How Old Bones Fracture [Lines Numbered for Reference] 1 2 Old bones fracture more easily than 3 young ones, even under small amounts 4 of stress. 5 This is partly because old bones lose 6 density, but partly because they also 7 change their structure. 8 9 Many human bones contain two different 10 internal structures. 11 Some central tissue is quite solid 12 (cortical bone). 13 Other tissue, however, contains a 14 cellular foam or open-celled lattice 15 of collagen (trabecular bone). 16 Trabecular bone occurs in 17 * individual parts of the spine 18 (vertebrae), 19 * the femur (the long bone that joins 20 the knee to the hip), 21 * the tibia (the larger of the two 22 bones connecting the knee to the 23 ankle), 24 * the humerus (the long bone linking 25 the shoulder to the elbow), and 26 * the iliac crest (the widest part of 27 the hip bone). 28 29 Trabeculae are like sponges. 30 They absorb loads from the joints just as 31 Styrofoam absorbs impacts in packages. 32 33 All bone renews itself regularly. 34 The human body continuously removes 35 old bone (resorption) and replaces it 36 with new bone (formation). 37 The average bone turnover rate is 38 about 6 years. 39 40 In menopausal women, however, this 41 turnover process becomes unbalanced. 42 More bone is resorbed that is formed, 43 so bone density decreases (osteoporosis). 44 Medical treatments for osteoporosis 45 usually focus on stopping resorption 46 of old bone while still allowing new 47 bone to fill in. 48 Reducing turnover in this way leaves 49 bone more massive yet also more brittle. 50 51 Three-dimensional computed-tomography 52 images reveal a structural change in 53 human trabecular bone with age. 54 In young bone, the trabeculae form a web 55 of short, stubby struts. 56 In older bone, on the other hand, these 57 trabeculae are mostly long, slender 58 columns. 59 60 Fracture (failure) in younger bones 61 usually happens when stress overcomes 62 the strength of the bone tissue. 63 Fracture in older bones happens at 64 much lower stress levels. 65 The long, thin trabeculae in old bones 66 are unstable. 67 Hence, when compressed, they buckle at 68 far lower stresses than bone tissue 69 normally withstands. 70 71 Bone resorption forms small pits on the 72 surface of the trabeculae. 73 As bone turnover increases, the number 74 of pits increases too. 75 76 An empty aluminum can requires much 77 stress to crush it axially. 78 But with a small dent in its side wall 79 the can buckles easily. 80 In the same way, trabecular pits are 81 themselves enough to destabilize 82 bone lattice. 83 In old human bone, 60% of trabeculae 84 are vulnerable to buckling just because 85 of their pits.