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p. 8-9 Summary: The Tshipi Mine is located on the southern extremity of the Kalahari Manganese Fields ("KMF"), which covers an area of approximately 23, 000 hectares. The KMF is known to contain approximately 80% of the world's in-situ manganese resources. It is important to note that the Tshipi orebody is contiguous with and is the direct extension of South32's (formerly BHP) Mamatwan operation that has been producing manganese for over 50 years. The KMF is dominated by the Hotazel geological formation comprising three sedimentary manganese layers interbedded with banded iron formations. Of the three sedimentary manganese layers, the lower manganese deposit is the best developed and laterally continuous. The middle and upper manganese orebodies act as stratigraphic markers rather than potential mining targets given the relatively low manganese content contained in these layers. The lower manganese orebody ("LMO") consists of banded, very fine-grained braunite-kutnahorite lutite, containing concretionary ovoids, laminae and lenticeles of Mn-calcite with which hausmanite is commonly associated.
