Pure Resources Limited announced preliminary results from the maiden geological fieldwork campaign that covered less than 5% of the 261km2 project area at the Company's Laforge Lithium Project (the Project), located in Quebec, Canada. The 2022 winter rock sampling program was designed to evaluate the potential for LCT (Lithium-Cesium-Tantalum)-bearing pegmatites on the Project in northern Quebec. Rock grab samples were collected to test for a suite of major and trace elements via ICP-MS at ALS laboratories.

Prospecting on the Project was helicopter-supported (to and from Mirage Adventure Lodge) and took place between December 1st ­ December 13th, 2022. Prospective locations for rock sampling were chosen based on topographic relief and previously mapped outcrops of migmatitic rock near contacts with metasedimentary units. In general, exposure on the Property was limited due to snowfall and terrain conditions.

Preference was given to sampling directly from outcropping units from wind- swept outcrops, but float samples which displayed characteristics similar to known lithologies on the Property were also collected. All samples were submitted to ALS laboratories in Val-d'Or Quebec for ME-MS61 analysis. Geological Summary and Recommendations: The 2022 winter rock sampling and prospecting program was successful at defining three zones of granitic-pegmatitic lithologies which possess the following key characteristics: Coarse mineral grain size with visible pegmatitic textures (graphic mineral intergrowths, exsolution laminae in feldspars); Encouraging presence of other phases indicative of a fertile melt (biotite, muscovite, possible tourmaline); and Elevated concentrations of pathfinder elements associated with the presence of LCT Pegmatites.

The rock zones contained outcrops of granitic-pegmatitic lithologies with elevated lithium as well key LCT pegmatite pathfinder elements such as tantalum and niobium . Pegmatitic samples from these zones will undergo mineralogical testwork to identify potential Li-bearing minerals or phases associated with Li-rich intrusions (e.g. spodumene and lepidolite). Biotite and muscovite were commonly observed and three samples contained small crystals of a fluorescent red mineral (possibly spodumene).

Multiple samples from Zone 2 contained anomalous concentrations of Li, Ta, Nb, and Cs and this area represents the most prospective zone for future exploration. Zones 1 and 3 also showed anomalous pathfinder element concentrations and outcrops of granitic- pegmatitic rocks forming topographic highs. These areas represent additional candidates for future exploration.

Other lithologies observed on the Property included variably metamorphosed gneisses, metasediments, and mafic-intermediate intrusions. Geochemical results from these units returned no relevant element anomalies. Given the geochemical anomalies present in granitic-pegmatitic units on the Property, a follow-up prospecting program could further constrain areas of high prospectivity.

Such a program will be undertaken in the summer-fall months to avoid complications from snow cover. The following steps will be undertaken to constrain the location of potential LCT pegmatites on the Project: An expanded surface geochemical sampling program (soil, rock, and potentially stream sediments) focusing on areas adjacent to the prospective zones identified in this report. Soil sampling may be especially valuable in areas of the Project with poor rock exposure.

An airborne radiometric survey of the Project to identify granitic-pegmatitic units. Ground magnetic surveys to establish a structural framework of prospective zones. Conduct mineralogy to determine the content of the Spodumene in lithium samples.

Rock Sampling: The 2022 winter rock sampling program resulted in a total of 240 rock samples collected across the Project. Of the 240 samples, 41 were described as pegmatite or pegmatitic. Of the three prospective areas, Zone 2 displayed the highest concentration of samples with anomalous geochemistry, including maximum concentrations of 12 ppm (~6x crustal concentration) and 98.1 ppm (~5x crustal concentration) for Ta and Nb respectively.

These samples were collected from a large pegmatite outcrop which formed a topographic high. Rocks from this area displayed common pegmatite textures including graphic mineral intergrowths and mica megacrysts.