A little pyroxene near MgSiO 3 in composition is present. The matrix appears to consist largely of iron-rich serpentine. The meteorite is a C2 chondrite. Sample No . The exterior of this carbonaceous chondrite is covered with black fusion crust and is frothy in some areas.
Flow lines are present on some surfaces.
Areas devoid of fusion crust are brown, pitted and weathered. Fractures are numerous and penetrate the surface. The interior of the sample reveals a grayish-black matrix, weathered brown in areas. The meteorite is a C2 chondrite. Sample No .