Eagle Mountain Mining Limited provided an exploration update at its 100% owned Oracle Ridge Mine Project in Arizona, USA. Assays have been received for three drill holes at The Talon Zone, namely WT-21-29 and the high-grade zones from drill hole WT-21-31 and WT-21-32. illustrates the location of these new results. An very thick mineralised zone was intersected in WT-21-31 from 253.5 metres to 345 metres for a total downhole length of 91.5 metres. This interval contains five high-grade zones varying in thickness between approximately 5 and 15 metres and displays strong magnetite and copper sulphides. These high-grade intercepts are separated by weakly to moderately altered and mineralised sediments. Results include: 91.5m at 1.37% Cu, 10.86g/t Ag and 0.38g/t Au, including 9.7m at 3.39% Cu, 29.65g/t Ag and 0.67g/t Au, and 11.7m at 1.90% Cu, 15.22g/t Ag and 0.52 g/t Au, and 14.8m at 1.62% Cu, 11.93g/t Ag and 0.53g/t Au, and 8.7m at 2.00% Cu, 15.20g/t Ag and 0.4g/t Au, and 8.0m at 1.90% Cu, 13.92g/t Ag and 0.85g/t Au The 91.5 metre zone is significantly thicker than any mineralisation encountered in nearby holes. The only area of the mine where similar thicknesses and grade are found is to the north where recent reported results include 110.1m at 1.06% Cu, 9.64g/t Ag and 0.16g/t Au (WT-21-24) and 96.1m at 0.98% Cu, 7.84g/t Ag and 0.15g/t Au (WT-21-18; see ASX announcement 15 September 2021). The results from WT-21-31 are highly encouraging and indicate that substantial thicknesses of mineralisation could occur also in The Talon area. Further assays for the upper part and the lower part of WT-21-31 (above and below the high-grade zone) remain outstanding. WT-21-32 was drilled in the Western Talon area and encountered a 28.9 metre zone of moderate to strong copper mineralization. Assays have now been received for this interval, confirming its very high-grade nature. The best results include: 28.9m at 2.34% Cu, 21.95g/t Ag, 0.37g/t Au from 270.6m, across two zones: Upper zone: 13.2m at 3.53% Cu, 33.89g/t Ag, 0.54g/t Au from 270.6m, including 5.4m at 4.85% Cu, 54.80g/t Ag, 0.96g/t Au from 271.4m, including 1.4m at 9.99% Cu, 147g/t Ag, 2.83g/t Au from 271.4m Lower zone: 7.2m at 2.04% Cu, 15.71g/t Ag, 0.29 g/t Au from 292.3m These results are some of the best ever at Oracle Ridge. The upper zone is characterised by abundant disseminated to semi-massive bornite and chalcopyrite (copper minerals) while the lower zone contains the same minerals hosted in bands. The two intersections are separated by a lower grade zone of 8.5m at 0.76% Cu, 8.68g/t Ag and 0.16g/t Au. Further details about the geological interpretation of this zone are provided in the latter part of the announcement. Assays for the some of the upper and lower parts of WT-21-32 are still awaited. WT-21-29 was drilled approximately 35 metres to the east of WT-21-32. The hole intersected multiple narrow zones of greater than 1% copper mineralisation with the best intervals being: 3.0m at 1.12% Cu, 9.43g/t Ag and 0.45 g Au from 244.5m 10.5m at 1.20% Cu, 13.16g/t Ag and 0.23g/t Au from 292.5m This second intersection occurs at the Leatherwood-Sediment contact and is interpreted to be the continuation of the high-grade mineralisation in the lower part of WT-21-32. The lower grade and less extensive mineralised zones in WT-21-29 may be explained by the local geology. Stratigraphy in the area dips steeply to the east, as confirmed by structural observations in the core. This geometry causes the most favourable sediments for hosting skarn alteration and mineralisation to be intersected only at the very bottom of WT-21-29, just before the Leatherwood intrusive truncates them.