Northwest Africa 999 is a brecciated eucrite composed of very fine-grained basaltic material, which represents both the host and the clasts within the meteorite. The very fine-grained texture of this eucrite is consistent with rapid cooling from an extruded igneous melt. Moreover, it exhibits the typical thermal metamorphic features characteristic of other equilibrated eucrites. From a preliminary analysis performed by UCLA, NWA 999 was determined to be an extremely fine-grained eucrite that is slightly Fe-rich and REE-rich. Black mineral grains (chromite?) are interspersed throughout the matrix, and a rare FeNi-metal grain is present in the specimen shown above. This eucrite was low to moderately shocked and is cross-cut by thin, dark gray, shock-melt veins. The specimen of NWA 999 shown above is a 2.44 g slice.