The Skeletal System: Bones, Joints, and Cartilage

Updated July 2026
The human skeletal system consists of 206 bones in adults, along with cartilage, ligaments, and tendons that connect them. Beyond providing the rigid framework that supports the body and protects vital organs, bones are living, dynamic organs that produce blood cells in their marrow, store critical minerals like calcium and phosphorus, and continuously remodel themselves in response to mechanical stress throughout your entire life.

Bone as a Living Tissue

Bones appear solid and inert, but they are highly active organs with their own blood supply, nerves, and lymphatic vessels. Bone tissue is a composite material, roughly 65% mineral (primarily hydroxyapatite, a crystalline calcium phosphate) and 35% organic matrix (mostly type I collagen fibers). The mineral component provides compressive strength and rigidity, while the collagen provides tensile strength and flexibility. This combination gives bone a strength-to-weight ratio superior to steel or concrete: a cubic centimeter of compact bone can withstand compressive forces exceeding 170 megapascals.

Four cell types maintain bone tissue. Osteoblasts are bone-building cells that synthesize and secrete the organic matrix (osteoid) and regulate its mineralization. Once an osteoblast becomes embedded in the matrix it produced, it differentiates into an osteocyte, a mature bone cell that resides in a small cavity called a lacuna. Osteocytes communicate with each other through long cytoplasmic extensions (canaliculi) and act as mechanosensors, detecting mechanical stress and signaling where bone needs to be strengthened or removed. Osteoclasts are large, multinucleated cells derived from monocytes that break down (resorb) bone tissue by secreting hydrochloric acid and proteolytic enzymes. The balance between osteoblast building and osteoclast resorption determines bone mass and density.

Bone remodeling, the continuous process of breaking down and rebuilding bone tissue, replaces about 10% of the adult skeleton each year. This process serves multiple purposes: it repairs microdamage from daily mechanical stress, adjusts bone architecture to match current loading patterns (Wolff's law), and releases stored minerals when blood calcium levels drop. The entire skeleton is completely replaced roughly every 10 years, though the rate varies by location. Trabecular bone (spongy bone) in the spine and pelvis remodels faster than cortical bone (compact bone) in the femur shaft.

Bone Structure

A typical long bone, like the femur or humerus, has several distinct regions. The diaphysis (shaft) is a cylinder of compact bone surrounding a central medullary cavity filled with yellow bone marrow, which is mostly fat in adults. The epiphyses (ends) are expanded, knobby regions covered in articular cartilage where the bone meets other bones at joints. Beneath the articular cartilage, the epiphysis contains spongy (cancellous) bone, an interconnected network of bony struts called trabeculae that resemble a three-dimensional lattice. This spongy architecture distributes compressive forces while minimizing weight and provides spaces for red bone marrow.

The periosteum, a tough fibrous membrane, covers the outer surface of all bones except at articular surfaces. It contains osteoblasts for bone growth and repair, blood vessels that supply the outer bone layers, and sensory nerves, which is why a sharp blow to the shin (where the tibia lies just beneath skin and periosteum) causes intense pain. The endosteum, a thinner membrane, lines the medullary cavity and the internal surfaces of spongy bone.

Compact bone, when examined microscopically, is organized into structural units called osteons (Haversian systems). Each osteon consists of concentric rings (lamellae) of bone matrix surrounding a central canal (Haversian canal) that contains blood vessels and nerves. Osteocytes sit in lacunae between the lamellae and communicate through canaliculi that connect to the central canal. Perforating canals (Volkmann's canals) run perpendicular to the Haversian canals, connecting adjacent osteons and the periosteum to the medullary cavity. This network ensures that no osteocyte is more than 0.1 millimeters from a blood supply.

Divisions of the Skeleton

The skeleton divides into the axial skeleton and the appendicular skeleton. The axial skeleton, containing 80 bones, forms the central axis of the body: the skull (22 bones, plus 6 auditory ossicles), the hyoid bone (1), the vertebral column (26 bones: 7 cervical, 12 thoracic, 5 lumbar, 1 sacrum, 1 coccyx), and the thoracic cage (sternum plus 24 ribs). The axial skeleton protects the brain, spinal cord, heart, and lungs and provides the attachment base for the muscles of the head, neck, and trunk.

The appendicular skeleton, containing 126 bones, includes the upper and lower limbs and the girdles that attach them to the axial skeleton. The pectoral (shoulder) girdle consists of the clavicle and scapula on each side and attaches the arms. The pelvic girdle consists of the two hip bones (each formed from the fused ilium, ischium, and pubis) and attaches the legs. The upper limb includes the humerus, radius, ulna, 8 carpal bones, 5 metacarpals, and 14 phalanges. The lower limb includes the femur, patella, tibia, fibula, 7 tarsal bones, 5 metatarsals, and 14 phalanges.

The vertebral column is not a rigid rod but a flexible, curved structure. Its four curvatures, cervical (concave posteriorly), thoracic (convex posteriorly), lumbar (concave posteriorly), and sacral (convex posteriorly), distribute the weight of the upright body over the pelvis and lower limbs. Intervertebral discs, composed of a fibrocartilage outer ring (annulus fibrosus) and a gelatinous core (nucleus pulposus), sit between adjacent vertebrae and absorb shock during walking, running, and jumping. A herniated disc occurs when the nucleus pulposus protrudes through a weakened area of the annulus fibrosus, often pressing on spinal nerves and causing pain, numbness, or weakness.

