FUSE BATTERY METALS INC 
$0.0314  $0.0002  0.64%  
FUSE BATTERY METALS INC 
$0.05  $0.005  11.11%  

The Teledyne Cobalt Project

Unlocking the Potential of Cobalt: Fuse’s Teledyne Property, a Valuable Asset with Historical Drilling and Infrastructure for Future Exploration.

Overview of the Teledyne Project

In 2016, Fuse entered into an option agreement to acquire up to a 100% interest, subject to a 2% net smelter royalty (“NSR”), on the Teledyne Cobalt Property then in the spring of 2018, Fuse announced that it had amended and accelerated the option agreement and had earned a 100% interest in the Property with the vendors retaining the 2% NSR. The Property, located in Bucke and Lorrain Townships, consists of 5 patented mining claims totaling 79.1 ha, and 46 unpatented mining claim cells totaling approximately 705.99 ha. The Property is easily accessible by highway 567 and a well-maintained secondary road.

Based on historical drilling and data a cobalt resource was developed in the 1980’s however it is not consistent with current 43-101 standards and will require work to be completed by a QP in order to be brought up to current NI -43-101 resource standards. As such the Company is not treating the historical reserve estimate as a current mineral resource or mineral reserve. Over $25 million Can has been spent thus far, (2020 dollars inflation-adjusted) on the Teledyne Property resulting in valuable infrastructure including a development ramp and a modern decline going down 500 ft parallel to the vein.

Ontario, Canada

Cobalt Property

Ownership

100%

Total Area

1500 ac
Fuse Battery Metals

Latest Developments at Fuse's Teledyne and Glencore Bucke Cobalt Properties

Teledyne Cobalt Property

In 2017, Fuse completed 11 diamond drill holes totaling 2,204 m at the Teledyne Cobalt Property, testing the Main Zone for a strike length of 220 m and confirming mineralization along strike and up and down dip. Results included 1.82% cobalt over 6.00 m and 5.06% Co over 1.75 m. In 2018, Phase 2 drilling involved 9 additional diamond drill holes totaling 1,713 m, testing mineralized zones and outlying targets, with results expected in Q2 2020. The Teledyne Cobalt Property covers 607.1 ha with 5 patented and 8 unpatented mining claims, while the Glencore Bucke Cobalt Property consists of 1 patented mining claim covering approximately 16.2 ha. Both properties have off-take agreements with Glencore Canada Corp, the world’s largest cobalt producer.

Geology

xxxx

History

xxxxx

Significant cobalt intersections from the Phase 1 diamond drilling program include:

Hole_IDCo_pctLength_mFrom_mTo_m
TE17-010.626136142
incl.3.920.75140.25141
TE17-020.951.9143144.9
incl.2.580.6144.3144.9
TE17-020.593.9156159.9
incl.2.220.6156.6157.2
TE17‐041.826138144
incl.5.061.75141.25143
TE17‐052.324126.5130.5
TE17‐051.76136142
TE17-070.52.1127.6129.7
TE17-080.773.4169.5172.9
incl.1.172169.5171.5
TE17-080.591.2174175.2
TE17-080.620.6178.6179.2
TE17-110.542130132

Key Advantages

Environmental

We follow strict policies and procedures to minimize the impact of our exploration and development activities on the environment and local communities. We engage with local stakeholders and respect their rights and interests.

Market Potential

The demand for Lithium is expected to increase significantly in the coming years due to its crucial role in the production of electric vehicle batteries and energy storage systems, driven by the rapid growth of the electric vehicle market

Shareholders

With our expertise in mineral exploration and our commitment to environmental and social responsibility, we are well-positioned to unlock the potential of the Lithium deposit and create value for our shareholders and stakeholders.
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Geological Summary of Holes NN2001 thru NN2208

Generally, mineralization is found in three distinct horizons of silty, weakly calcareous, claystone and with seams of blue-grey clay. Sedimentary textures are not well preserved in the chips, so the depositional environment is not clear, but it is thought to be in a lakebed environment. Rocks between the productive horizon are mostly reduced felsic air fall tuffs and tuffaceous siltstone. All holes ended in coarse cobble to pebble conglomerate or ash flow tuff. The lower tuff shows moderate propylitic alteration with replacement of mafic minerals by chlorite and disseminated pyrite.