Gold79 Mines Ltd. announced that it has completed additional mapping and sampling at the Sheep Trail Mine Area within its Gold Chain project, located in northwest Arizona. 6.0m of 3.96 g/t gold (composite of samples 752-754) 7.0m of 5.06 g/t gold (composite of samples 755-757)-3.7m of 19.52 g/t gold (composite of samples 758-759) This sampling program focused on the Sheep Trail patented claim block (113.15 acres) and followed up initial sampling focused on the numerous small pits and mine dumps which revealed multiple high-grade sample results. The results reported below reflect chip-channel samples collected from widely mineralized outcrops spatially proximal to the initial results and likely reflect source material.

All recent sample results from the Sheep Trail area. Sheep Trail geology mapped by Gold79's geologic staff along with rock samples collected to date. Gold mineralization is mostly hosted in the Miocene rhyolite dike complex near contacts with the hosting Precambrian granite.

The primary structural corridor here is the Sheep Trail ledge (fault zone) where historical mining has occurred. At this pronounced bend, referred to as the Golden Elbow, quartz-chalcedony-calcite veins and veinlets attain greater widths (50-75 metres) and suggest a southwest-plunging shoot. The rhyolite intrusive within this jog displays strong quartz- pyrite-illite alteration consistent with gold mineralization at depth.

Alteration of the rhyolite dike complex remains strong throughout this area.