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Single crystals of natural diamond which exhibit an approximately cubic morphology are known to have grown either (a) by nonfaceted cuboid growth or (b) by fibrous growth branching in a multiplicity of <111> columns, to give a mean surface orientation of {100}. Interpenetrant twins of diamond are uncommon; but when they occur they are usually coloured and appear (by X-ray topography) to have been formed by fibrous growth upon a twin origin, with the 14 growth sectors adequately filled by fibres, without the necessity of branching.