The matrix consists dominantly of an Fe-rich serpentine. The interior is a medium gray matrix that contains some rusty halos and minor metal. Light gray inclusions are present. The section exhibits isolated pyroxene and plagioclase grains up to 0.5 mm. The meteorite is a howardite.
Thin fractures penetrate the surface.
The interior matrix is light gray in color but most areas are rusty due to a high concentration of metal. No ringwoodite was noted. The interior is dark brown to black with some light colored crystalline faces in one area and some areas that are highly oxidized. A single plagioclase grain is An 91 Or 1 . The meteorite is a howardite.