Abstract
Fractures occurring in the humerus, ulna, radius, femur, tibia, and fibula are collectively categorized as long bone fractures. Long bone fractures are further classified by type and location. Interpretation of the forces associated with the fracture depends on the location, type, and extent of the fracture. Common long bone fracture types include spiral, oblique, transverse, torus (or buckle), greenstick, and classic metaphyseal lesion (CML) [1]. A spiral fracture circles the shaft and typically results from a rotational force. An oblique fracture crosses the bone diagonal to the long axis, and a transverse fracture crosses the bone at a right angle to the long axis. A torus (or buckle) fracture, in which the cortical bone balloons out, is typically the result of a compression force loading through the long axis of the bone. A greenstick fracture is an incomplete fracture, most often an incomplete transverse fracture, and is commonly found in children as a result of the increased elasticity of the developing bone. CML is a fracture of the physeal plate of a long bone.
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Love, J.C., Derrick, S.M., Wiersema, J.M. (2011). Long Bone Fractures. In: Skeletal Atlas of Child Abuse. Springer’s Forensic Laboratory Science Series. Humana Press. https://doi.org/10.1007/978-1-61779-216-8_5
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