El Cobre Project is located about 70 Km southwest of Guadalajara City, the capital of the State of Jalisco and 10.5 Km southwest of San Martín Hidalgo town.

The project is Surrounded by Timmins Gold Corp Cocula claim and Soltoro Quila project. Also located nearby Southern Silver and Magistral mine and La Sorpresa project.

Access to this area is done as a starting point the city of Guadalajara to Ameca by Federal Highway N° 70 with a distance of 60 Km; continue by road to San Martín Hidalgo for a distance of 11 Km and continues dirt road that connects with San Jeronimo village to 7 Km. To continue on dirt road to the property for a distance of 4 Km. The Elevations at the property range from 1, 400 to 1,800 and the terrain is slightly steep and rugged.

DEPOSIT TYPES: Oxidized breccias zones containing gold, silver, lead, copper and zinc values. Possible related to system of the IOGC Type (Iron Oxide Copper Deposit).

PRODUCTION DATA: Historically the property has been mined on a small scale in attempt to develop the high-grade mineralization in fractures. > 5 g/t Au, 20 g/t Ag.

During early 2008 the Company completed first phase sampling of several trenches at its Cocula Project located next to El Cobre project. The 102 channel samples taken across the oxidized and brecciated zone returned an average grade of 2.21 g/t Au, 19 g/t Ag, 0.97 % Pb, 0.11 % Zn and 0.08 % Cu across 99 metres. A high grade core within the breccia returne d 6.90 g/t Au, 17.7 g/t Ag, 0.06% Cu, 1.07 % Pb, 0.12% Zn across 18 metres.

This NW-SE trending alteration zone has been traced a long s trike for o ver 1.5 kilometres. The zone has an average width of 200 metres and is exposed over a vertical extent of between 40 and 50 metres. The zone remains open along s trike and is projected to extend at least 150 metres down dip. While the Company had been confident a low grade, bulk tonnage target would be identified, the high grade results encountered on surface have made evaluation of the economic potential of the Cocula Property a higher priority for the Company. The epithermal mineralization lies within an argillized and brecciated shear zone between two semi parallel faults within a volcano-sedimentary sequence. The zone is strongly o xidized and silicified with common jarosite and stockworks of galena and sphalerite. Silicification is present in the form of vuggy silica, chalcedony banding and quartz veinlets. The bottom of the oxidized cap within the volcano sedimentary sequence can be I dentified by pervasive silicification and intense quarts veinlets, including disseminated pyrite, lead and zinc sulfides near Its base.

A comprehensive sampling, trenching, mapping program and 32 hole, 2,700 meter reverse circulation drill program were also completed during the current period. A total of 302 channel samples were taken from seven trenches excavated along 400 meters of strike. T he trenches, 2 meters deep, 25 to 250 meters long and 25 and 100 meters apart, were all cut perpendicular. To the principal trend of the mineralization. Results from t he trenching program Include 2.398 g/t Au across 136 meters, including a high grade core grading 5.506 g/t Au across 50 meters, 2.080 g/t Au across 19 meters and 2.087 g/t Au a cross 18 meters.

The mineralization is hosted in two highly oxidized and brecciated zones known as the Cerro Colorado and La Chabela stockwork zones. It is important to note that while the mineralized system has been traced for over three kilometers, this detailed mapping and sampling of the trenches concentrated on only 400 meters of strike length.

The program identified the zones of alteration and the distribution of the precious and base metal along the entire 400 meters sampled.

Source :http://www.timminsgold.com/s/Cocula.asp