The quartz of the Witwatersrand gold-ore deposits contain abundant pebblelike forms of pyrite. The pyrite and its pebblelike forms have been studied by a number of authors. The data obtained in this study indicate that pebblelike pyrite forms in the Witwatersrand gold-bearing conglomerates make up four groups: (1) consisting of round, ellipsoidal or, less commonly, pear-shaped concretions, usually with a concentrically zoned structure; (2) representing pyrite pseudomorphs after alluvial pebbles of different compositions; (3) represented by so-called 'shot'; (4) represented by round pyrite shapes. The occurrence of these four groups of pseudopebbles suggests that in the Witwatersrand ores, there are no alluvial pyrite pebbles.