Small inclusions of Olivine can be seen on all specimens, within the metal, with the aid of 10X magnification. The specimens in this group exhibit naturally oxidized, reddish-brown surfaces, without saw cuts or polished areas. Olivine can be seen in several areas on the sides and back of the specimen. This specimen could be enhanced for exhibit by sawing and polishing one of the edges to reveal the fresh metal and Olivine, same as the Type I specimens above. 550.00 grams - large natural specimen with distinct regmaglypts.
Metallic inclusions are sparse, and very fresh.
A fairly good size exposure of the fusion crust is present on the back of the specimen. The Hugoton H5 has a dark brownish-black, brecciated stone matrix with sparse metallic inclusions. All specimens have American Meteorite Laboratory labels.