In the clast, olivine composition is Fa16-18, pyroxene Wo10Fs15. The meteorite is tentatively classified as a C3 chondrite of the Vigarano subtype. Roughly half of each of these specimens is covered with weathered black fusion crust. Evaporite deposit was noted on RKP92416. Abundant small light and dark inclusions are present in the dark gray to black matrix.
Oxidation is heavy but metal is still obvious.
Brown limonitic staining pervades the sections. It is smooth and shiny in areas. This meteorite is heavily weathered. No features were noted in the dark red brown, fine-grained matrix. The meteorite is severely weathered, with veins and patches of red-brown limonite throughout the section.