NWA 13951 is a fine grained brecciated mix of plagioclase, olivine and melts. Numerous Fe-Ni metal grains are seen scattered throughout the meteorite. Cut surfaces of NWA 13951 show numerous clasts with gray and white grains bounded by darker melt veins. NWA 13951 was found with no remaining fusion crust. Some of the metal grains are as large as 1mm.