Diastatic fractures occur when the fracture line transverses

one or more sutures of the skull causing a widening of the suture. While this type of fracture is usually seen in infants and young children as the sutures are not yet fused it can also occur in adults. When a diastatic fracture occurs in adults it usually affects the lambdoidal suture as this suture does not fully fuse in adults until about the age of 60.

Diastatic fractures can occur with different types of fractures and it is also possible for diastasis of the cranial sutures to occur without a concomitant fracture. Sutural diastasis may also occur in various congenital disorders such as cleidocranial dysplasia and osteogenesis imperfecta.

Basilar skull fractures are linear fractures that occur in the floor of the cranial vault (skull base), which require more force to cause than other areas of the neurocranium. Thus they are rare, occurring as the only fracture in only 4% of severe head injury patients.

Basilar fractures have characteristic signs: blood in the sinuses; a clear fluid called cerebrospinal fluid (CSF) leaking from the nose (rhinorrhea) or ears (otorrhea); periorbital ecchymosis often called 'raccoon eyes' (bruising of the orbits of the eyes that result from blood collecting there as it leaks from the fracture site); and retroauricular ecchymosis known as "Battle's sign" (bruising over the mastoid process).

A basilar skull fracture is a break of a bone in the base of the skull. Symptoms may include bruising behind the ears, bruising around the eyes, or blood behind the ear drum. A cerebrospinal fluid (CSF) leak occurs in about 20% of cases and can result in fluid leaking from the nose or ear. Meningitis is a complication in about 14% of cases. Other complications include cranial nerve or blood vessel injury.

They typically require a significant degree of trauma to occur. The break is of at least one of the following bones: temporal bone, occipital bone, sphenoid bone, frontal bone, or ethmoid bone. They are divided into anterior fossa, middle fossa, and poterior fossa fractures. Facial fractures often also occur. Diagnosis is typically by CT scan.

Treatment is generally based on the injury to structures inside the head. Surgery may be done for a CSF leak that does not stop or an injury to a blood vessel or nerve. Preventative antibiotics are of unclear use. It occurs in about 12% of people with a severe head injury.

Individuals with Jefferson fractures usually experience pain in the upper neck but no neurological signs. The fracture may also cause damage to the arteries in the neck, resulting in lateral medullary syndrome, Horner's syndrome, ataxia, and the inability to sense pain or temperature.

In rare cases, congenital abnormality may cause the same symptoms as a Jefferson fracture.

In orthopedic medicine, fractures are classified in various ways. Historically they are named after the physician who first described the fracture conditions, however, there are more systematic classifications in place currently.

Basilar skull fractures include breaks in the posterior skull base or anterior skull base. The former involve the occipital bone, temporal bone, and portions of the sphenoid bone; the latter, superior portions of the sphenoid and ethmoid bones. The temporal bone fracture is encountered in 75% of all basilar skull fractures and may be longitudinal, transverse or mixed, depending on the course of the fracture line in relation to the longitudinal axis of the pyramid.

Bones may be broken around the foramen magnum, the hole in the base of the skull through which the brain stem exits and becomes the spinal cord, creating the risk that blood vessels and nerves exiting the hole may be damaged.

Due to the proximity of the cranial nerves, injury to those nerves may occur. This can cause of the facial nerve or oculomotor nerve or hearing loss due to damage of cranial nerve VIII.

Even though symptoms vary widely after experiencing a bone fracture, the most common fracture symptoms include:

- pain in the fractured area

- swelling in the fractured area

- obvious deformity in the fractured area

- not being able to use or move the fractured area in a normal manner

- bruising, warmth, or redness in the fractured area

Pediatric fractures can be classified as complete and incomplete:

- Incomplete: there are three basic forms of incomplete fractures:

- The first is the greenstick fracture, a transverse fracture of the cortex which extends into the midportion of the bone and becomes oriented along the longitudinal axis of the bone without disrupting the opposite cortex.

- The second form is a torus or buckling fracture, caused by impaction. They are usually the result of a force acting on the longitudinal axis of the bone: they are typically a consequence of a fall on an outstretched arm, so they mainly involve the distal radial metaphysis. The word torus is derived from the Latin word 'torus,' meaning swelling or protuberance.

- The third is a bow fracture in which the bone becomes curved along its longitudinal axis.

- Complete fractures

There are also physeal fractures (fractures involving the physis, the growth plate, which is not present in adults). The Salter-Harris classification is the most used to describe these fractures.

A "corner fracture" or "bucket-handle fracture" is fragmentation of the distal end of one or both femurs, with the loose piece appearing at the bone margins as an osseous density paralleling the metaphysis. The term "bucket-handle fracture" is used where the loose bone is rather wide at the distal end, making it end in a crescent shape. These types of fractures are characteristic of child abuse-related injuries.

