Macroscopic Description: Kathleen McBride
The exterior of this meteorite is covered by dull, thin, black fusion crust. Chondrules are visible through the fusion crust which covers 90% of this meteorite. The interior is a dark gray matrix with some light gray patches visible. This meteorite is loaded with chondrules, several mm in diameter, the largest seen is 7 mm. The meteorite has a high metal content and has rusty patches with metal veins. This ordinary chondrite was very heavy and difficult to break.

Thin Section (,2) Description: Brian Mason
The section shows a close-packed aggregate of chondrules (up to 1.8 mm across), chondrule fragments, and mineral grains in a dark matrix containing a moderate amount of nickel-iron and troilite. The meteorite is considerably weathered, with limonitic staining throughout the section. Microprobe analyses show olivine and pyroxene of variable composition: olivine, Fa_19-27, mean Fa₂₁; pyroxene, Fs_7-23. The meteorite is classified as an H3 chondrite (estimated H3.7).