Bayhorse Silver: Unveiling the Potential of the Extended Breccia Zone

Bayhorse Silver Inc. (TSXV: BHS) (OTCQB: BHSIF) (FSE: 7KXN) has recently extended the Bayhorse Breccia Zone from 90m (300ft) downhole to 318m (1050ft), revealing promising assay results and preliminary IP results. This significant development has the potential to enhance the mine's economic viability and open up new exploration opportunities.

The extended breccia zone, characterized as a highly silicified hydrothermal polymictic breccia, contains multiple rounded, "milled" clasts, likely resulting from high-pressure fluids derived from a buried pluton. The presence of elevated levels of copper, zinc, and lead in this zone, as indicated by XRF field analysis, suggests that the mineralization could be more extensive and valuable than previously thought.

The anomalous copper-zinc assay results from the first 115m of the breccia zone have significant implications for the mine's future economic viability and potential for further exploration. The presence of elevated copper and zinc levels suggests that the mineralization could be more extensive and valuable than previously thought, potentially increasing the mine's reserves and lifespan. Additionally, the results validate the Company's exploration model, which suggests that the silver-copper-antimony rich mineralization at the Bayhorse Silver Mine could have its source in underlying shallow granites that may host porphyry copper mineralization.

The preliminary IP results have contributed to the understanding of the geology and mineralization within the Bayhorse Breccia Zone by identifying zones of high chargeability, which are indicative of the presence of sulfide minerals. These zones are associated with areas of strong silicification, epithermal-style vuggy quartz veining, and hydrothermal brecciation, suggesting proximity to porphyry or related epithermal mineralization.



Further geophysical surveys, such as downhole IP surveys, can provide additional insights into the geology and mineralization within the Bayhorse Breccia Zone. These surveys can help to discriminate between rocks that conduct electrical current and those that do not, allowing for a better understanding of the rock types present and their distribution within the zone. Additionally, they can measure the chargeability of rocks, which can help to identify areas with common but disconnected zones of sulfides, as well as massive sulfides and copper porphyry, which are ideal chargeability targets.

In conclusion, the extended Bayhorse Breccia Zone, along with the associated anomalous copper-zinc assay results and preliminary IP results, has the potential to significantly enhance the mine's economic viability and open up new exploration opportunities. As the Company continues to explore and develop the mine, investors should keep a close eye on these developments, as they could have a substantial impact on the Company's future prospects.