Red Top Porphyry Cu-Mo Project Advanced Argillic alteration (pyrophyllite-dickite) Bronco Creek Exploration’s Red Top property is located in the Superior district near the world class Resolution deposit. TARGET: Middle to upper levels of large porphyry Cu-Mo system. Near surface supergene enriched Cu mineralization. Hypogene Cu(-Mo) porphyry style mineralization at depth. Sericitically-altered schist cross cut by oxidized quartz-sulfide veins. Oxidized vein surfaces contain anomalous Cu, Mo, Pb, Zn. Commonly vein densities are 1-5 vol% and locally >10 vol%. Maher, 2008

Red Top Porphyry Cu-Mo Project Multiple generations of outcropping ferricretes indicate a large, nearby sulfide source OPPORTUNITIES: Line of section ~967 hectares: 120 Federal Lode Claims with excellent access. Significant areas of outcropping paleo and modern ferricretes indicate abundant, local sulfides. Hydrothermal dickite and pyrophyllite identified, characteristic of shallow levels of a porphyry system. Cu, Mo anomaly in rock chip samples correspond to zones of intense sericitic alteration and vector towards system center. Quartz-sulfide-sericite vein stockwork hosted in upper level basement host rocks. System is intact, and moderately east-tilted, recorded by post-mineral sedimentary rocks. Red Top offers the opportunity to discover a large porphyry Cu-Mo deposit near the world class Resolution deposit. W E PARTICIPATE: Eurasian Minerals and Bronco Creek are seeking Joint Venture partners. Prospect Generation Business Model: EMX acquires early stage exploration properties, and seeks partnerships or joint ventures to advance these projects through the discovery stage. This strategy provides business partners with high-quality opportunities, and allows EMX to diversify its interests and participate in many exploration programs around the world. Dean Turner P.Geo., a Qualified Person as defined by National Instrument 43-101 and consultant to Eurasian Minerals, has reviewed and verified the technical information contained in this presentation.