A problem first described in marching soldiers

In 1855, a German military surgeon named Breithaupt described a curious pattern of foot pain and swelling in young army recruits. It was later understood to be closely tied to marching — and so earned the name “march fracture.” Today we call it a stress fracture, and more than a century and a half later, soldiers in training, runners, dancers, and athletes remain the classic patients.

What is a stress fracture?

A stress fracture is not caused by a single injury. It is a fatigue failure of bone — the result of repetitive loading that outpaces the bone’s ability to repair itself. Under Wolff’s law, bone is living tissue that constantly remodels in response to mechanical load: osteoclasts resorb bone, osteoblasts build it, and normally the bone adapts and grows stronger. But when strong, frequent forces are applied faster than this remodeling can keep up, the bone progressively weakens instead of strengthening, and microscopic damage accumulates into a crack.

Other contributing mechanisms have been proposed: muscle fatigue reducing the limb’s ability to absorb shock, repetitive traction from muscles pulling at their bony attachments, and transient ischemia with each impact increasing osteoclast activity.

Who gets them, and why

Stress fractures account for roughly 1–7% of sports injuries — and by some reports up to 20% of patients presenting to a sports clinic. They occur mainly in people doing weight-bearing activity such as running and jumping, especially in high-intensity groups like military recruits, athletes, and dancers.

Risk factors fall into two groups. Intrinsic factors include cavus (high-arched) feet, leg-length discrepancy, excessive forefoot varus, tarsal coalition, a prominent posterior calcaneal process, tight heel cords, osteopenia or osteoporosis, poor vascular supply, and abnormal hormone levels — including, in female athletes, low energy availability (RED-S, formerly the female athlete triad). Extrinsic factors include the type of activity, an excessive or brand-new training regimen, poor footwear or equipment, improper technique, the training surface, and sleep deprivation. A stress fracture is often a signal to look at the whole patient, not just the bone.

The most common sites are the posteromedial distal tibia, the metatarsals, and the calcaneus. Interestingly, the pattern differs by sex in military recruits: men tend to sustain metatarsal (about 66%) and calcaneal (about 20%) fractures, whereas women more often have calcaneal (about 39%) and tibial (about 27%) fractures, more frequently bilateral and appearing earlier in training.

The typical story — and why X-rays can look normal

The history is usually telling: mild pain or discomfort that appears after a certain amount of activity, sometimes with swelling and focal tenderness. Push through it, and the pain worsens and starts to appear earlier and earlier in the activity. On examination there is a focal spot of tenderness — broader and more diffuse in the early stress-reaction phase. Symptoms in metatarsal fractures tend to appear much faster than in the tibia or fibula, typically within two to six weeks.

Early on, plain X-rays are frequently normal — abnormalities such as cortical lucency, sclerosis, endosteal callus, or a fracture line usually take at least two to three weeks to appear, and occasionally up to three months. When suspicion is high, an early bone scan (99mTc) or, better, MRI is recommended: MRI detects bone marrow edema (the earliest stage of bone stress injury) and shows how advanced the injury is, which directly guides treatment. Occasionally a stress fracture must be distinguished from an osteoid osteoma — characterized by night pain relieved by aspirin, and a nidus visible on CT or MRI.

Location matters: low-risk vs high-risk fractures

Not all stress fractures behave the same way. The single most important factor is where the fracture is. Low-risk fractures sit on the compression side of bone and heal reliably with activity modification. High-risk fractures lie in zones of tension or poor blood supply and are prone to delayed union, nonunion, or progression to a complete fracture — so they need protection from weight-bearing and, at times, surgery.

Low-risk sites

Posteromedial distal tibia — the most common running stress fracture. Pain appears toward the end of activity and doesn’t settle with brief rest. X-rays are normal early, then show cortical changes and periosteal reaction after two to three weeks (graded on MRI by the Fredericson system). Treatment is rest and avoidance of impact loading.

Calcaneus (heel) — posterior plantar heel pain, often with a 7–10 day prodrome, and tenderness on squeezing the heel from both sides (side-to-side squeeze test) rather than underneath as in plantar fasciitis. Changes appear on X-ray at 10–14 days, clearer by six weeks; bone scan lights up as early as 2–8 days. Usually treated with a short-leg cast for two to four weeks, with return to sport around eight weeks once tenderness resolves.

