Stress Fracture
A stress fracture results from repetitive loading that exceeds the capacity of bone to remodel and repair microdamage.
Pathophysiological classification
Fatigue fracture
Normal bone exposed to abnormal repetitive stress.
Typical patient:
- Runner
- Military recruit
- Athlete after sudden increase in training volume
Insufficiency fracture
Abnormal weakened bone exposed to normal physiological loading.
Causes include:
- Osteoporosis
- Osteomalacia
- Vitamin D deficiency
- Chronic corticosteroid exposure
- Metabolic bone disease
- Previous radiation
Classification by risk
The most clinically important classification divides stress fractures into low risk and high risk based on likelihood of displacement, delayed union and nonunion.
Low risk sites
Examples include:
- Posteromedial tibial cortex
- Fibula
- Calcaneus
- Second to fourth metatarsal shafts
- Many femoral shaft stress injuries
High risk sites
Examples include:
- Superolateral tension side femoral neck
- Anterior tibial cortex
- Tarsal navicular
- Proximal fifth metatarsal
- Medial malleolus
- Patella
High risk stress fractures require substantially more aggressive protection and sometimes prophylactic fixation.
Fredericson MRI classification
Originally developed for tibial stress injury but commonly used to describe increasing MRI severity.
Grade 1
- Periosteal oedema
- T1 normal
Grade 2
- Periosteal and marrow oedema visible on T2 weighted imaging
- T1 remains normal
Grade 3
- Marrow oedema visible on both T1 and T2 sequences
Grade 4
- Severe oedema with a visible cortical or intracortical fracture line
Some modified systems divide grade 4 into:
- 4a: severe cortical signal abnormality
- 4b: definite linear fracture line.

