Investor Presentaiton

EL EDEN Mineralization Style @ Buenavista The style of the mineralized system at El Eden is very similar to Guadalupe Los Reyes The Au and Ag mineralization found at EDEN, like at Guadalupe de Los Reyes, occurs in a series of quartz rich vein-breccia-stockwork structures which consist of high- grade narrow veins contained in a broader, 10m to 25m wide, lower grade envelope containing intensely. oxidized breccias and quartz stockworks. Host rocks at EDEN, like at Guadalupe de Los Reyes, are coffee-colored andesite tuffs, ash-tuffs and agglomerates. Both EDEN and Guadalupe de Los Reyes are spatially related to a nearby intrusive body. 875mRL The mineralized structures extend for kilometers along strike and follow regional fault systems. Most of the vein-stockwork systems dip moderately to the E and NE. At EDEN, like at Guadalupe de Los Reyes, an earlier, pre- mineralization, volcanic event (rhyolite-dacite dikes, sills and rhyolite domes), served as the main conduits (plumbing system) for the migrating mineralized fluids. Dacite dikes are occasionally seen along the footwall of the vein structures. 850mRL 626mRL 800mRL 775mRL 750mRL ---Open Pit Resourory Bottom of Inferred 22GE-33 GL020 725mRL 700mRL 675mRL 650mRL New 22GE-33 11.60 g/t Au, 219.0 g/t Ag over 1.5 m (1.2 m etw) Mineralized Interval 625RL Geology Drill Hole Trace Into Section Out of Section Inferred Stopes (old mine workings) GL020 GL072 GL073 86.07 m GL010 meters Section GE-4935 E GL041 12GL-02 GL041 GL010 26.29 m 12GL-02 GL073 GL072 Estaca Vein A' New 22GE-33 3.67 g/t Au, 120.5 g/t Ag over 35.60m (29.2 m etw) including 6.57 g/t Au, 137.2 g/t Ag over 9.0 m (7.4 m etw) & including 8.39 g/t Au, 321.0 g/t Ag over 2.6 m (2.1 m etw) Andesite Feldspar Porphyry Rhyolite Intr Quartz Vein/ Breccia Zones Inferred 14 PRIME MINING CORP. 22GE-33 Los Reyes Project Section GE-4935 E Section Looking WNW (290°) Section Envelop 30m Projector WOD4 213 1000 CENTENARIO GOLD CORP WWW.CENTENARIOGOLD.COM 12

View entire presentation