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 . The interior is light gray with clasts up to 3 cm in diameter. Plagioclase and pyroxene grains are numerous.