Golden Ridge Resources Ltd. announced the final assay results from the 2023 Phase II drilling campaign at the Williams Gold Property within the Appleton and Dog Bay Fault Corridors. Golden Ridge has continued to generate encouraging results at the Property with recent assays recording mineralization up to 24.65 meters grading 2.22 g/t Au. The Williams Project is surrounded by New Found Gold Corp. (NFGC)'s Queensway Gold Property where NFGC is currently undertaking a 650,000 meter drill program. Phase II drilling at the Williams Project was focused on the five mineralized zones as identified by earlier prospecting, soil sampling and drilling programs. These mineralized zones (Figure 3) are known as the: Cabin Zone (CZ), Cabin Zone Extension (CZX), EQ Zone (EQZ), Gray Jay Zone (GJZ) and the Blue Jay Zone (BJZ) all of which are open along strike and down-dip. Although these zones were first identified during the 2020 - 2021 surficial sampling and trenching programs, several other prospects remain to be targeted. Upon completion of in-fill drilling at the Grey Jay Zone the 2024 drilling campaign switched gears and began to target outlying prospects. The final phase of the 2023 drilling program returned to the Cabin Zone. Its purpose was to follow-up on exciting results obtained in 2022, with the objective of increasing the strike length of the prospect and connecting the Cabin Zone to the Cabin Zone Extension. Excitingly, Phase II drilling was not only successful in confirming the presence of Au-mineralization at the Blue Jay and EQ Zones it also increased the strike length of the Cabin Zone and established along strike continuity between it and Cabin Zone Extension. Mineralization at these locations is characterized by a broad sericite-chlorite alteration halo that is associated with a complex system of quartz-carbonate veins like those identified by earlier trenching and drilling. This is exemplified by WIL-23-51, at the Blue Jay Zone, which intersected a 12.30-meter section grading 0.67 g/t Au including a 5.45-meter section which yielded 1.00 g/t Au. Additionally, WIL-23-54 (located 450 meters NE of WIL-23-51) intersected a 24.65-meter section grading 2.22 g/t Au including a 11.7-meter section which yielded 4.46 g/t Au. WIL-23-54 also intersected 0.65-meter zone grading 77.40 g/t representing a potential high-grade target at this prospect. Mineralization was also identified in outlying targets located at the southwestern extension of the Gray Jay Zone and EQ Zones. Drilling at these prospects once more revealed broad zones of Au-mineralization such as those observed in WIL-23-63 which contained 3.10-meters yielding 1.29 g/t Au. In-fill drilling at the Cabin Zone was centered around WIL-22-09 and WIL-22-08 which intersected 46.50 meters at 0.39 g/t Au and 10.00 meters grading 0.50 g/t respectively. Drilling at this location continued defining broad zones of mineralization as documented by WIL-23-68 (a 300-meter step-out from WIL-22-08) which contained a 21.70- meter section grading 0.44 g/t Au including an 8.55-meter section at 0.74 g/t Au. Additionally, WIL-23-70 (a 12.5-meter step-out from WIL-22-09) intersected a 58.40-meter section grading 0.46 g/t Au including a 5.50-meter section which yielded 1.10 g/t Au. Importantly, drilling at the Cabin Zone indicates along strike continuity of Au-mineralization between the Cabin Zone and Cabin Zone Extension. Ultimately, the 2023 drilling campaign increasing the total strike length of the Cabin Zone Prospect by 200-meters. Interestingly, mineralization throughout the project area is often associated with fault/rubble zones most commonly occurring along the eastern margin of the system. This is especially apparent at the EQ Zone, Cabin Zone and Cabin Zone Extension where these faults/rubble zones contain clay and graphite. These zones also display variable amounts of vein fragments and anomalous Au concentrations indicating syn-mineralization to post-mineralization movement along these structures. A structural analysis of these zones is currently underway to determine the exact relationship between them and the mineralized system. It is important to note that all prospects at Williams Property are currently still open along strike and down dip, and further drilling will be required to delineate the overall size and grade of the Au mineralization system. In total, 41 holes were completed during Phase II drilling campaign consisting of 5,982 meters. Upon completion of this program Golden Ridge Resources Ltd. has now drilled 70 holes at the Williams Property for a grand total of 10,182 meters. With an average depth between 100-200 meters each drill hole was focused on testing near surface gold-mineralization associated with soil, bedrock and drilling anomalies identified during earlier exploration programs. Highlights from these programs include soil, grab and core samples yielding 1.5 g/t, 281 g/t and 77.4 g/t respectively. Building on earlier successes, the Phase II diamond drilling campaign continued to increase the potential of the Williams Project. Infill drilling at the Grey Jay, Cabin and Cabin Zone Extension outlined a core region of Au-mineralization with intercepts up to 86.00 meters yielding 1.00 g/t Au and 70.75-meters with 1.05 g/t. Individual core samples from this region also returned assay results up to 13.30 g/t at the Cabin Zone Extension and 6.58 g/t at the Gray Jay Zone and increased the overall Au-grade at these prospects. Drilling at prospects outside the mineralized core also confirmed the presence of Au-in-bedrock mineralization throughout the project area. This is exemplified by WIL-23-54 which intersected 24.65-meters of 2.22g/t. Interestingly, this drill hole also contains the highest Au-grade sample obtained in drill core to date at 0.65-meters at 77.40g/t further confirming the presence of high-grade gold samples throughout the Williams Property.
Phase II drilling indicates that mineralization at the Williams Zone is more widespread than previously identified. This program continued to characterize the style of gold-mineralization as a complex system of up to 1.5 meters veins, veinlets, and vein breccias, up to 1.5-meters in size. This Au-bearing system is associated with weak to locally intense sericitic and chloritic alteration with the highest gold assays correlating to areas of increased alteration. Additionally, sulphide mineralization appears to be more pervasive in core obtained from Phase II drill holes. The host rock often contains disseminated pyrite crystals, blebs, and stringers throughout and acicular crystals and blebs of arsenopyrite occur near mineralized zones. Gold-bearing veins contain primarily pyrite and are often associated with arsenopyrite, pyrrhotite, chalcopyrite, and galena with trace amounts of stibnite, molybdenite and sphalerite.