Alianza Minerals Ltd. reports the final two holes from the 2021 drilling campaign at the Company's wholly-owned Haldane high-grade silver property located in the historic Keno Hill Mining District of Yukon Territory. Drilling has focused on the West Fault Complex target where a strong vein- fault system with high-grade silver mineralization is being defined. Following up on the success in earlier holes, HLD21-26 and HLD21-27 have infilled and further extended the West Fault mineralization by 50 metres along strike to the northeast. The 8,579 hectare Haldane Property is located in the western portion of the Keno Hill Silver District, 25 kilometres west of Keno City, YT. Exploration at Haldane is targeting extensions of historical high-grade silver production on the property as well as recently defined targets, such as the West Fault, in new areas of the property. The 8,579 hectare Haldane Property is located in the western portion of the Keno Hill Silver District, 25 kilometres west of Keno City, YT. Exploration at Haldane is targeting extensions of historical high-grade silver production on the property as well as recently defined targets, such as the West Fault, in new areas of the property. HLD21-26 intersected the West Fault structure at 268.43 m over a core length of 15.42 m (estimated true width of 9.25 m), exhibiting good strength and width. Strong siderite/sulphide breccia and veining was intersected at 270.41 m returning a 5.09 m (3.05 m estimated true width) intersection of 205 g/t silver (369 g/t silver-equivalent). The highest grade interval of 0.55 m (0.33 m estimated true width) of 437 g/t silver, 9.99% lead and 16.9% zinc (1,383 g/t silver-equivalent) consisted of very strong siderite- galena-sphalerite with trace tetrahedrite in veins and breccia. Siderite/sulphide veining is bounded on both sides by zones of clay-gouge with elevated silver content. HLD21-27 intersected the West Fault structure at 222.40 m over a core length of 16.75m (estimated true width of 10.05 m). Strong siderite vein and vein breccia with banding open-space fill textures was intersected at 225.00 m, returning an 8.00 m (4.80 m estimated true width) intersection of weakly mineralized material grading 81.4 g/t silver (113 g/t silver-equivalent). This intersection expanded vein mineralization at the West Fault 50 m to the northeast along strike from HLD20-19 that intersected 8.30 m (4.48 m estimated true width) of 444 g/t silver (554 g/t silver-equivalent). Although the vein and vein breccia was wide and consisted of textures associated with productive mineralization, it was moderately to strongly oxidized with remnant sulphides occurring predominantly as disseminated blebs indicating a lower overall original galena and sphalerite content.