Sample No . The exterior of this achondrite has patches of dull black fusion crust with polygonal fractures. Most of the fusion crust has weathered away. Several fractures are visible. This meteorite is very hard and extremely difficult to break.
Some areas are completely rusty.
Cleavage planes were visible on some of the larger mineral grains. This achondrite has an igneous texture. The section shows an aggregate of anhedral to subhedral grains, up to 6 mm across, of olivine and pyroxene. Individual grains are rimmed by carbonaceous material which contains trace amounts of nickel-iron and troilite. The meteorite is a ureilite.