There are many normal features which can mimic fractures
Genuine fractures are often accompanied by soft tissue swelling
Correlation with clinical findings is essential
There are numerous normal anatomical features which may mimic fractures. Careful correlation of X-ray findings with clinical features are often useful to eliminate significant injury.
Some fracture mimics have characteristic features. Here are some examples.
Unfused growth plate
To the uninitiated eye the growth plate in a young patient with an unfused skeleton can mimic a fracture.
Oblique distal clavicle shaft fracture with inferior displacement
Widening of the acromioclavicular joint (arrowheads) indicating dislocation
Lines passing through the acromion and proximal humerus are growth plates - not fractures
Unfused apophysis
The apophysis of the 5th metatarsal base is often mistaken for a fracture. Here the normal apophysis is orientated nearly longitudinally to the bone. A fracture at this site will typically be perpendicular to the length of the bone shaft.
Another clue is that the bones of an aphophysis will have a rounded and corticated edge. The edge of a fracture will be angulated with no cortication.
The normal apophysis runs lengthways along the bone
The fracture runs across the bone
Note the corticated and rounded edge of the apophysis compared with the sharp and non-corticated edge of the fracture fragment
Accessory ossicles
Accessory ossicles (small bones) are considered normal, but are not present in all individuals. They should not be mistaken for fractures. The best clue is that they have a dense fully corticated edge, whereas the edge of a fracture will not be corticated.
It should be remembered that although usually innocent, accessory ossicles and their surrounding soft tissues can be injured, and become symptomatic.
This patient has an extra bone adjacent to the navicular
This bone is normal - note the corticated edge
Vascular/nutrient lines
Bones are highly vascular structures that are penetrated by nutrient vessels. These appear as low density black lines which often mimic fractures. Characteristically they pass obliquely through the cortex and may have a visible corticated edge. They are not associated with loss of alignment of bone as seen in genuine fractures.
A well-defined lucent line passes lengthways through the bone
This vascular line passes obliquely through the cortex (lateral image)
A dense (white) corticated edge is a reassuring sign
Harris lines
You may see thin sclerotic lines passing transversely across the shaft of long bones. Although it is important not to overlook a genuine impacted fracture, these commonly seen lines are not pathological, and are considered developmental.