Os vesalianum pedis (OVP) is one of the exquisite accessory ossicles adjacent to the foot's fifth metatarsal base. Though most of the OVP cases are asymptomatic, only a handful of patients who presented with lateral foot pain have been reported. A 36-year-old professional badminton player presented with swelling and tenderness in the right foot at the metatarsal base. An initial radiographic examination revealed a pseudo-Jones fracture. As a result of persistent pain and concerns regarding OVP, a reassessment of the X-ray was conducted. The examination revealed a radiolucent line with well-defined and well-corticated edges, uniformly separating the ossicle from the metatarsal in the right foot, consequently leading to the diagnosis of OVP. Following diagnosis, the patient was managed conservatively. Os vesalianum is not a common source of pain on the midfoot's lateral side. An oblique radiograph is an appreciable strategy to demonstrate the accessory ossicle. Thus, a careful clinical examination, coupled with the correlation of radiological findings, is a prerequisite to prevent misdiagnosis and overtreatment thereafter.

Lateroplantar foot pain may be caused by various entities, whereby painful os peroneum syndrome should be included in the differential diagnosis. Physical examination and multimodal imaging enable a definitive diagnosis. We report on a 59-year-old man with severe, load-dependent pain, corresponding to an os peroneum syndrome, triggered by a pes planovalgus with consecutively induced focal inflammation and tendovaginitis of the tendon of the peroneus longus muscle. Multifactorial conservative measures including infiltration and shockwave therapy finally led to a restoration of the original condition.

Accessory bones in the elbow region are rare anatomical variations with important clinical significance as they can be misdiagnosed as pathological lesions. Usually, they are asymptomatic and found incidentally during X-ray examination in the context of trauma. Although these bones have been previously described, their development is not fully understood. The present case provides complex macroscopic, X-ray and histological descriptions of a sesamoid bone in the posterior region of the elbow-patella cubiti and the related surrounding structures. Moreover, this report indicates the presence of a well-defined syndesmosis between patella cubiti and the proximal ulna.

Different anatomical variants can be found in the ankle and foot, generally as occasional findings, although they can be the cause of diagnostic pitfalls and difficulties, especially in radiographic interpretation in trauma. These variants include accessory bones, supernumerary sesamoid bones, and accessory muscles. In most cases, they represent developmental anomalies found in incidental radiographic findings. This review discusses the main bony anatomical variants, including accessory and sesamoid ossicles, most commonly found in the foot and ankle that can be a cause of diagnostic challenges.

The purpose of this article is to discuss most common diagnostic pitfalls of the lower limb with specific attention to the knee, ankle, and foot joints. The knowledge of normal anatomic variants, correlation with age, symptoms, and medical history together with these potential MR imaging pitfalls is fundamental for an accurate interpretation of the imaging findings of the lower limb.

This report described the management of a lady with a rare finding of a large size of Os intermetatarseum in a bizarre location. This unique condition resulted in a splay foot which was rarely discussed in the literature.

A lady in her early fifth decade has complained of foot swelling and difficulty wearing shoes for the last two years. Her main concern was the worry of a malignant condition.

She had an unusually huge articulated lump in the third web space. Also, it showed a central foot splay. A full battery of radiological investigation gave a narrow list of possible differential diagnoses. The final diagnosis showed that it was Os intermetatarseum. Surgical treatment involved enucleating the mass and correcting foot splay using a mini-tight rope®. The histopathology report confirmed the diagnosis of Os intermetatarseum. The central forefoot splay was treated by a known surgical tool differently. Post-operatively she was put on physical therapy. Five years follow-up showed improved foot anatomy and functional outcomes with no recurrence.

Awareness of this rare condition as a differential diagnosis. Complete excisional biopsy of the lump will be a valid option for this condition, as well as using a mini-tight rope® in dealing with central foot splay.

Accessory ossicles are well-corticated bony structures found close to bones or a joint. They may be unilateral or bilateral. The os tibiale externum is also known as accessory navicular bone, os naviculare secundarium, accessory (tarsal) scaphoid, or prehallux. It is found within the tibialis posterior tendon near its insertion on the navicular bone. The os peroneum is a small sesamoid bone located within the peroneus longus tendon, adjacent to the cuboid. We present a case series of five patients with accessory ossicles of the foot to demonstrate pitfalls in the diagnosis of foot and ankle pain.

