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Location: 52 km S from Musina, South Africa
Ground Floor Greystone Building Fourways Golf Park, Roos StreetFourwaysSouth Africa2191
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Coal forms in sedimentary environments due to the accumulation, compaction and induration of variously altered plant matter. Coal is a readily combustible sedimentary rock containing more than 50% by mass and more than 70% by volume, carbonaceous material. Coal typically occurs as seams and the presence thereof is determined by the palaeo-depositional environment occurring at the time of deposition and subsequent preservation mechanisms. Formation of coal and the resultant quality of coal is determined by the depositional setting and pressure and temperature conditions post-deposition and postcompaction.DimensionsThe project extends approximately 17km along strike with a dip of 12° to the north. A limit of approximately 30m of oxidation has been used to limit the upper boundary near the outcrop. The open cast depth has been theoretically defined as 200m below topography and this is the limit of the resource.