Search results
Results from the WOW.Com Content Network
Le Fort's fracture of the ankle is a vertical fracture of the antero-medial part of the distal fibula with avulsion of the anterior tibiofibular ligament, [1] opposite to a Tillaux-Chaput avulsion fracture. The injury was described by Léon Clément Le Fort in 1886. [2]
An avulsion fracture is a bone fracture which occurs when a fragment of bone tears away from the main mass of bone as a result of physical trauma. This can occur at the ligament by the application of forces external to the body (such as a fall or pull) or at the tendon by a muscular contraction that is stronger than the forces holding the bone ...
posterior dislocation of hip with avulsion fracture of fragment of femoral head by the ligamentum teres: impact to the knee with the hip flexed (dashboard injury) Type II-V: Posterior Fracture Dislocations at Wheeless' Textbook of Orthopaedics online Pott's fracture [4] Percival Pott: bimalleolar fracture of the ankle: eversion of ankle
Ankle fractures may result from excessive stress on the joint such as from rolling an ankle or from blunt trauma. [1] [2] Types of ankle fractures include lateral malleolus, medial malleolus, posterior malleolus, bimalleolar, and trimalleolar fractures. [1] The Ottawa ankle rule can help determine the need for X-rays. [2]
Talofibular ligament sprain or distal fibular avulsion fracture; Vertical medial malleolus fracture and impaction of anteromedial distal tibia; Supination-External rotation: Anterior tibiofibular ligament sprain; Lateral short oblique fibular fracture (anteroinferior to posterosuperior) Posterior tibiofibular ligament rupture or avulsion of ...
A Tillaux fracture is a Salter–Harris type III fracture through the anterolateral aspect of the distal tibial epiphysis. [1] It occurs in older adolescents between the ages of 12 and 15 when the medial epiphysis had closed but before the lateral side has done so, [2] due to an avulsion of the anterior inferior tibiofibular ligament, at the opposite end to a Wagstaffe-Le Fort avulsion fracture
In geology, accretion is a process by which material is added to a tectonic plate at a subduction zone, frequently on the edge of existing continental landmasses. The added material may be sediment, volcanic arcs , seamounts , oceanic crust or other igneous features.
fracture front – the line separating the rock that has been fractured from the rock that has not; fracture tip – the point at which the fracture trace terminates on the surface; fracture trace – the line representing the intersection of the fracture plane with the surface; Griffith cracks – preexisting microfractures and flaws in the rock