Puma Exploration Inc. announced that during the initial exploration work conducted on the Chester property in November and December 2019, Puma sampled 1.87% Cu, 1.36% Cu and 1.03% Cu in trench T19-04 located in the East Zone. Furthermore, Puma reported values of up to 1.06 g/t Au in the gossan zone overlying the East Zone recently trenched by the technical team. Very limited gold analysis has been performed in the past and will be systematically evaluated in the upcoming exploration programs. The trenching program also identified a large hydrothermal system characterised by geochemical anomalies (Se/S, As, Cu+Pb+Zn, Mg+Fe, Ba and Si) located NE of the East Zone. The Se/S ratio can be used as an indicator of a probable magnetic component for high temperature sulfurs (hydrothermal alteration). Adding to the alteration signature, the area coincides with a major gravity anomaly and a low magnetic boundary. Only one hole was drilled by Noranda and was then deepened by Teck in 1994 (CN-12) in the area. The hole CN-12 intersected the favorable horizon consisting of strongly altered and variably mineralized felsic volcanic grading 0.19% Pb+Zn over 118 meters without any further follow-up program. The East Zone and Central Zone represent the most prospective areas of the property to find significant new deposits as the previous operators and the recent work concentrated their efforts on the West Zone (feeder zone). No mineral resource estimates have been calculated under NI43-101 guidelines for the Central and the East Zones and most of the holes drilled were completed before the 1980’s. The massive sulphide zones are exposed at the surface as a gossan mineralization. The previous operators at Chester Deposit reported historical resources totalling 16.8 Mt at 0.76% Cu divided in three zones: East Zone: 0.5 Mt of massive and disseminated sulphide grading 0.78%Cu, 0.36% Pb and 1.14% Zn. Central Zone: 1.1 Mt of massive sulphide grading 0.47%Cu, 0.90% Pb and 2.22% Zn. West Zone: 15.2 Mt of copper stringers grading 0.78%Cu.