Fuse Cobalt Inc. announced that Simcoe Geoscience of Stouffville, Ontario completed a detailed induced polarization geophysical survey utilizing the Alpha IP Wireless Time Domain Distributed Technology System over the Glencore/Bucke Project at Cobalt, Ontario. Preliminary 2D profiles and an early 3D model have been received with promising chargeability results evident. The complete report including final results and recommendations is estimated to take a further two weeks at which time the results will be released.

The objective of the survey was to resolve narrow vein cobalt and silver mineralization and any cross-cutting structures to a depth of approximately 125m on 400m long grid lines with a 50m line spacing. Previous drilling has indicated veins to be present at least 100m from surface, and this survey will assist in determining if the mineralization continues both up and down dip along the structures. The technical team will correlate the new IP geophysical data with the existing drillhole database to create new drill targets for the upcoming drill program.

In addition, the survey may assist in identifying volcanic hosted massive sulphide (VHMS) mineralization by tracing/correlating polymetallic intersections in drill holes GB 18-44 and GB 18-45 to the IP results. Although there has been no success to date in locating economic VHMS deposits in the Cobalt camp, the possibility should not be dismissed. (Joerg Kleinboeck P. Geo and David Jamieson, P. Geo, Ni 43-101 Report on the Glencore/Bucke and Teledyne Properties, Feb.

2021). For example, step out hole GB 18-44 intersected visible cobalt mineralization returning 0.11% Co, 9.4 g/t Ag, and 1.04% Cu over 8.40m from 110.60 to 119.00m.