Gold and silver mineralization at the Shahuindo Gold Project consists of several zones of hydrothermal alteration in which 5 resource-bearing zones have been derived. These include from East-South-East (ESE) to West-North-West (WNW) Moyan Alto, East, South Contact, Porphyry and San José Zone. These zones comprise the Main Mineralized Corridor (MMC).

Two other mineralization corridors, generally parallel to the MMC, are also found on the property. The South Mineralized Corridor is located 1.5 kilometers South-South-West (SSW) of the MMC and encompasses areas of high-grade veins located on top of the Algamarca Anticline. The North Mineralized Corridor is located 2.5 km North-North-East (NNE) on the MMC, and hosts the Mina Shahuindo (Minas Azules) old gold mine operated intermittently by Minera Algamarca in the 1980’s.

For more information on the geology of the Shahuindo deposit, click HERE to view the "Geological Forum" presentation from November 17th, 2009.