MacDonald Mines Exploration Ltd. announced results from two diamond drill holes completed last fall at its SJP property, 40 kilometres east of Sudbury, Ontario. Both drill holes intersected a wide breccia zone in the Bristol Structure, outside and west of the historic Scadding Deposit, that hosts cobalt and gold mineralization. The cobalt and gold grades, and the intensity of brecciation are comparable to and appear to increase southward towards the Long Trench Breccia 4 kilometres to the south. These drill results show gold-cobalt mineralization that is comparable to the mineralization sampled in 2018 at the Long Trench. This suggests that the Bristol breccia and Long Trench breccia are related and may be hosted in the same structural corridor. The Bristol breccia is open in all directions and to depth. These results greatly increase the potential size of the Scadding Deposit footprint with the high-grade zones of gold reported to date potentially being contained within a larger envelope of lower grade gold, cobalt and other secondary mineralization. The mineralized Bristol breccia, intersected in holes SM-19-009 and SM-19-010, is composed of sodic-altered clasts hosted in a quartz matrix with accessory carbonates. The breccia matrix contains variable amounts of disseminated pyrite and there is a good spatial association between zones with increased content of pyrite and gold-cobalt mineralization in the breccia. In SM-19-009, the Bristol breccia is incipiently to moderately developed and the ratio of fragments/matrix remains high throughout the breccia zone. In SM-19-010, the Bristol breccia is moderately to strongly developed and the ratio of fragments/matrix is moderate to low in many zones of the breccia. There is also an increased abundance of sulfides in the Bristol breccia in SM-19-010 compared to SM-19-009 and this correlates with higher gold and cobalt grades. The Bristol breccia is geologically similar to the Long Trench breccia located 4 km south of the Scadding Deposit. The Long Trench breccia is formed of albitized clasts hosted in a quartz-carbonate matrix with variable disseminated pyrite. MacDonald’s 2018 channel sampling in the Long Trench breccia revealed gold-cobalt mineralization comparable to gold-cobalt mineralization in the Bristol breccia. Considering a likely north-south orientation for the Bristol breccia and the location of Long Trench breccia due south of the Bristol breccia, the Bristol and the Long Trench breccias are possibly hosted in the same structural corridor.