Ref.: South African Journal of Geology, Dec. 2004, V 107, N 4, pp. 505-520.
A PGE mine in a hortonolite-dunite body. Now closed. Workings were at least to the 250 foot/meter (?) level.
Platiniferous magnesian dunite subvertical cylindrical pipe crosscutting the layered cumulates of the Bushveld complex (Lower Zone).
Existence of magmatic replacement.
Magnesian dunite rimmed by harzburgite gradational intopyroxenitic wallrock (layered norites and anorthosites).
Mineral List:4 entries listed. 2 valid minerals.
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