They show a few small chondrules, up to 0.5 mm across, some irregular aggregates, and numerous small mineral grains in a translucent brown isotropic matrix. The mineral grains are almost entirely olivine, near Mg 2 SiO 4 in composition, with a few iron-rich grains. The matrix consist of iron-rich serpentine. The meteorites are C2 chondrites. The exterior of this meteorite has some patches of thin shiny black fusion crust.
Most surfaces have a brownish color and areas of heavy oxidation are yellowish-brown in color.
A few fractures penetrate the interior. Despite the abundant metal, this stone broke easily. Minor weathering is indicated by a moderate amount of brown limonitic staining. The meteorite is a mesosiderite. Interior is black with some inclusions and metal visible despite the heavily oxidized interior.