ePower Metals Inc. announced the results of the 2018 summer-fall exploration program at Panther Creek Cobalt Project located in the Idaho Cobalt Belt in Lemhi County, Idaho. Exploration mapping has defined three new cobalt targets which are supported by the soil and grab sample program. Assays from 43 rock and 746 soil samples from across the property have been received with rock values that range from trace to 30.8% Cu, trace to 29.67 g/t Au and trace to 0.4% Co. Results not only confirmed and expanded previously recognized Co-Cu±Au mineralized horizons but also discovered three new mineralized horizons. Soil sample results highlight two new areas of anomalous Co-Cu-Au. In addition, a major geological structure has been recognized coincident with Little Deer Creek. This fault projects along the southern extent of most of the historic mineralized horizons of the Blackbird Co-Cu deposit. This fault may have been a conduit for mineralizing fluids and may represent a significant geological target. The Little Bear Creek Horizon is partially covered but locally appears to be 1.5 metres ("m") wide and was traced for more than 150m along an east-west trend that remains open along strike, The zone is coincident with a large Co-Cu-As-Au soil anomaly that extends to the west for more than 1.2 kilometres ("km"). The high copper assays combined with low cobalt and arsenic and sulphur values suggest that outcrops are strongly oxidized and depleted of cobalt which has a much higher mobility than copper. Sampling and mapping of mineralized zones at the historic Little Deer Creek prospect has confirmed mineralization occurs in at least four parallel horizons, including two newly recognized zones. One newly discovered horizon is 40 metres up-slope of a horizon previously recognized and returned 0.87 g/T Au, 2.70% Cu, 0.27% Co from a grab sample of poorly exposed biotite schist. A second newly discovered horizon returned 2.0 g/t Au, 0.67% Cu, 0.02% Co from a grab sample of a partially covered, oxidized outcrop. Mapping and rock sampling within the Long Dike patented claims have revealed a Au-bearing quartz vein structure traced intermittently over a strike length of 500m, returning gold grades of 9.15 g/T, 7.84 g/T, 1.64 g/T and 0.39 g/T from grab samples. The 1m wide structure is composed of a series of narrow quartz veins. This structure has at least one historic adit with partially caved underground workings. Two chip samples in 2017 from near the adit returned 5.95 g/T Au and 4.15 g/T Au over 0.9m as reported in the Company's news release dated January 22, 2018. In a separate area, two float samples from quartz vein material returned 29.67 g/T Au and 22.68 g/T Au, respectively. Two extensive soil anomalies are recognized within the southern half of the property. A Co-Cu-As±Au soil anomaly extends for over 1 km and further south a predominately Cu anomaly extends for 1.4 km. These areas have not been geologically mapped although one reconnaissance mapping traverse recognized at least three geological units that show unique geochemical responses. In addition, geological mapping has recognized that there is a major NE-SW trending fault structure partially coincident with Little Deer Creek. The structure cuts the property with most of the known mineralization and soil anomalies occurring on the western side. This structure can be traced to the SW where it appears as the southern boundary for most the Blackbird mineralized horizons. This major structure has several coincident Co-Cu-As-Au soil anomalies and may represent a new drill target where it is in contact with highly prospective geological units.