Canter Resources Corp. reported that the Company has acquired additional third-party data including historical soil sampling results and geophysical survey data that highlights significant lithium in soils along the eastern edge of the 5 by 2.5 km priority target area at the Columbus Lithium-Boron Project. The acquisition of substantial third-party historical geochemical sampling data, alongside Canter's own database and sampling efforts, provides a comprehensive dataset within the 23,000-acre project area.

This combined dataset includes 473 surface samples and reveals a maximum surface sediment lithium value of 540 ppm Li. Analysis of the newly acquired third-party data shows an average concentration of 144 ppm Li across 54 surface sediment samples and multiple locations exceeding 200 ppm Li, with the highest value from the historical dataset reported at 348ppm Li. Additionally, previous surface brine samples reveal lithium concentrations reaching 240 mg/L. This extensive combined dataset highlights the basin's potential for near-surface lithium enrichment.

The Company recently engaged renowned geophysicist, Jim Wright of Wright Geophysics, who completed reinterpretation of available geophysical data. The Company has also obtained airborne magnetic and radiometric data from the recently completed collaboration between the U.S. Geological Survey (USGS) and the Department of Energy (DOE) designed in part to support geologic and geophysical mapping and modeling of Nevada's lithium clay and brine resources. During a recent trip to site, the Company's geologists completed a single, one metre (three feet) deep auger hole approximately 500 metres east of the first planned exploration well at Columbus.

The small portable auger rig was not suitable for reaching the interpreted upper brine layer depth; however, the Company still collected a sediment sample at the bottom of the test hole that returned a value of 430 ppm Li. The Company will test the upper brine layer during its upcoming Geoprobe campaign. Reprocessing of historical gravity data, incorporating data from both regional and property-specific surveys, has identified a prominent gravity anomaly within the basin.

This anomaly is indicative of a substantial layer of low-density sediment that may extend to depths exceeding 3,300 meters. Canter Resources has also integrated airborne magnetic and radiometric data from the USGS - DOE collaboration. This data, underpinned by a comprehensive reinterpretation by Wright Geophysics, has highlighted the intricate structural dynamics at play within the Columbus Basin.