It occurs in older children at the end of growth. Variability in fracture pattern is due to progression of physeal closure as anterolateral part of distal tibial physis is the last to close. When the lateral physis is the only portion not fused, external rotation may lead to<unk>  or Triplane fractures.
Tillaux fracture
Bosworth fracture
Smith fracture
Jefferson fracture
Rolando fracture
Duverney fracture
Hume fracture
Holdsworth fracture