Copperhead Resources. Inc. reported that it has discovered three highly prospective intrusions on the Red Line project ("Red Line" or the "Project"), including 2 areas of K-feldspar porphyritic syenite similar to one of the key units found at the giant Galore Creek porphyry Cu-Au deposit. A previously undocumented K-feldspar por Murphyritic syenite pluton believed to be more than 300 m wide was discovered <1.5 km south of the Red Line claims and immediately staked and added to the Project. This large body of highly gossanous syenite closely resembles one of the key intrusions associated with the Galore Creek alkalic porphyry Cu-AU-Ag deposits. Numerous K-feldspar syenite boulders were located on the Red Line 2 claim, derived from the upper part of a steep ridge of metasediments and lesser volcanics, many of which are pervasively altered to epidote. The association of strong epidote alteration with the syenite dikes may be indicative of a porphyry copper type system at depth here. A second, previously unknown intrusion was located on the Red Line 2 and 3 claims, in this case a >700 m long body of pervasively altered hornblende granodiorite. The discovery of these 2 highly prospective intrusions, and numerous syenite dikes associated with widespread epidote alteration, has significantly improved the odds of locating a porphyry Cu- Au-Ag type occurrence on the Red Line claims. Porphyritic Syenite Pluton: During Copperhead's 2023 exploration program, a very gossanous, potassium feldspar-porphyritic syenite intrusion (field name), thought to be at least 300 m wide, was noted on open ground south of the Red Line claims. The syenite intrusion has numerous large patches of pyritic gossans throughout, potentially indicative of the pyrite shell around a porphyry Cu-A Au system. It is notable for the pervasive green alteration and the disseminated pyrite found throughout most of the unit. Lithogeochemical analyses and thin section studies are planned to determine if the alteration is part of a porphyry-type system and if this pluton is part of the Galore Creek suite. Syenite Dike Swarm and Associated Epidote Alteration: A 1 km long ridge on the Red Line 4 claim is notable for the prominent and relatively pervasive epidote alteration, potentially part of the propylitic alteration zone around the periphery of a porphyry centre. Numerous coarse-grained K-feldspar porphyritic boulders occur along the lower slopes of this steep ridge, presumably derived from a dike
swarm at higher elevations. Minor secondary copper mineralization was noted on fracture surfaces in some of the local sedimentary talus. The valley floors on either side of the ridge are occupied by small glaciers but the association of the epidote alteration, syenite dike swarm, and local copper mineralization warrants a detailed examination of the lower elevations for further indications of a porphyry system at depth beneath this ridge. A sample of the syenite has also been sent for age-dating at the University of British Columbia.