Mined the east-west trending 350 meter long Pacocahua vein on the south slope of Cerro Pacocahua (elevation 4,282 meters). Country rock is Eocene sandstone intruded by rhyolite, both altered by silicification and sericitization. Hydrothermal activity continues to the present time.
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Map Reference: 17°19'6"S , 69°14'32"W
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