The Phinney Lake project is strategically located adjacent to the Dash Lake area. The land position covers granodiorite and monzonite in contact with mafic to intermediate metavolcanics and lesser clastic metasediments proximal to a regional fault and smaller splays.
Zn-Cu, Zn-Au-Cu and Au occurrences have been identified within and around the property(1,2,3). Phinney Lake mineralization is associated with massive sulphides (sphalerite, pyrrhotite, pyrite, chalcopyrite) in felsic metavolcanic rocks. From the early 70’s throughout the 90’s, mapping, sampling, trenching, drilling, and geophysical surveys (Mag and EM) were completed(2). *Historical drilling database is incomplete, yet 1999-2000 results of Bernard Barton returned anomalous Zn, Au and Cu.
EMX has not performed sufficient work to verify the published assay data reported above, and these data cannot be verified as being compliant with NI43-101 standards. These historically reported data should not be relied upon until they can be confirmed, but EMX believes this information is considered reliable and relevant. NOTE: True widths unknown