Although bone tissue itself contains no nociceptors, bone fracture is painful for several reasons:

- Breaking in the continuity of the periosteum, with or without similar discontinuity in endosteum, as both contain multiple pain receptors

- Edema of nearby soft tissues caused by bleeding of torn periosteal blood vessels evokes pressure pain

- Muscle spasms trying to hold bone fragments in place. Sometimes also followed by cramping

Damage to adjacent structures such as nerves or vessels, spinal cord, and nerve roots (for spine fractures), or cranial contents (for skull fractures) may cause other specific signs and symptoms.

A Jefferson fracture is a bone fracture of the anterior and posterior arches of the C1 vertebra, though it may also appear as a three- or two-part fracture. The fracture may result from an axial load on the back of the head or hyperextension of the neck (e.g. caused by diving), causing a posterior break, and may be accompanied by a break in other parts of the cervical spine.

It is named after the British neurologist and neurosurgeon Sir Geoffrey Jefferson, who reported four cases of the fracture in 1920 in addition to reviewing cases that had been reported previously.

This type of fractured mandible can involve one condyle (unilateral) or both (bilateral). Unilateral condylar fracture may cause restricted and painful jaw movement. There may be swelling over the temporomandibular joint region and bleeding from the ear because of lacerations to the external auditory meatus. The hematoma may spread downwards and backwards behind the ear, which may be confused with Battle's sign (a sign of a base of skull fracture), although this is an uncommon finding so if present, intra-cranial injury must be ruled out. If the bones fracture and overlie each other there may be shortening of the height of the ramus. This results in gagging of the teeth on the fractured side (the teeth meet too soon on the fractured side, and not on the non fractured side, i.e. "open bite" that becomes progressively worse to the unaffected side). When the mouth is opened, there may be deviation of the mandible towards the fractured side. Bilateral condylar fractures may cause the above signs and symptoms, but on both sides. Malocclusion and restricted jaw movement are usually more severe. Bilateral body or parasymphysis fractures are sometimes termed "flail mandible", and can cause involuntary posterior movement of the tongue with subsequent obstruction of the upper airway. Displacement of the condyle through the roof of glenoid fossa and into the middle cranial fossa is rare. Bilateral condylar fractures combined with a symphyseal fracture is sometimes termed a guardsman's fracture. The name comes from this injury occurring in soldiers who faint on parade grounds and strike the floor with their chin.

Some clinical features of a greenstick fracture are similar to those of a standard long bone fracture - greenstick fractures normally cause pain at the injured area. As these fractures are specifically a pediatric problem, an older child will be protective of the fractured part and babies may cry inconsolably. As per a standard fracture, the area may be swollen and either red or bruised. Greenstick fractures are stable fractures as a part of the bone remains intact and unbroken so this type of fracture normally causes a bend to the injured part, rather than a distinct deformity, which is problematic.

By far, the two most common symptoms described are pain and the feeling that teeth no longer correctly meet (traumatic malocclusion, or disocclusion). The teeth are very sensitive to pressure (proprioception), so even a small change in the location of the teeth will generate this sensation. People will also be very sensitive to touching the area of the jaw that is broken, or in the case of condylar fracture the area just in front of the tragus of the ear.

Other symptoms may include loose teeth (teeth on either side of the fracture will feel loose because the fracture is mobile), numbness (because the inferior alveolar nerve runs along the jaw and can be compressed by a fracture) and trismus (difficulty opening the mouth).

Outside the mouth, signs of swelling, bruising and deformity can all be seen. Condylar fractures are deep, so it is rare to see significant swelling although, the trauma can cause fracture of the bone on the anterior aspect of the external auditory meatus so bruising or bleeding can sometimes be seen in the ear canal. Mouth opening can be diminished (less than 3 cm). There can be numbness or altered sensation (anesthesia/paraesthesia in the chin and lower lip (the distribution of the mental nerve).

Intraorally, if the fracture occurs in the tooth bearing area, a step may seen between the teeth on either side of the fracture or a space can be seen (often mistaken for a lost tooth) and bleeding from the gingiva in the area. There can be an open bite where the lower teeth, no longer meet the upper teeth. In the case of a unilateral condylar fracture the back teeth on the side of the fracture will meet and the open bite will get progressively greater towards the other side of the mouth.

Sometimes bruising will develop in the floor of the mouth (sublingual eccymosis) and the fracture can be moved by moving either side of the fracture segment up and down. For fractures that occur in the non-tooth bearing area (condyle, ramus, and sometimes the angle) an open bite is an important clinical feature since little else, other than swelling, may be apparent.

The term "Colles fracture" is classically used to describe a fracture at the distal end of the radius, at its cortico-cancellous junction. However, now the term tends to be used loosely to describe any fracture of the distal radius, with or without involvement of the ulna, that has dorsal displacement of the fracture fragments. Colles himself described it as a fracture that “takes place at about an inch and a half (38mm) above the carpal extremity of the radius” and “the carpus and the base of metacarpus appears to be thrown backward”. The fracture is sometimes referred to as a "dinner fork" or "bayonet" deformity due to the shape of the resultant forearm.

Colles' fractures can be categorized according to several systems including Frykman, Gartland & Werley, Lidström, Nissen-Lie and the Older's classifications.

