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If sliced, the peridioles are exposed, giving the false impression of a stony-iron meteorite.
Chondrites are made primarily of rock and so have a lower density than stony-iron meteorites, which contain some metal.
Nickle-iron can be found in many stone meteorites in the form of small flakes or in irons and in stony-irons as large chunks or as the entire mass of the meteorite.
Material like that of the stony-irons is thought to occur at the core-mantle boundary of the Earth.
Irons and stony-irons are dense, with up to equal amounts of silicates and iron, and are often irregular in shape.
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