Eagle Mountain Mining Limited announced assay results from its ongoing drilling program at the company's 80% owned Oracle Ridge Mine Project ("Oracle Ridge") in Arizona, USA. Assay results from holes WT-20-12, WT-20-13, WT-20-14 and WT-20-15 have been received. WT-20-12 was designed to test the western extensions to the high-grade mineralization in hole WT- 20-11. The drill hole intersected three zones of high-grade mineralization up to 6m in thickness. Zones are hosted by sediments, above the Leatherwood-Sediments contact, consistent with the high-grade mineralization observed in adjacent holes. Further drilling is currently being planned in the area to expand the mineralized horizon and understand the correlation between skarn mineralization and breccia-hosted mineralization intersected in holes WT-20-10 (13.3m @ 2.43% Cu, 52.6 g/t Ag and 0.94 g/t Au, including 1.5 m @ 11.55% Cu, 273 g/t Ag and 5.41 g/t Au) and WT-20-06 (3.0m @ 6.76% Cu, 63.51 g/t Ag and 0.87 g/t Au). WT-20-13 was drilled to the east of an unconstrained high-grade historical intersection in hole C-058 (10.1m @ 3.47% Cu and 35.23 g/t Ag). The drill hole intersected moderate mineralisation with two zones returning copper values exceeding the reporting cut-off. The lower of these zones occurs at the Leatherwood-Sediments contact and is interpreted as the extension of skarn mineralisation in hole C- 058, C-130 and 2011-130. Further drilling is planned in the vicinity of these drill holes to further understand the continuity of mineralisation defined. WT-20-14 was drilled to the northwest of hole WT-20-04 (4.6m @ 5.28% Cu, 50.70 g/t Ag and 0.77 g/t Au) testing extension to mineralisation within the Escabrosa Limestone as well as at the Leatherwood- Sediments contact. Over 7m @ 1.45% Cu were intersected at the contact with this intersection remaining open to the east. Lower grade mineralisation was intersected within the Escabrosa Limestone suggesting that the mineralising system is still present in the area. WT-20-15 was drilled to the south west of drill hole WT-20-04 testing for extension to mineralization within the Escabrosa Limestone and at the Leatherwood-Sediments contact. The intersection of 6.1m @ 4.24% Cu, 36.16gt/t Ag and 0.36 g/t Au is consistent with the thickness and tenor of mineralization encountered in WT-20-04 and nearby holes (e.g. OUH-063 - 7.7m @ 5.11% Cu, 55.83 g/t Ag and 0.72 g/t Au). WT-20-16 was drilled to the east of WT-20-03, targeting northern extensions to mineralisation at the Leatherwood-Sediments contact intersected in historical holes. Visual observations identified several zones of copper sulphide mineralisation between 206 and 300.5m downhole. The cumulative length of these zones is approximately 13m. Samples were recently submitted to the laboratory and assay results are expected in the coming weeks. Breccia zones similar to those previously intersected in holes WT-20-10 and WT-20-06 have been logged in WT-20-16. The geology team is currently reviewing all available information to better assess the extent of these breccia occurrences. Further drilling will be planned following this review to assess the significance of the breccias as sources of additional mineralised material and as possible vectors to skarn and porphyry mineralisation.