Joints: Where Bones Meet

Joints (articulations) are classified by structure and by the degree of movement they allow. Fibrous joints, where bones are connected by dense fibrous connective tissue with no joint cavity, are generally immovable. Examples include the sutures of the skull and the syndesmosis between the tibia and fibula at the ankle. Cartilaginous joints, where bones are connected by cartilage, allow slight movement. The pubic symphysis and the intervertebral discs are cartilaginous joints.

Synovial joints are the most common and most mobile joint type. They feature a joint cavity enclosed by an articular capsule, with articular cartilage covering the bone ends, synovial membrane lining the capsule interior, and synovial fluid filling the cavity. Synovial fluid, a viscous liquid similar to egg white, lubricates the joint surfaces (reducing friction to a coefficient lower than ice on ice), provides nutrients to the avascular articular cartilage, and absorbs shock. Many synovial joints also contain menisci (fibrocartilage pads that improve fit and distribute load) and bursae (fluid-filled sacs that reduce friction between tendons, muscles, and bones).

Synovial joints are further classified by shape and movement. Hinge joints (elbow, knee) allow flexion and extension in one plane. Ball-and-socket joints (shoulder, hip) allow movement in all planes plus rotation, making them the most mobile joints. Pivot joints (atlas-axis in the neck) allow rotation around a single axis. Saddle joints (thumb carpometacarpal) allow biaxial movement. Condyloid joints (wrist) allow flexion, extension, abduction, and adduction. Gliding joints (between carpal bones) allow sliding movements in multiple directions.

Cartilage

Cartilage is a firm but flexible connective tissue found throughout the skeletal system. Unlike bone, cartilage lacks blood vessels, nerves, and lymphatic vessels, receiving its nutrition entirely through diffusion from surrounding tissues. This avascular nature is why cartilage heals slowly and often incompletely after injury. Three types of cartilage exist in the human body.

Hyaline cartilage is the most common type, found at the articular surfaces of synovial joints, in the tracheal rings, at the costal cartilages connecting the ribs to the sternum, and in the nasal septum. It provides smooth, low-friction surfaces for joint movement and structural support for the airways. Elastic cartilage, found in the ear pinnae and epiglottis, contains abundant elastic fibers that allow it to spring back after deformation. Fibrocartilage, the toughest type, contains dense collagen fibers and is found in the intervertebral discs, menisci of the knee, and pubic symphysis, where it absorbs compression and resists tearing.

Bone Development and Growth

Bone formation (ossification) occurs through two processes. Intramembranous ossification forms the flat bones of the skull, the clavicle, and parts of the mandible directly from mesenchymal tissue without a cartilage precursor. Osteoblasts differentiate within the mesenchyme and begin secreting osteoid, which mineralizes to form woven bone and later remodels into mature lamellar bone.

Endochondral ossification forms most of the remaining bones and is the process by which a cartilage model is gradually replaced by bone. A hyaline cartilage template forms first, then ossification begins at the primary ossification center in the diaphysis during fetal development. Secondary ossification centers appear in the epiphyses after birth. Between the primary and secondary centers, the epiphyseal plate (growth plate), a band of proliferating cartilage, is responsible for longitudinal bone growth. Chondrocytes in the plate divide, enlarge, and are replaced by bone in a coordinated sequence that lengthens the bone from its ends. Growth hormone, thyroid hormone, insulin-like growth factor 1 (IGF-1), and sex hormones all regulate this process.

The epiphyseal plates close (ossify completely) when growth is complete, typically between ages 18 and 25 depending on the bone and the individual. Once closed, no further longitudinal growth is possible. Bone can still increase in diameter throughout life through appositional growth, where osteoblasts in the periosteum deposit new bone on the outer surface while osteoclasts in the endosteum resorb bone on the inner surface.

Common Skeletal Conditions

Osteoporosis is a condition of decreased bone density and deteriorated bone microarchitecture that increases fracture risk. It affects approximately 200 million people worldwide, predominantly postmenopausal women, because the decline in estrogen after menopause accelerates osteoclast activity without a corresponding increase in osteoblast activity. Peak bone mass, reached around age 30, is the single strongest predictor of osteoporosis risk later in life, which is why building bone density through weight-bearing exercise and adequate calcium and vitamin D intake during youth is so important.

Osteoarthritis, the most common joint disease, affects over 500 million people globally. It involves progressive degradation of articular cartilage, leading to bone-on-bone contact, pain, stiffness, and reduced mobility. Unlike rheumatoid arthritis (an autoimmune disease), osteoarthritis is primarily a mechanical and biological degenerative condition associated with aging, joint overuse, obesity, and previous injury. Treatment focuses on pain management, physical therapy, weight reduction, and in severe cases, joint replacement surgery. Hip and knee replacements are among the most successful surgical procedures in medicine, with over 95% of implants lasting more than 15 years.

Fractures are classified by pattern (transverse, oblique, spiral, comminuted) and by whether the bone pierces the skin (open/compound vs. closed/simple). Bone healing follows a predictable sequence: hematoma formation at the fracture site, fibrocartilaginous callus formation (soft callus), bony callus formation (hard callus), and remodeling. Simple fractures in healthy adults typically heal in 6 to 8 weeks, though the remodeling phase can continue for months to years. Factors that impair healing include poor blood supply, infection, inadequate immobilization, smoking, diabetes, and nutritional deficiencies.

Key Takeaway

Bones are living organs that continuously remodel themselves, produce blood cells, store minerals, and respond to mechanical stress. The adult skeleton's 206 bones, connected by over 300 joints, provide the structural framework for all movement and organ protection, while the balance between bone building and bone breakdown determines skeletal health across a lifetime.