Eagle Mountain Mining Limited announced further assay results from its recently commenced drilling program at the Company's 80% owned Oracle Ridge Mine Project in Arizona, USA. Assay results from selected zones within drill holes WT-20-06, WT-20-07, WT-20-09, WT-20-11 have been received and are reported in this announcement. Initial observations from hole WT-20-10 are also provided. Quartz-breccia grading 6.76% Cu, 63.51g/t Ag and 0.87g/t Au over 2.95m at 210m downhole. Below this breccia structural zone are three moderate to high grade intervals intersected over approximately a 35m horizon: 0.9m at 2.61% Cu, 20.8 g/t Ag and 0.59 g/t Au at 218.3m; 9.25m at 1.19% Cu, 9.51 g/t Ag, and 0.21 g./t Au from 225.37m; and 3.57m at 2.18% Cu, 19.49 g/t Ag and 0.89 g/t Au from 245.43m. The average grade of this whole 39m zone averages 1.17% Cu, 10.26g/t Ag and 0.23 g/t Au. The large thickness of the mineralisation exceeding 1% Cu is quite encouraging for the potential of either increased lower grade tonnes or alternatively higher-grade portions. WT-20-07: Three zones of disseminated copper over 1% Cu were intersected. WT-20-08: Abandoned at 196m due to stuck drill rods. WT-20-09: Two mineralised skarn zones were intersected: 2.85m @ 1.38% Cu, 10.85g/t Ag and 0.17 g/t Au from 175.29m and 4.77m @ 1.21% Cu, 13.05g/t Ag and 0.20 g/t Au from 260m. WT-20-10 (Assays Pending): WT-20-10 tested the eastern extension of the mineralised zone of 15.1m @ 1.72% Cu, 16.87g/t Ag, 0.38g/t Au encountered in hole WT-20-05 at the Leatherwood-sediments contact. From 317m downhole for approximately 50m, visual disseminated copper mineralisation was observed including high-grade veins and breccias up to 1.5m thick. Veins and breccias cross-cut the Leatherwood intrusive suggesting that some of the copper at Oracle Ridge was introduced after emplacement of the Leatherwood thus enhancing the prospectivity for a deeper copper-bearing system. WT-20-11: WT-20-11 was drilled to the west of WT-20-05 testing the western extension of mineralisation at the Leatherwood-sediments contact. A thick zone of high-grade mineralisation was intersected assaying 2.80% Cu, 18.75g/t Au and 0.61g/t Au over 8.4m. A relatively narrow but very high-grade zone was also intersected approximately 10m above the contact mineralisation (1.35m @ 9.14% Cu, 52.5 g/t Ag and 0.69 g/t Au). Observations in holes WT-20-05, WT-20-10 and WT-20-11 suggest a new interpretation for the geology of the area. The Leatherwood granite-limestone contact is now believed to be steeper possibly due to a structure just to the west of hole WT-20-11. Interpretation is ongoing to understand the extent of this feature (e.g. possible links to the breccia zone in hole WT-20-06) and its significance for mineralisation at Oracle Ridge. While several targets remain untested in the WT-20-10 area shown in Figure 5, it was decided to wait until all assay results are received and detailed interpretation completed on holes WT-20-05 to WT-20-12. The data and interpretation will aid targeting and enhance the effectiveness of future drill holes in the area.