KRUISRIVIER COBALT PROJECT 62 • The geology of Kruisrivier Cobalt and the adjoining area has been researched in detail in South Africa and includes a portion of a small norite protuberance on the eastern rim of the Bushveld Complex • Several xenolithic bodies of Pretoria group quartzite and shale occur within this, with the largest and most southerly of these masses dipping at an angle of 50 to 60 degrees to the south and with the cobalt ore associated parallel to the quartzite bedding plane • The historic underground mine infrastructure is now largely inaccessible, other than a decline dipping at approx. 45 degrees (Fig 1) and from which the Company was able to complete inspection of the visible underground high-grade cobalt mineralisation • Numerous occurrences of cobalt mineralisation have been observed across the Kruisrivier Cobalt area and surrounding area (Fig 3)
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