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Bayhorse Silver Extends Bayhorse Breccia Zone From 90 M (300ft) Downhole to 318 M (1050 ft) Reports Anomalous Copper-Zinc Assay Results From The First 115 M Of The Breccia Zone, And Preliminary IP Results

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Vancouver, British Columbia--(Newsfile Corp. - March 4, 2025) - Bayhorse Silver Inc, (TSXV: BHS) (OTCQB: BHSIF) (FSE: 7KXN) (the "Company" or "Bayhorse") reports that assay results have been received for the first 115 m (380 ft) of the silicified breccia zone encountered 90 m (300 ft) downhole in drill hole BH24-01 to test a VTEM anomaly at the Bayhorse Silver Mine.

Anomalous values of continuous copper, (up to 125 ppm) and zinc (up to 695 ppm) and intermittent anomalous gold values (up to 0.023 ppm) were encountered in the first 115 m (380 ft) of the brecciation zone that now extends to the current bottom of the hole at 318 m (1050 ft). A further 112 m of samples of brecciation and rhyolite have been submitted for assay. The presence of chalcopyrite was noted at the bottom of the hole.

Bayhorse CEO Graeme O'Neill comments, "we are very encouraged by the continuous copper/zinc mineralization in the upper 115 m (380 ft) part of the 227 m (750 ft) length breccia intersection that lies in close proximity to the IP chargeability and low-resistance zones that may indicate the presence of massive sulfides/copper porphyry."

As well, the preliminary IP results by S.J. V Geophysics, that are overlaid on the geologic map, (figure 1) has identified both chargeability (green) and low resistance targets (blue) extending to depth within the VTEM geophysics signature within the rhyolite hosted copper and silver rich Bayhorse Silver Mine deposit. The IP geophysical survey will be extended onto the Pegasus project as soon as ground conditions permit.

Drilling BH24-01 has confirmed that the Bayhorse Ag-Cu-Zn-Sb mineralization is epithermal in nature and is expected to extend to significant depths. In Hole BH24-01 there are areas of strong silica flooding, epithermal-style vuggy quartz veining, sporadic tetrahedrite mineralization and hydrothermal brecciation. This extends from 90m (300 ft) to the current bottom of the hole at 318 m (1050 ft). This alteration could mark the hole's proximity to a porphyry or related epithermal system.

Figure 1. Plan view of rhyolite occurrences hosting silver/copper mineralization and geophysical anomalies. Geological mapping by Dr. Clay Conway, P.Geol.

To view an enhanced version of this graphic, please visit:
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In figure 1, the top of silver bearing rhyolite dyke 1 has been cut and offset by thrusting, and the overlying segment (dyke 2) has been displaced to the south. This displaced section, with an estimated vertical extent of 120 m (396 ft) is the area of the Company's planned mining based on the National Instrument 43-101 inferred resource of 6.3 m ounces of silver at a grade of 21.65 opt ((673 g/t) (Turner et al. 2018).