Green River Gold Corp. provided the following assay results and updated drilling results for Zone 2 of the Quesnel Nickel Project. The Company has received assay results for hole WK-22-06 drilled to a depth of 128 meters in Zone 2 of the Deep Purple target. The drill hole is the deepest hole drilled on the project to date and it ended in mineralization. The hole was drilled using a portable Winkie drill and the drill reached its capacity at 128 meters. The assay results received are presented in Table 1 below. Another 6 drill holes are planned for this Winter. Zone 2 is located approximately 8 kilometers southeast of Zone 1, which was drilled by Green River in the Winter of 2021 and Spring of 2022. Both zones are extensive bedrock exposures that are located within the Deep Purple magnetic anomaly consisting of nickel, chromium, cobalt, magnesium, and talc mineralization. The entire Deep Purple magnetic anomaly has a linear length of 14 kilometers with an approximate area of 6.63 square kilometers. The entire project is located within a one hour drive of Green River's shop and office in the City of Quesnel, B.C. XRF results for the most recent drill hole WK-22-07are presented below in Table 3. The drill core was delivered to the Company's facility in Quesnel and was scanned with an XRF analyzer. Drill hole WK-22- 07 was scanned to a depth of 93.3 meters. Hole WK-22-03 was drilled vertically from the same drill collar as hole WK-22-02. The drill core from
WK-22-03 has been sent to Base Metallurgical Laboratory in Kamloops for a scoping level metallurgical analysis involving hardness and grindability along with assessing the metallurgical performance of samples using conventional flotation processes. This data will be used to help guide the selection of metallurgical testing to develop a viable recovery process. Nickel on the Property is hosted in ultramafic rocks, mainly black phaneritic peridotite, belonging to the Slide Mountain Terrane (Crooked Amphibolite). The peridotite exhibits intense serpentine alteration and strong brecciation. Sulfides in the core are made up of disseminated pyrite, pyrrhotite, and pentlandite. The Slide Mountain Terrane overlies metasediments (limestone and sandstone) belonging to the Ramos Succession of the Barkerville Terrane. The Ramos Succession was intersected at 75.0 meters in hole WK-22-03. Hole WK-22-06 was drilled on the east side of the drilling pattern, with a -60 degree dip for 129.2 meters. Hole WK-22-06 did not intersect the Ramos Succession.