Stress fractures are small incomplete fractures that often involve the metatarsal shafts. They are caused by repetitive weight-bearing stress.
Stress fractures do not usually result from a discrete injury (eg, fall, blow) but occur instead following repeated stress and overuse that exceeds the ability of the supporting muscles to absorb the stress. Stress fractures can involve the proximal femur, pelvis, or lower extremity. Over 50% involve the lower leg and, in particular, the metatarsal shafts of the foot. Metatarsal stress fractures (march fractures) usually occur in
They most commonly occur in the 2nd metatarsal. Other risk factors include the following:
Stress fractures also may be a sign of the female athlete triad (amenorrhea, eating disorder, and osteoporosis).
Symptoms and Signs
Forefoot pain that occurs after a long or intense workout, then disappears shortly after stopping exercise is the typical initial manifestation of a metatarsal stress fracture. With subsequent exercise, onset of pain is progressively earlier, and pain may become so severe that it prohibits exercise and persists even when patients are not bearing weight.
Patients who have groin pain with weight bearing must be evaluated for a proximal femur stress fracture. Patients with such fractures should be referred to a specialist.
Standard x-rays are recommended but may be normal until a callus forms 2 to 3 wk after the injury. Often, technetium diphosphonate bone scanning is necessary for early diagnosis. Women with stress fractures may have osteoporosis and should undergo dual-energy x-ray absorptiometry (see Diagnosis).
Treatment includes cessation of weight bearing on the involved foot (in case patients have a metatarsal stress fracture) and use of crutches. Although casting is sometimes used, a wooden shoe or other commercially available supportive shoe or boot is preferable to casting to avoid muscle atrophy. Healing can take anywhere from 6 to 12 wk.
Last full review/revision April 2009 by Brian D. Johnston; Paul L. Liebert, MD
Content last modified November 2010