Figure 5. Hand-specimen photographs of serpentinite cataclasites (deformation stage D). A. Sample 149-897D-17R-4, 104–117 cm. B. Ronda peridotites (Betic Cordillera, southern Spain); sample was collected in a brittle fault zone south of the Ronda Massif. This sample is more cohesive than those shown in Plate 4, Figure 2. Note the similarity of the fragment angularity and fabric. In both cases the matrix is calcite-free comminuted serpentine. Scale bar = 2 cm.