Summary

Mine Type	Open Pit
Study Completed	Feasibility
Stage	Permitting
Commodities	Copper
Mining Method	Truck & Shovel / Loader
Project Timeline	...
Mine Life	...
Snapshot	Omitiomire is a fully de-risked copper project with a completed Bankable Feasibility Study, a valid mining licence through 2036, and environmental approvals submitted for construction and operation. Over US$30 million has already been invested in technical and regulatory development. The project is now positioned to transition into execution, with a strategic partner being sought to advance to production. Designed with a strong sustainability profile, Omitiomire features a closed water system, advanced evaporation management, and a heap leach process that uses only one-third of the water compared to conventional flotation. As of November 2024, the Project has completed the Environmental and Social Impact Assessment (ESIA) and the Environmental and Social Management Plan (ESMP) – both of which have been submitted to the relevant regulatory authorities as part of the Environmental Clearance Certificate Application to construct and operate the mine.

Deposit type

• Metamorphic hosted

Summary:

The Omitiomire Copper Deposit lies within the Kalahari Copperbelt. Geophysics and regional work have suggested an along-strike correlation of geology between Zambia, Botswana and Namibia. Some of the major copper deposits of northern Zambia, including Lumwana and Sentinel/Kalumbila, are associated with geological formations that share similarities with Omitiomire in the Damara Belt and other deposits in the Ghanzi-Chobe Belt.

Mineralisation occurs in the Ekuja Dome inlier, which covers an area of approximately 15 km x 12 km. The Dome is one of three dome-like gneisses penetrating through overlying high-grade metasediments. Rocks are mainly felsic gneiss with subordinate amphibolite and mafic schists, probably of volcanic origin. The Dome system is similar to Sandfire’s Motheo in Botswana and other regional deposits.

Deposit geology comprises two main rock packages:
• Mafic rocks, hosting the Cu mineralisation, mainly of quartz, plagioclase, dark biotite and amphibole. Mineralised banding up to 100m thick;
• Surrounding leuco-gneisses usually unmineralized, quartz, plagioclase, variable amounts of biotite and trace amounts of garnet and sphene.

Orebody strike length of 3.5km, open at depth.

Mining Methods

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Comminution

Crushers and Mills

Processing

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Commodity Production

Operational metrics

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Personnel

Job Title	Name	Profile	Ref. Date
.......................	.......................		Sep 2, 2025

Total Workforce	Year
......	2024