The latter phases often occur as rounded enclaves in the enstatite. The meteorite is an unusual aubrite. Sample No . The interior is a steel gray color with rusty patches and is somewhat flaky. It is very dense with no visible inclusions.
Olivines exhibit planar fractures and mosaicism.
Sample No . The exterior of this carbonaceous chondrite is dull and black with white evaporites along the edges. The top face has a large yellowish brown inclusion. The meteorite appears to have no fusion crust. The interior is brown, very weathered and crumbles easily.