A small spheroidal object, typically about 0.2–3.8 mm in size, although 0.5–1.5 mm is more usual, found in all chondritic meteorites except the CI subgroup of carbonaceous chondrites. The composition of chondrules varies widely, and may consist of one or more of any number of silicate minerals, or glass. Chondrules apparently existed independently before their incorporation in meteorites, but their precise origin is still unclear. Whatever their origin, chondrules are clearly some of the most primitive solid material in the Solar System.