First Cobalt Corp. announced positive assay results from two holes intersecting cobalt mineralization on two separate veins in the Woods Extension area of the Cobalt Camp, Ontario. One intersection occurs along strike of the Watson vein and the other is likely a new vein between the Woods and Watson veins. These intercepts, in conjunction with previous results from this area, suggest a broad deformation zone of mineralization may exist between the Woods and Watson veins. The Woods and Watson veins accounted for over 80% of the production in the southern end of the Cobalt Camp area known as Silver Centre. The veins were previously believed to have ended at an east-west fault. Nine drill holes were completed at the Woods Extension area to the north of the Frontier mine to test the possible extension of the Woods and Watson veins. Assay results have been received from seven drill holes. Calcite veins have been intersected in most holes and five holes returned anomalous cobalt (>0.05% Co). A number of samples from these five drill holes have also returned anomalous silver (>10 g/t) as well as other metals Cu, Zn and Pb, which may represent a broad zone of mineralization rather than discrete individual veins. The lower grade of silver mineralization may explain the lack of mine development to the north of the historic Frontier mine, but this area remains prospective for cobalt mineralization. Hole KF-WV-0003 intersects a calcite vein containing cobalt occurring between the Woods and Watson Veins, including 0.57% Co and 1.4% Ni over 0.4m. The higher grade nickel is noteworthy as this has not been described previously in this area. Elevated nickel is commonly associated with cobalt-silver mineralization elsewhere in the Cobalt Camp suggesting this vein may be part of a network developed in a broad deformation zone between these two major veins. Early results from hole KF-WV-0002, which is collared at the same station as KF-WV-0003, were reported November 2, 2017. Further interpretation of KF-WV-0002 indicate an intersection of the Woods Vein at 111.9m, where cobalt was assayed above (>0.05% Co) and below (0.03% Co) historic mine workings, thereby providing support to the view that KF-WV-0003 encountered a new vein. KF-WV-0007 to the north KF-WV-0003, returned 0.34% Co over 0.4 metres. Multiple holes were collared from the same drill station in many locations during this program to determine the dip of the major veins within the Keeley-Frontier mines. Although only a few intersections are now interpreted in this area, the Watson vein does appear to bend around mafic and felsic dykes, therefore could easily have been missed by mining along a single narrow drift.