Bone can be categorized into two morphological components: cortical and cancellous bone. The dense cortical bone envelopes the entire structure, while cancellous – or trabecular – bone is typically found towards the ends of the bone. The internal spaces of bone are filled with marrow. Reprinted, with permission, from Lynch SE, Genco RJ and Marx RE (1999) Tissue Engineering: Applications in Maxillofacial Surgery and Periodontics. Quintessence.

Diagram depicting a section of the cortical shaft of a long bone, showing the arrangement of the lamellae in the osteons, the interstitial lamellae, and the outer and inner circumferential lamellae. The outer surface is protected by the periosteum, while the inner surface is covered by the endosteum. Within the cortical shell, the branching out of the buttressing trabeculae can be seen. Reprinted, with permission, from Bloom W and Fawcett DW (1986) A Textbook of Histology, 11th edn. Saunders.

Bone may be categorized into three microstructural components: (1) bone cells, which include osteoblasts, osteocytes and osteoclasts (stained with a modified Goldner trichrome stain); (2) an organic matrix consisting of collagenous and noncollagenous factors, such as the bone morphogenetic proteins (the mineralized matrix has been removed and cells have been coloured green to distinguish them from the organic framework); (3) an inorganic component consisting primarily of calcium and phosphate; this component has been stylized as an array of hexagonal crystals. Reprinted, with permission, from Lynch SE, Genco RJ and Marx RE (1999) Tissue Engineering: Applications in Maxillofacial Surgery and Periodontics. Quintessence.

Osteoclasts (red) and osteoblasts (dark green) interact through cytokines released into the bone micromilieu. Macrophages secrete (MCSF), various interleukins and tumour necrosis factor, all of which promote osteoclast differentiation from haematopoietic stem cells, from the s (CFU‐GM) and the (CFU for macrophage) to terminal osteoclast phenotype. Osteoblasts interact by expressing factors which affect osteoclasts, mainly RANKL and MCSF, as well as factors affecting bone mineralization and progression of their own phenotype, such as insulin‐like growth factors and basic fibroblast growth factors. Importantly, disuse will also upregulate osteoclast activity, while increases in mechanical factors will elevate bone formation.

Development of a long bone as shown in longitudinal sections (A–J), and in cross‐sections A′, B′, C′ and D′. Pale blue is cartilage; purple, calcified cartilage; black, bone; red, arteries. A, The original cartilage model of the bone; B, a periosteal collar of bone appears before any calcification of cartilage occurs; C, cartilage begins to calcify; D, vascular mesenchyme enters the calcified cartilage and divides it into two zones of ossification (E and F); G, blood vessels and mesenchyme penetrate the epiphyseal cartilage and the epiphyseal ossification centre develops within it; H, a similar ossification centre develops in the lower epiphyseal cartilage; as the bone ceases to grow in length, the lower epiphyseal plate disappears first (I) and then the upper epiphyseal plate (J). The marrow cavity then becomes continuous throughout the length of the bone, and the blood vessels of the diaphysis, metaphyses and epiphyses intercommunicate. Reprinted, with permission, from Bloom W and Fawcett DW (1986) A Textbook of Histology, 11th edn. Saunders.

The cutting–filling cone has a head of osteoclasts that cut through the bone, and a tail of osteoblasts that form a new secondary osteon. The velocity through bone is determined by measuring between two tetracycline labels (1 and 2) administered 1 week apart. Reprinted, with permission, from Graber T and Vanarsdall RL (2000) Orthodontics: Current Principles and Techniques, 3rd edn. Mosby.