お知らせ • Jan 14
Silver North Resources Ltd. Receives Results from the Remaining Two Haldane Silver Property in the Historic Keno Hill Silver District, Yukon
Silver North Resources Ltd. announced that the Company has received results from the remaining two holes from the 2025 exploration program at its flagship Haldane Silver Property in the historic Keno Hill Silver District, Yukon. Results include 2.80 metres averaging 1,069 g/t silver, 1.41 g/t gold, 12.60% lead and 3.01% zinc within a larger 9.10 metre intersection of 428 g/t silver, 0.73 g/t gold, 5.26% lead and 1.73% zinc from 182.40 metres down hole. A total of eight holes (totalling 1,759.5 metres) were completed in the 2025 program, seven of which successfully tested the Main Fault, intersecting silver-bearing siderite-sulphide vein and vein breccia mineralization. One hole (HLD25-37) was abandoned within what is interpreted to be the Main Fault but no core was recovered. The road-accessible 8,579 hectare Haldane Property is located 25 km west of Keno City, YT, adjacent to Hecla Mining's producing Keno Hill Silver Mine property, and hosts numerous occurrences of silver-lead-zinc-bearing quartz siderite veins resembling the ore-bearing veins being mined at Keno Hill. HLD25-36 and 38 were drilled off section to test for structures oblique to the Main Fault ("linkage" or "transverse" faults), and to investigate the continuity of vein and structure internal to the Main Fault complex. The collar location table and plan map shown below indicate the collar and hole orientation with respect to the rest of the Main Fault. As with other intersections at the Main Fault and elsewhere on the Haldane property, mineralization in both holes consists of siderite +/- quartz, galena and sphalerite veins and breccias, as well as strongly faulted and ground up vein and vein breccia material. HLD25-36 intersected two splays of the Main Fault over 31 metres, starting at 161.0 m, separated by 18.25 metres of weaker structurally influenced quartzite, phyllitic quartzite, and phyllite with anomalous silver between the upper and lower splay. The entire 161.00 to 192.00 metres returned 174 g/t silver, 0.26 g/t gold, 1.68% lead and 0.64% zinc. The upper splay, from 161.00 to 164.15 returned 3.15 m averaging 228 g/t silver, 0.10 g/t gold, 0.48% lead and 0.45% zinc, while the more strongly mineralized lower splay averaged 428 g/t silver, 0.73 g/t gold, 5.26% lead and 1.73% zinc over 9.10 metres starting at 182.4 m down hole. A high-grade section of this interval, from 188.00 to 190.80 m averaged 1,069 g/t silver, 1.41 g/t gold, 12.60% lead and 3.02% zinc over 2.80 metres. HLD25-38 intersected multiple mineralized intervals starting at 177.00 metres depth. A 1.50 metre section of brecciated vein material returned 406 g/t silver, 0.10 g/t gold, 3.13% lead and 0.18% zinc overlying 17.80 metres of quartzite, minor vein breccia and phyllitic quartzite anomalous in silver, lead and zinc from 178.50 to 196.30 metres. The lower section of Main Fault mineralization was intersected from 196.30 to 218.30 metres, a 22 metre zone which includes a 1.90 metre strongly mineralized section averaging 437 g/t silver, 0.35 g/t gold, 14.55% lead and 4.04% zinc.