Alianza Minerals Ltd. reports additional results 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 initial success in hole HLD20-19, HLD21-25 has further extended the West Fault mineralization by 62 metres down dip with an intersection averaging 1,107 g/t silver, 6.98% lead and 3.97% zinc (1,485 g/t silver-equivalent(2)) over 1.60 metres (estimated true width of 1.00 metres). This occurs within a wider zone of siderite veining and brecciation, fault gouge with lesser galena and sphalerite which averaged 363.4 g/t silver, 1.73% lead and 2.80% zinc (534.2 g/t silver-equivalent) over 6.83 metres (estimated true width 4.27 metres). 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. HLD21-25 intersected the West Fault structure at 291.5 m over a core length of 13.38 m (estimated true width of 8.36 m), averaging 220.5 g/t Ag (325.0 g/t silver-equivalent). Strong siderite/sulphide breccia and veining was intersected at 293.44 m returning a 6.83 m (4.27 m estimated true width) intersection of 363.4 g/t silver (534.2 g/t silver-equivalent). The grade interval of 1.6 m (1.00 m estimated true width) of 1,107 g/t silver, 3.97% lead and 3.97% zinc (1,485 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. The West Fault intersection in HLD21-25 occurs approximately 25 metres uphole from where the target was modelled to occur and it is now believed that the West Fault is a complex of faults and splays rather than a single discreet fault structure. Narrow structures hosting siderite-galena-sphalerite veins have been intersected above the West Fault mineralization in previous holes (HLD20-19, HLD21-24) and are now thought to represent the upper splay of the West Fault, now referred to as WF2. The WF1 structure, host to the high grade silver mineralization previously released in hole HLD20-19 and HLD21- 24, looks to weaken to down dip to the northwest, perhaps stepping over to the WF2 splay in this direction.