Mr. Deepak Varshney reports

USHA RESOURCES COMPLETES PHASE THREE PROGRAM, EXTENDING STRIKE TO 27 KILOMETRES AT THE WHITE WILLOW LITHIUM PEGMATITE PROJECT

Usha Resources Ltd. has provided this update on its continuing field program at the White Willow lithium pegmatite project located 170 kilometres west of Thunder Bay, Ont.

The company has completed 10 weeks of fieldwork as part of phase 3. The focus of the program was to advance the Bingo lithium-cesium-tantalum (LCT) pegmatite swarm to a drill-ready stage and further assess the Maple Leaf LCT pegmatite swarm. A total of 727 grab samples were collected from pegmatites and their host rocks and submitted for laboratory analysis as part of detailed mapping and prospecting to identify geochemical anomalies associated with lithium mineralization not visible at surface.

The existing 25 km strike length of fractionated pegmatites has been extended approximately two km farther to the west, where preliminary results at Bingo have returned some of the most evolved chemical signatures on the property. Potassium/rubidium: approximately 20; niobium/tantalum: less than one; 4,100 parts per million Rb; and 954 ppm Cs.

"We are thrilled with the findings from the most recent phase of fieldwork at White Willow and are very excited to continue to build on our success," said Deepak Varshney, chief executive officer of Usha Resources. "As seen at Patriot Battery Metals' Corvette project, which has over 20 kilometres of trend, lithium pegmatite swarms occur in clusters, each of which has the potential to become a deposit. With 10 existing primary target areas already identified across our 27-kilometre-plus trend, we believe phase 3 will contribute significantly in the identification of additional targets for our planned maiden program of 4,000 metres. The findings thus far strongly validate our belief that Willow is a flagship asset where Ontario's next major lithium discovery will occur."

Mr. Varshney continued: "I am grateful to Jason Wolf, Andrew Tims and James Macdonald and their respective teams for pushing themselves to the limit and working late into the season far past beyond when most teams had quit. Their persistence has been a huge part of why Usha has been successful in the field and we are thankful to have some of the brightest minds in this business working on this project. We look forward to returning to the field as soon as the snow melts and building on the successes of 2023."

Detailed sampling and hand stripping have successfully identified beryl and Nb-Ta oxides over an approximately two km strike length. Fractionation indicators suggest the dikes have reached spodumene-type degrees of fractionation. Preliminary results show lithium (Li), cesium (Cs) and rubidium (Rb) elevations in the metasedimentary host rocks around the beryl-type pegmatites with up to 450 ppm Li were returned in the metasedimentary rocks adjacent to the largest of the beryl-type dikes.

Lithogeochemical sampling of pegmatite host rocks is one of the most common techniques to test for buried spodumene mineralization. Pegmatites leave a recognizable chemical halo in the surrounding country rocks, and this halo is reflective of the chemistry of the pegmatite. By sampling the country rocks in a systematic grid, Usha plans to identify the areas of the Bingo pegmatite swarm that have the highest chance of hosting spodumene. The preliminary results have returned up to 450 ppm Li along the margins of beryl- and tantalum-bearing pegmatites, suggesting that the evolved pegmatites are part of a lithium-enriched system.

The Bingo pegmatites display many textural similarities with spodumene-bearing pegmatites in Ontario, most notably a strong planar fabric and albitization of coarse K-feldspars. Beryl is present as light green to white euhedral crystals (up to seven centimetres long) along approximately two km of the exposed strike length.

The white colour of beryl indicates a high Cs content and suggests crystallization in a highly evolved pegmatite. Nb-Ta oxides (up to one cm long) are also present throughout the mapped strike length of the dike and their presence was confirmed using electron dispersive spectrometry (EDS). Apatite is common as bright blue equant crystals up to five millimetres in width. The white beryl and the Nb-Ta oxides are locally associated with the partial to complete replacement of coarse K-feldspars by albite.

To date, the company has delineated 10 high-priority drill targets with K/Rb ratios below 30. K/Rb is a key tool in identifying potentially spodumene-bearing dikes. Values below 30 are indicative of rare-earth pegmatites and 20 of spodumene-subtype pegmatites.

Pegmatite dikes from phase 3 that contain positive indicator minerals (beryl or Nb-Ta oxides), prospective fractionation indicators, or are situated in areas of anomalous Li, Cs or Rb haloes will be followed up with more detailed prospecting, outcrop exposing, and will ultimately be a part of the company's maiden 4,000-metre drill program anticipated to commence in spring 2024 that will test these new and previously identified targets for the first time.

Quality assurance/quality control

All collected rock samples were put in sturdy plastic bags, tagged and sealed at site. Sample bags were then put in rice bags and kept securely before being sent by road transport or delivered by the crew supervisor to either Agat Laboratories Ltd. or Activation Laboratories in Thunder Bay, Ont. All samples are analyzed with four-acid digestion/combined inductively coupled plasma atomic emission spectroscopy/mass spectrometry package (49 elements). The QA/QC protocol included the insertion and monitoring of appropriate reference materials, in this case high-concentration and low-concentration certified OREAS and CDN lithium standards to validate the accuracy and precision of the assay results.

Qualified person

The technical content of this news release has been reviewed and approved by Mr. Tims, PGeo, a qualified person as defined by National Instrument 43-101.

About Usha Resources Ltd.

Usha Resources is a North American mineral acquisition and exploration company focused on the development of quality lithium metal properties that are drill ready with high upside and expansion potential. Based in Vancouver, B.C., Usha's portfolio of strategic properties provides target-rich diversification and includes Jackpot Lake, a lithium brine project in Nevada, and White Willow, a lithium pegmatite project in Ontario that is the flagship among its growing portfolio of hard-rock lithium assets. Usha trades on the TSX Venture Exchange under the symbol USHA, the OTCQB Exchange under the symbol USHAF and the Frankfurt Stock Exchange under the symbol JO0.

We seek Safe Harbor.