Eminent Gold Corp. announced that Phase 1 geochemical and mapping results of its Hot Spring Range Project (HSRP) located 15 km northwest of the Getchell Trend (42.5Moz Au endowment), demonstrates proof of concept that a Getchell Trend analogous Carlin-type gold system exists on the Property. The structural framework and host rock lithologies at HSRP have never before been explored. Now that the Company has identified targets associated with geochemical anomalies the next step is to confirm targets through ground geophysical surveys followed by drill testing. HSRP is located in Humboldt County Nevada, approximately 50 kilometers (km) northeast of the town of Winnemucca, NV and 20 km northwest of Nevada Gold Mine'sTurquoise Ridge mine complex, which together with Twin Creeks forms the Getchell Trend (42.5M oz in gold endowment1). The HSRP is comprised of over 3,200 hectares of highly prospective ground that has seen no exploration activity prior to being acquired by Eminent Gold in 2020. Phase 1 Field Work: The Company took 1,312 soil samples at 125-meter centers and 157 rock samples at the Otis target, and 79 pediment soil samples at the Eden target to test the conceptual model of a Carlin-type hydrothermal gold system analogous to the Getchell Trend occurring in the Hot Springs Range. Additionally, geologic mapping by the Company's experienced technical team confirmed the presence of multiple key characteristics of a Carlin-type system a) a prospective Carlin-type host rock (i.e., limestone & andesite package similar to the Comus formation), b) a remarkably similar structural architecture between HSRP and the Getchell Trend of steeply dipping feeder faults and shallowly dipping thrust faults, c) alteration characteristics (i.e., decalcification of carbonate rocks and sulfidation of iron-bearing igneous rocks), and d) anomalous gold and pathfinder geochemistry occurring in predicted places spatially associated with feeder faults that intersect favourable host rocks and thrust faults. The cumulative Phase 1 evidence validates a proof of concept that a Carlin-type hydrothermal gold system may exist in the Hot Springs Range that has never before been recognized or explored.