Triplane fracture is a fracture at the epiphyseal plate of the tibia in early adolescence with involvement of the epiphysis and metaphysis of the tibia. The link presents two types of imaging. The first four images (figures 1-4) are radiographic images while the last 3 are CT scans of the left distal tibia and fibula. The first radiographic image is an anterior-posterior view of the distal third of the left tibia and fibula. The image presents a fracture of the distal epiphyseal plate of the tibia and fibula. The primary imaging (radiograph) identifies the abnormality in the anatomy of subject’s left distal tibia and fibula. However, it is difficult to view the extent of the fracture and classify the fracture based on radiographic image. Figure four is a CT scan of the posterior aspect of the left distal tibia and fibula. Note that in this image the extent of the fracture is more visible extending to the epiphysis and metaphysis. The type of fracture is a Salter-Harris type IV. The CT scan was an appropriate choice of advance imaging which helps clinicians determine the extent of the fracture and enable us to address the problem appropriately.

There are nine types of Salter–Harris fractures; types I to V as described by Robert B Salter and W Robert Harris in 1963, and the rarer types VI to IX which have been added subsequently:

- Type I – transverse fracture through the growth plate (also referred to as the "physis"): 6% incidence

- Type II – A fracture through the growth plate and the metaphysis, sparing the epiphysis: 75% incidence, takes approximately 2–3 weeks or more in the spine to heal.

- Type III – A fracture through growth plate and epiphysis, sparing the metaphysis: 8% incidence

- Type IV – A fracture through all three elements of the bone, the growth plate, metaphysis, and epiphysis: 10% incidence

- Type V – A compression fracture of the growth plate (resulting in a decrease in the perceived space between the epiphysis and metaphysis on x-ray): 1% incidence

- Type VI – Injury to the peripheral portion of the physis and a resultant bony bridge formation which may produce an angular deformity (added in 1969 by Mercer Rang)

- Type VII – Isolated injury of the epiphyseal plate (VII–IX added in 1982 by JA Ogden)

- Type VIII – Isolated injury of the metaphysis with possible impairment of endochondral ossification

- Type IX – Injury of the periosteum which may impair intramembranous ossification

A Smith Fracture is a named vertebral fracture occurring most commonly in the lumbar spine. It is similar to that of a Chance fracture and is associated with seat belt injuries. This fracture represents a fracture through the posterior elements including the superior articular processes but not the spinous process, as well as an avulsion fracture of the vertebral body. This fracture is not to be confused with the more commonly referred to Smith's fracture of the wrist.

A Tillaux fracture (or a Tillaux-Chaput avulsion fracture) is a Salter–Harris type III fracture through the anterolateral aspect of the distal tibial epiphysis. 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, due to an avulsion of the anterior tibiofibular ligament, at the opposite end to a Wagstaffe-Le Fort avulsion fracture

The fracture is most commonly caused by people falling onto a hard surface and breaking their fall with outstretched hand (FOOSH)–falling with wrists flexed would lead to a Smith's fracture. Originally it was described in elderly and/or post-menopausal women. It usually occurs about three to five centimetres proximal to the radio-carpal joint with posterior and lateral displacement of the distal fragment resulting in the characteristic "dinner fork" or "bayonet" like deformity. Colles fracture is a common fracture in people with osteoporosis, second only to vertebral fractures.

The fracture commonly results from an abduction-external rotation force, causing the anterior tibiofibular ligament to avulse the anterolateral corner of the distal tibial epiphysis resulting in a Salter Harris Type III fracture.

A Salter–Harris fracture is a fracture that involves the epiphyseal plate or growth plate of a bone. It is a common injury found in children, occurring in 15% of childhood long bone fractures.

A Smith's fracture, also sometimes known as a reverse Colles' fracture or Goyrand-Smith's, is a fracture of the distal radius. It is caused by a direct blow to the dorsal forearm or falling onto flexed wrists, as opposed to a Colles' fracture which occurs as a result of falling onto wrists in extension. Smith's fractures are less common than Colles' fractures.

The distal fracture fragment is displaced volarly (ventrally), as opposed to a Colles' fracture which the fragment is displaced dorsally. Depending on the severity of the impact, there may be one or many fragments and it may or may not involve the articular surface of the wrist joint.

Signs and symptoms include crepitus (a crunching sound made when broken bone ends rub together), pain, tenderness, bruising, and swelling over the fracture site. The fracture may visibly move when the person breathes, and it may be bent or deformed, potentially forming a "step" at the junction of the broken bone ends that is detectable by palpation. Associated injuries such as those to the heart may cause symptoms such as abnormalities seen on electrocardiograms.

The upper and middle parts of the sternum are those most likely to fracture, but most sternal fractures occur below the sternal angle.

This fracture is named after the orthopedic surgeon, Robert William Smith (1807–1873) in his book "A Treatise on Fractures in the Vicinity of Joints, and on certain forms of Accidents and Congenital Dislocations" published in 1847.