Approximately true size. Slice of a stony iron meteorite. Other part is olivine crystals. Approximately twice actual size. Light gray colored.
Ordinary chondrites Have light-colored spherical structures called chondrules.
May be droplets of once molten material. Most abundant type of meteorite. Minerals were formed at low temperatures. Contain chondrules and irregular pieces of crystalline material. Overall, chemically similar to the sun, but without the H and He.