Macroscopic Description: Cecilia E. Satterwhite
The exterior of this carbonaceous chondrite is covered with black fusion crust and is frothy in some areas. Flow lines are present on some surfaces. Areas devoid of fusion crust are brown, pitted and weathered. Fractures are numerous and penetrate the surface. The interior of the sample reveals a grayish-black matrix, weathered brown in areas. Minor white evaporite deposits are visible and small inclusions/chondrules are present but weathered.

Thin Section (,3) Description: Brian Mason
The section shows numerous chondrules (up to 1.8 mm across), irregular aggregates, and small mineral grains in a dark brown to black matrix; accessory nickel-iron and troilite are present, mainly rimming chondrules. The chondrules, aggregates, and mineral grains consist almost entirely of an isotropic to weakly birefringent serpentine; a little calcite is present. The meteorite is a C2 chondrite.