FUSE BATTERY METALS INC 
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FUSE BATTERY METALS INC 
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The Glencore Bucke Project

Explore the vast potential of the Glencore Bucke Property with Fuse’s Teledyne Cobalt Project, featuring two patented mining claims spanning 16.2 hectares located on the western edge. Discover high-grade cobalt mineralization and join us on our journey to transform the world’s energy landscape.

Overview​ of the Glencore Bucke Project

The Glencore Bucke property consists of two patented mining claims totaling approximately 16.2 ha in area located on the west boundary of Fuse’s Teledyne Cobalt Project. In 1981, Teledyne leased mining claim 585 (“Glencore Bucke Property”) from Falconbridge Nickel Mines Ltd. The company recognized the significant exploration potential that the Property had due to the possible southern extensions of the Cobalt Contact veins on mining claim T43819 that projected southward onto the Property. In the fall of 2017, Fuse completed 21 diamond drill holes totalling 1,913.50 m at Glencore Bucke in a first phase of drilling designed to confirm and extend the existing known mineralized zones on the property. The program tested the Main Zone for a strike length of approximately 55 m and the Northwest Zone for a strike length of approximately 45 m.

Results were encouraging with the majority of holes hitting cobalt mineralization including 4.45% cobalt over 0.30 metres in hole GB 17-06 and 8.42% cobalt over 0.3 metres in hole GB-17-15 (core lengths only, not true widths.) In 2018, Fuse completed 24 diamond drill holes totaling 2,559 m in phase II at Glencore Bucke with the intent of intersecting mineralized zones along strike and vertically above and below previous intersections reported in 2017 on the Main and Northwest Zones. The Phase 2 program also tested several outlying targets with drill hole GB18-41 aimed at testing for mineralization at depth beneath a historical trench which intersected anomalous cobalt mineralization. Cobalt, zinc, silver and copper were present. Not all holes were released, with holes GB18-31 through to GB18-40 expected in Q2 2020.

Ontario, Canada

Cobalt Property

Ownership

100%

Total Area

40.23 ac
Fuse Battery Metals

Exploration and Development

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xxxxxx

Geology

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History

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DDHFrom (m)To (m)Core length (m)Co (%)Ag (ppm)Cu (ppm)Zn (ppm)Pb (ppm)
GB17-01182130.311.541274
GB17-0239.3739.670.30.42707210013621900
GB17-0327.1528.91.750.270.64272
GB17-0416.2516.750.51.627994349328
GB17-0622.524.251.750.25122881326
incl.23.2523.750.50.5828.9714396
GB17-0644.444.70.34.4534.24602600159
GB17-0799.79100.050.267.649.14414416
GB17-10283350.550.87322
GB17-1377.678.50.90.46132.51461417592059
incl.77.6780.40.792212400036703840
GB17-13100.51021.50.3298.881244176588
incl.100.8101.40.60.5516.949703766110
GB17-1527.528.40.90.552.12912618
incl.27.828.10.30.922.94020829
GB17-1542.562.720.20.1719.9898326384747
incl.62.462.70.38.421361280884447

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.
89

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Contact Details

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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.