Silver Cord Project Reports High-Grade Veins Encountered

VANCOUVER – King Global Ventures Inc. reported on the recently completed 9,000-foot, eight-hole diamond drill program at the Silver Cord Project in Yavapai County, Arizona. The drill program consisted of holes SC-25-001, through to 007, designed to test induced polarization (IP) anomalies beneath the historic Silver Cord Mine and to transect the host Spud Mountain Formation, where geophysical and geochemical data indicated strong potential for volcanogenic massive sulfide (VMS)–related mineralization.
Drilling successfully intersected multiple polymetallic intervals and confirmed the presence of a polyphase Ag-Pb-Zn-Sb vein system hosted within the Spud Mountain stratigraphy. The program also provided important insight into the nature of the IP anomaly beneath Silver Cord.
Eight-hole, 9,000-ft drill program completed with multiple holes intersected high-grade silver–lead–zinc–antimony mineralization typical of a robust hydrothermal vein system.   
SC-25-004 intersected a high grade 9.0 ft interval of 619.6 grams (21.8 ounces) per tonne Silver, including 1.5 ft interval grading 1,390 (49 ounces) g/t Silver (48 oz/t), 2.2 g/t Gold with strong Lead, Zinc and Antimony support. SC-25-007 intersected a high-grade 1.0 ft interval of 625 g/t Ag, 1.0% Pb, and 1,175.0 g/t Antimony.  
The IP anomaly beneath the Silver Cord Mine is interpreted as intense siliceous alteration and anomalous copper consistent with intrusive-related hydrothermal activity. Results support a model for multiple mineralizing pulses and stacked structurally controlled mineralized zones. 
The results of the 2025 Silver Cord drill program indicate that the project hosts a polymetallic vein system within the Spud Mountain Formation, with geological features that may be consistent with VMS-related hydrothermal processes. Several drill holes, including SC-25-004 and SC-25-007, intersected intervals characterized by elevated silver, lead, zinc, and antimony, while SC-25-005 and SC-25-006 returned Zn-Pb-Cu–rich stringer-style mineralization. Collectively, these results support the conceptual interpretation that the Silver Cord structural corridor acted as a long-lived hydrothermal pathway capable of transporting and depositing metal-bearing fluids.
Robert Dzisiak, CEO, said, “The Silver Cord drill program has delivered very encouraging results at this early stage of exploration. Several holes have returned strong polymetallic intervals, and mineralization remains open in multiple directions. These results continue to build our confidence in the exploration potential of the Silver Cord corridor, and we look forward to advancing the next phase of drilling to better understand the geometry and continuity of the mineralized zones.”