Angel Gold Corp. (TSX-V: ANG) is a Canadian precious metals exploration company focused on the acquisition and responsible development of mineral resources in Colombia. Colombia is the most under-explored country in the Andean region and hosts the northern extension of the mineral-rich Andes Cordillera.
Colombia is a stable democracy with a history of fiscal responsibility and respecting private property, including some of the best investor protections in the world. The historical metal production in the country has been dominated by gold. Angel has considerable in-country experience and members of its management team directly contributed to Ventana Gold Corp.´s success.
Angel's property portfolio includes the El Porvenir project in the Segovia-Remedios gold belt, historically the largest gold producing region in Colombia and applications for concession contracts for the El Pino West and Heliconia properties, also in Antioquia.
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Sample from an outcrop of fault breccia containing pyrite and abundant iron oxide, at the contact between the Segovia Batholith and Cretaceous sedimentary rock, which is the Nus Fault. Lab results reported 5.51 g/t gold and 3330 g/t silver. This outcrop site is located within 50 meters of an artisanal mine near the south boundary of license 6717 on the Segovia Batholith / carbon rich sedimentary rock contact. Sample from an outcrop of a hard gray mineralized lava bed in the zone of alteration in sedimentary rock and mineralization is disseminated pyrite. This site is located in the south central part of the El Porvenir Project and is part of the Nus-Corales stream geochemical anomaly. The mineralized lava bed occurs is an area of intense sericite alteration of sedimentary rock. This alteration zone which also contains shear zones extends 3200 meters north and 800 meters south of the sample site.Sample from outcrop within the alteration zone containing multiple shear fault zones, and is hard baked black sedimentary rock containing coarse crystalline pyrite, and is part of the Nus-Corales stream geochemical anomaly. These heat baked mineralized sediment zones were originally rich in carbon (black shale). These altered sediments occur inside the four kilometer long sericite bleached zone which contains multiple shear zones and extends 3200 meters to the north and 800 meters to the south of the sample site.Sample from outcrop of jasperoid next to a shear zone in the four kilometer long sericite alteration zone containing multiple shear zones. The jasperoid is highly fractured and the fractures have been filled with quartz. This is part of the Nus-Corales stream geochemical anomaly. The zone of sericite bleached alteration, which contains multiple shear zones, extends four kilometers north from this site in the El Porvenir Project license 6717.Sample from outcrop next to shear zones and silicified beds. This is a sedimentary rock with intense sericite alteration, with disseminated pyrite and pyrite veinlets and is part of the Nus-Corales stream geochemical anomaly. This is in the far north of the El Porvenir Project license 6717, and is part of the same sericite bleached alteration zone which contains multiple shear zones for 3.5 kilometers south of this sample site.Sample from a silicified and mineralized gray lava bed that occurs in the sericite bleached alteration zone which is four kilometers long in the El Porvenir Project license 6717 and is part of the Nus-Corales stream geochemical anomaly. This sample site is central in the license and in the alteration zone which contains multiple shear zones. This zone containing the sample site extends 1300 north and 1700 meters south of the sample site.
NI 43-101 Technical Report for the El Porvenir project
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