Metatarsal shafts (1st–4th) — the classic march fracture, making up roughly 14–20% of lower-limb stress fractures, most often the second (about 52%) and third (about 35%) metatarsals. Symptoms come on quickly, within two to six weeks, sometimes after a single hard training session. Activity restriction is the key to treatment.

Distal fibula — typically 1.5–3 inches above the tip, thought to result from excessive hindfoot eversion causing subfibular impingement. Sudden diffuse pain and swelling within about ten days of a training change; a characteristic transverse fracture appears at three to four weeks. Nearly always treated non-operatively, with improvement inside six weeks.

Cuboid and cuneiforms — both very rare; MRI is recommended for diagnosis, and treatment is almost always non-operative.

High-risk sites

Anterior tibial cortex — the tension side of the bone. A fracture line here (the ominous “dreaded black line”) signals a real risk of delayed union or complete fracture. A trial of non-operative care is reasonable, but if there is no improvement four to six months after diagnosis, surgery — curettage and bone grafting with plate fixation, or intramedullary nailing — is needed, with union taking about five months on average.

Tarsal navicular — the central third has a relatively poor blood supply, and that is exactly where these fractures occur. They happen in athletes doing explosive push-off and cutting, symptoms are vague, and diagnosis is commonly delayed by four to seven months. CT is the best imaging study. Non-displaced fractures are treated with 6–8 weeks of non-weight-bearing cast immobilization (total recovery 6–8 months); displaced or sclerotic complete fractures require surgery.

Medial malleolus — from repetitive ankle dorsiflexion and rotation in runners and jumpers; often insidious and sometimes found only in delayed union months later. Early cases are treated with a cast to limit dorsiflexion, activity resuming after two to three months (union averaging about nine months). Incomplete fractures may need percutaneous screw fixation; complete vertical fractures an antiglide plate.

Proximal fifth metatarsal — lateral foot pain and tenderness, classified by chronicity (Torg). Zone 2–3 fractures are often treated with four weeks of non-weight-bearing cast then four weeks weight-bearing, but many athletes are managed surgically with an intramedullary screw for a more reliable, faster return.

Sesamoids (under the big toe) — pain during activity or climbing stairs; must be distinguished from a bipartite sesamoid. Treated first with a toe-spica cast and orthotics; surgery (partial or complete excision, sometimes bone grafting) is reserved for cases failing six or more months of conservative care.

Talus — very rare and without a firmly established protocol; treatment usually begins with six weeks of non-weight-bearing immobilization.

How stress fractures are treated

For fractures seen only on bone scan or MRI — with no fracture line on plain films — about six to eight weeks of activity restriction is usually enough, and even clearly visible low-risk fractures can start with non-operative care. Most stress fractures heal in four to fifteen weeks. Activity restriction is the foundation; pain relievers or NSAIDs may help, and 7–10 days of protected weight-bearing is used if daily activities are difficult. Once the patient can manage daily life and the focal tenderness has gone, activity is increased gradually. Cycling and pool work keep fitness during this time.

High-risk fractures are approached more aggressively from the start, with strict protection, close imaging follow-up, and a lower threshold for screw or plate fixation. Whatever the site, I also look for the reason the bone failed — training errors, footwear, alignment, vitamin D, bone density, and, in female athletes, energy availability and menstrual history. Treating the fracture without correcting the cause invites the next one.

When can I run again?

Most low-risk stress fractures allow a return to running in roughly six to twelve weeks, following a graduated program once walking is pain-free. High-risk sites take longer — navicular, anterior tibial, and medial malleolar fractures often need several months to well over half a year, whether treated in a cast or with surgery. Returning too early is the most common reason for recurrence, so the schedule is set by healing on examination and imaging, not by the calendar alone.

Preventing the next one

Increase training load gradually, replace worn running shoes, maintain adequate calcium and vitamin D, ensure you are eating enough for your training volume, and take new, persistent, focal bone pain seriously. A stress fracture caught at the bone-edema stage may cost you weeks; one ignored until it becomes a complete fracture — particularly at a high-risk site — can cost a season, or require surgery.

This article is for general education and is not a substitute for individual medical advice.

One response

  1. […] If you’d like to read more on this topic, see the companion article: Stress Fractures of the Lower Leg and Foot: From Tibia to Toe. […]

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