This meteorite has been classified by the University of Washington with a description mentioning that it is a "monomict breccia composed of rock and mineral clasts derived from a plutonic eucrite." The classification also states that this meteorite contains "Calcic plagioclase, exsolved pigeonite, silica polymorph, troilite, Al-Ti-poor chromite and ilmenite (one grain with a very tiny zircon inclusion).  FeO/MnO ratios in host orthopyroxene (30.8) and exsolved clinopyroxene (30.0) are typical of eucrites"

The plutonic description would refer to the deep igneous or magmatic origin of this meteorite within the asteroid. This meteoritic material would have been later liberated during an impact event upon this asteroid. This meteorite is very unusual and unique with its obvious light coloured clasts set amongst a rich, contrasting charcoaled-coloured array of melt veins. There are also many vesicles throughout this meteorite which are primarily enclosed within melt veins. Some of these range up to centimetre-sized cavities. This is extremely rare and only a few Eucrites to date have been found with vesicles. The specimen below is an 8.7g Complete Slice and is part of the Meteorites Australia Collection (MA.06.0002). (High Resolution images also available below.)