Silver Storm Mining Ltd. announce further drill results from its Phase 1 diamond drilling program at the Company's 100% owned La Parrilla Silver Mine Complex, located in Durango Mexico. Results from the seven holes within this release are from the Quebradillas mine. The San Nicolas Zone is considered part of the Quebradillas Mine, located approximately 400 m to the SW and connected by underground development utilizing shared services from the mine.

The San Nicolas Zone had 5 levels of development established and mined by First Majestic, and a ventilation raise from surface down to 275 m. As a result of the drilling and surface mapping conducted by the Company, high-grade silver mineralization can now be traced with continuity down to approximately 370 m from surface. Management anticipates follow-up drilling and mapping will continue to extend mineralization at the San Nicolas Zone, and the additional four proximal subparallel veins identified to date. The San Nicolas Zone is comprised of subvertical quartz-carbonate vein and breccia mineralization striking NW (315/87) over a known length of approximately 600 m. Massive sulphide replacement zones occur within the hanging wall and footwall along the bedding within the sediments.

The sulphide mineralization consists of pyrite, galena, sphalerite, acanthite, and native silver and is oxidized from the surface down to approximately 100 m. A second set of east-west trending sulphide bearing quartz- carbonate veins crosscuts the principal NW trend. Breccia pipes (chimneys) form at the intersection of these two trends. Holes Q-23-013A to 015A targeted the southeastern down-dip extension of the zone beneath the 1886 m EL stope.

Hole Q-23-024 successfully intersected sulphide breccia mineralization, returning 689 g/t Ag.Eq over 9.39 m (71.75 to 81.14 m), including 1,000 g/t Ag.Eq over 5.25 m (72.75 to 78.00 m). This intercept is located approximately 18 m above the last mine development in this area, with similar mineralization. This high-grade breccia zone lies at the intersection of the NW trending San Nicolas and the east-west trending Quebradillas structures and can be traced 235 m up-dip from this hole toward the surface.

Historical hole ILP-SN-19-08, which returned 530 g/t Ag.Eq. over 7.50 m (186.10 to 193.60 m), located approximately 40 m above hole Q-23-024, confirms this trend of the breccia to surface within a 25 m deep artisanal shaft. Hole Q-23-013A successfully intersected sulphide replacement type mineralization returning 316 g/t Ag.Eq over 4.09 m (87.49 to 91.58 m) including 663 g/t Ag.Eq.

over 1.00 m (88.55 to 89.55 m) and 297 g/t Ag.Eq over 1.58 m (90.00 to 91.58 m). This intercept is located approximately 30 m below the last mine development in this area, with similar mineralization. The composited weighted average grade of historical channel samples from the 1886 SE1 m EL stope returned 289 g/t Ag.Eq over a strike length of 8 m and average width of 1.62 m. The composited weighted average grade of historical channel samples from the 1887 W m EL stope returned 243 g/t Ag.Eq over a strike length of 10 m and average width of 2.61 m. Hole Q-23-014 intersected sulphide fault zone associated breccia and quartz-carbonate vein type mineralization returning 240 g/t Ag.Eq.

over 1.90 m (111.80 to 113.70 m). Hole Q-23-025 intersected sulphide fault zone associated breccia and quartz-carbonate vein type mineralization returning 211 g/t Ag.Eq. over 1.09 m (85.65 to 86.74 m).

The Veta Nueva Zone is located approximately 200 m to the NE and subparallel to the San Nicolas Zone, characterized by a NW trending fault-zone quartz-carbonate vein which dips 50 degrees to the NE (130/50). First Majestic had mined one Level of Veta Nueva prior to placing the mine on care and maintenance. Hole Q-23-016 successfully intersected sulphide fault zone associated quartz-carbonate vein type mineralization returning 525 g/t Ag.Eq over 0.4 m (53.83 to 54.23 m).