Eagle Mountain Mining Limited announced assay results from its recently commenced drilling program at the Company's 80% owned Oracle Ridge Mine Project ("Oracle Ridge") in Arizona, USA. Assay results from selected zones within drill holes WT-20-05 and WT-20-02 have been received and are reported. WT-20-05 WT-20-05 was the first hole testing the potential of the southern area at Oracle Ridge. A significant zone of 15.1m @ 1.72% Cu, 16.87g/t Ag, 0.38g/t Au from 313.9m was intersected within a magnetite-rich skarn zone just above the Leatherwood-Sediments contact. Two higher grade intervals are contained within this broader zone including 8.41m @ 2.46% Cu, 25.09g/t Ag, 0.56g/t Au from 321.29m and above this higher grade zone, 3.45m @ 1.89% Cu, 15.97g/t Ag, 0.35g/t Au from 313.9m. This result confirms the prospectivity of the Leatherwood-Sediments contact to host significant skarn-hosted copper mineralisation as already demonstrated by historical holes drilled by previous owners such as C-115 and C-113. Drill hole WT-20-10 was designed to test the Leatherwood-Sediments contact approximately 40m to the north east of WT-20-05. This drill hole intersected skarn alteration with zones of copper mineralisation at the contact. Detailed logging is pending at the time of this report. Drill holes WT-20-11 and WT-20-12 were designed to test the south western extension of the intersection in WT-20-05. Detailed logging is pending at the time of this report. WT-20-02 WT-20-02 was drilled at the northern end of the mine area. This hole was designed to test the Geesman Fault ("Geesman"), a major structure which bounds the Oracle Ridge mine geology to the north. No previous drilling has intersected the fault and its role as a pathway for mineralizing fluids had never been assessed. The Geesman was successfully intersected by WT-20-02 and appears as a series of strongly sheared zones up to 15m thick occurring within Leatherwood intrusive between approximately 115 and 310m downhole (Figure 4). Within this larger zone, a 54m interval from 200m downhole showed highly anomalous base metal values (Zn >700ppm, Pb > 600ppm and Cu >300ppm). Sphalerite (Zn sulphide), chalcopyrite (Cu sulphide), and galena (Pb sulphide) are hosted in veinlets cross-cutting the intrusive. Weak to moderate sericitic alteration was also observed.