BAROYECA GOLD & SILVER INC. announced the discovery of a widespread system of parallel veins at the La Ye target at the company's Atocha project in Tolima, Colombia following a large regional structure expanding its current footprint to over 250x500m. Another high-grade, gold and silver mineralized zone was discovered at Veta Grande, returning the best gold and silver assay results to date during this campaign and a new mineralized zone was also identified aligning with the Tavera vein system. The Company's geological team is working on the development of drill targets while conducting detailed geological/structural mapping. A robust geological model is being created based on structural interpretation using Lidar/DEM created models which is leading to the rapid discovery of a large number of vein occurrences. During the first month on the ground the geologists expanded the known vein system at La Ye and determined its continuity towards the west of the historical showings of Veta Grande from where the silver values (up to 3.48 kg/t silver) reported by the previous operator come. A series of sub-outcrops found during this program proved the continuity of the Tavera-Guaduas vein corridor, which is now in excess of 1,000m. Exploration during this program was focused on the identification and characterization of different vein exposures, following their continuity at surface and where possible collecting chip samples for assay to identify mineralized shoots within the veins. The best results (14.4 g/t Au and 420 g/t Ag) came from the western extension of the Veta Grande showings, where both gold and silver values are elevated and which extended the length of the identified high-grade shoot by an additional 100m. Most of the work performed to date has been focused on the La Ye vein zone, where systematic mapping and structural interpretation from Lidar imagery and DEM proved the existence of a major structural deformation corridor. The primary vein system is comprised of at least six major veins and several smaller associated veins covering a strike length in excess of 500m, which is open in both directions. Mapping has been possible due to the existence of a vast number of exposures and outcrop occurrences. Although these mineral occurrences are located in areas of intense weathering and saprock host, the first batch of rock chips collected at outcrops and sub-outcrops average 182 g/t Ag (or 304.4 AgEq). The principal veins show widths in outcrop ranging from 50cm to >2m and have a northeast strike and dip moderately to the NW, and secondary splays dip shallowly (10° to 30°). Veins are quartz dominant, showing marked banding with zones of semi-massive sulphides (pyrite, galena, sphalerite and Ag-sulfosalts) up to 30% locally.