromium values, suggesting lithium concentrations in the wallrock are likely due to the influence of hydrothermal fluids.
• As part of the company's continued advancement to a maiden resource at Augustus, FE Battery Metals is currently engaged in three-dimensional modelling of drill intercepts and surficial work. The basement rock data may play a pivotal role in enhancing this model, potentially aiding in resource size.
• A field geological mapping and sampling program will also be implemented to understand the contact zone of pegmatites with the basement rocks.

In a significant exploration undertaking, FE Battery Metals has sampled a larger section of drill core from hole LC23-63, spanning from 115.49 to 308 metres, which was then sent to Activation Laboratories in Ancaster, Ont. Building upon the preliminary findings of this investigation, FE Battery Metals' team of geologists will embark on a comprehensive relogging and sampling campaign encompassing drill core samples collected throughout the 2021-to-2023 exploration phase.

Gurminder Sangha, chief executive officer of FE Battery Metals, commented: "Augustus has exceeded our expectations at every phase of exploration. We are particularly enthused by the elevated lithium, cesium and rubidium values noted within the host basement rocks, which has the potential to reshape our exploration strategy. The new sampling effort, if successful, could greatly expand the lithium mineralization footprint at Augustus and advance our 3-D resource model of the project."

The drill core is logged, sampled and stored at FE Battery Metals' facility located in the village of St-Dominique du Rosaire, about 50 km from ALP. For quality assurance/quality control, field duplicates, standards and blanks are being inserted at industry-standard intervals. Best practices are maintained in the collection and delivery of the samples to Activation Laboratories, Ancaster, Ont., for sample preparation and analyses using laboratory code Ultratrace 7 and sodium peroxide fusion (Na2O2) for lithium. Activation Laboratories is an independent, commercial, accredited, ISO-certified laboratory.

Afzaal Pirzada, PGeo, geological consultant of the company, a qualified person for the purposes of National Instrument 43-101 -- Standards of Disclosure for Mineral Projects, has reviewed and approved the scientific and technical information contained in this news release.

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