Intersections Reported At West Joe Dyke

VANCOUVER - Power Metals Corp.reported that drill holes have intersected lithium (Li), cesium (Cs) and tantalum (Ta) mineralization with 20.25 % Cs2O, 1.29 % Li2O and 147 ppm Ta over 1.0 m in drill hole PWM-22-150 in the West Joe Dyke, Case Lake property, Cochrane, Ontario. High-grade Li-Ta mineralization was also intersected: 3.10 % Li2O, 0.09 % Cs2O and 841 ppm Ta over 2.0 m in drill hole PWM-22-149.

West Joe Dyke is a three-commodity pegmatite with lithium (Li), cesium (Cs) and tantalum (Ta) mineralization. The Ta mineralization occurs in the aplite border zone, the spodumene zone and the pollucite zone. The Li mineralization occurs in the spodumene zone and the pollucite zone. The spodumene ranges in color from pale green to white to pink to purple in the spodumene zone. The Cs mineralization occurs in the pollucite zone as a pod in the center of the West Joe Dyke.