Camino Minerals Corp. has completed an extensive surface exploration program within the Diva trend at the 20,000 hectare Chapitos Copper-Gold project, near Chala, Southern Peru. As reported on November 22, 2018, Camino has conducted intensified surface exploration at the Chapitos project. In total, 851 rock samples have been collected and have now delineated a 7km by 1.5km area that have named the "Diva trend." The rock samples were submitted to ALS Global for analysis and their copper results ranged from less than detection up to 15% Cu, with an average of 0.69% Cu. The Diva trend is host to the Lourdes, Adriana, Katty, Maria, Pilar, and Vicky copper occurrences. The Diva trend is open to the northwest and to the southeast and to date less than 20% of this trend has been drill tested (Adriana, Katty, and Vicky occurrences) and the rest remains open. The Diva trend comprises a broad zone of Copper (rock and soil) anomalies that is parallel/sub-parallel to the northwest trending contact between a Jurassic Volcano-sedimentary sequence (to the north) and a Cretaceous Monzonite Intrusive complex (to the south). The Diva fault, which lies within the Diva trend at or near this volcanic-intrusive contact, and was confirmed by the 2017-2018 Adriana drilling programs, appears to be an important control for copper mineralization and/or surface anomalism along the trend, although additional parallel structures also appear to be present. In addition, several intense zones of silica replacement, referred to as aplitic dykes on regional government maps, are also spatially associated with the Diva fault at, and northwest of, the Adriana area. Soil sampling was conducted at 25m intervals along northeast trending grid lines with 100-200m line spacing. A total of 2750 soil samples have now been collected along the Diva trend, as illustrated in Figure 1, which comprise an initial group of 1550 samples collected along wide-spaced lines that were analyzed in Chala by the Company using a portable XRF unit and a further 1200 infill soil samples that were submitted to ALS Global for ICP analysis (note: duplicate sampling has confirmed that there is no statistical difference between the pXRF and ICP Cu soil data). The Diva trend copper (Cu) data is illustrated in the accompanying figure (Figure 1) with both colored symbols (circles) at each sample site on top of a gridded (kriged) copper image (TIFF). Newly delineated soil anomalies and high-grade rock samples exist along the Diva trend at the Maria and the Lourdes copper occurrences. The Maria copper occurrence lies approximately 2.5km SSE of the Adriana area and is defined by a ~600m-long Cu-in-soil anomaly near the south end of the Diva Trend, where recent sampling of copper-oxide mineralized volcanics has yielded high grade results. This target has not yet been drill tested. At Lourdes, which lies approximately 1.5km NNW along strike from the Adriana occurrence, an 800m-long Cu-in-soil anomaly has been identified with coincident high-grade rock samples and also remains to be drill tested.