In life, bone is one of the connective tissues of the body and consists of crystallites of the mineral hydroxyapatite, deposited on a fibrous matrix of the protein collagen. Mineral occupies 71 per cent of the volume, collagen 19 per cent, other proteins 2 per cent, and water 8 per cent. After death, the proteins slowly decompose (this gradual decomposition forms the basis of a bone dating method — nitrogen analysis). The remaining mineral is subject to solution in acid soil conditions. Bones are preserved on a wide variety of archaeological sites, and the state of bone preservation varies widely. Two main types of bone are found in mature animals: compact, or cortical bone and cancellous, spongy or trabecular Compact bone forms the dense outer layer in a particular structure of the skeleton. Cancellous bone is found inside, forming a light internal framework. Bones as elements of the skeleton have a number of forms: long bones — as in the limbs; flat bones — as in the cranial vault of the skull; cuboidal bones — as in the wrists and ankles; irregular bones — vertebrae and bones of the face and jaws. For the study of bones from archaeological sites, see skeleton. Bone was also used as a raw material for making artefacts.
The Macmillan dictionary of archaeology, Ruth D. Whitehouse, 1983Copied