The case series includes four patients with os tibiale externum and one patient with os peroneum. Only one patient had symptoms related to os tibiale externum. The accessory ossicle in the rest of the cases was discovered incidentally after trauma to the ankle or foot. The symptomatic os tibiale externum was managed conservatively with analgesics and shoe inserts for medial arch support.

Accessory ossicles are considered developmental anomalies and they originate from ossification centers that have failed to fuse with the main bone. Clinical suspicion and awareness about the existence of the commonly occurring accessory ossicles of the foot and ankle are necessary. They can be a confounding factor in the diagnosis of foot and ankle pain. Failure to notice their presence might result in a misdiagnosis and unnecessary immobilization or surgery for the patients.

The accessory bones are common bone variations around the feet and ankles, which usually originate from nonunion of the secondary ossification center adjacent to the main bone mass, and most of them remain asymptomatic. Os subcalcis is an accessory bone at the plantar aspect of the calcaneus, which is located just posterior to the insertion of the plantar fascia. Focal bone formation at the calcaneal plantar pole with heel pain has rarely been reported.

A 55-year-old man presented to our clinic with left plantar heel pain and a progressive swelling for 8 years. X-ray, computer tomography and magnetic resonance imaging showed a large os subcalcison the plantar side of the calcaneus, located at the insertion of the plantar fascia. He underwent surgical excision of the lesion. Microscopically the bony trabeculae were intermingled with fat and covered with cartilage.

This is a rare case with accessory os subcalcis leading to heel pain. It highlights the awareness of os subcalcis and helps avoid future misdiagnosis of heel pain.

The aim of the study was to examine the ligaments of the os trigonum.

The ankle joint magnetic resonance imaging (MRI) of 104 patients with the os trigonum (experimental group) and 104 patients without the os trigonum (control group) were re-reviewed. The connections of the os trigonum and posterior talofibular ligament (PTFL), the fibulotalocalcaneal ligament (FTCL), the paratenon of the Achilles tendon, the posterior talocalcaneal ligament (PTCL), the osteofibrous tunnel of the flexor hallucis longus (OF-FHL) and the flexor retinaculum (FR) were studied.

The os trigonum is connected to structures. The posterior part of the PTFL inserted on the os trigonum in 85.6% of patients, whereas in all patients in the control group, the posterior part of the PTFL inserted on the posterior talar process (p < 0.05). The connection of the PTCL was seen in 94.2% of patients in the experimental group, while it was seen in 90.4% of patients in the control group (p > 0.05). The connection to the FTCL in the experimental group was 89.4%, while in the control group, it was 91.3% (p > 0.05). The communication with the paratenon was seen more often in the control group compared to that in the experimental group (31.7% vs. 63.8%, p < 0.001). The FTCL was prolonged medially into the FR in 85.6% of patients in the experimental group and in 87.5% of patients in the control group (p > 0.05). The flexor hallucis longus (FHL) run at the level of articulation between the os trigonum 63.5% and the posterior process of the talus 25% and less often on the os trigonum 11.5%.

The os trigonum is connected with all posterior ankle structures and more connections than previously reported.

The os intermetatarseum is an uncommon accessory ossicle of the foot located dorsally, between the bases of the first and second metatarsals that are usually asymptomatic. In the setting of trauma, this ossicle can clinically mimic a Lisfranc fracture-dislocation, a potentially disabling condition often requiring surgical intervention.

In this study, 47 cases of os intermetatarseum were reviewed across several Western Australian (WA) Hospitals and characterised based on morphology. Any fractures were recorded, and their cases were reviewed.

The most common type of os intermetatarseum was freestanding at 63%, followed by the articulating type at 30%. Only 7% were of the fused type. Two acute fractures were identified on plain radiography and computed tomography (CT).

The distribution of os intermetatarseum subtypes in the WA population is consistent with previous radiological studies. The two cases of isolated acute os intermetatarseum fracture are described, the first to our knowledge, highlighting the need for increased awareness of this ossicle in the setting of foot trauma.

The study was conducted to search for confident radiological signs in symptomatic cases of accessory bones. A normal accessory bone appearance on X-ray does not exclude that the accessory bone is the source of the discomfort; because of this, MRI examination can later be applied as part of the diagnosis.

We retrospectively analysed cases of 64 patients with recognized 70 symptomatic accessory bones of the foot. The average age was 29.2 (range 8-42) years. We included only patients with X-ray and MRI examinations. We investigated the following radiological features of the bone (structural and signal) in relation to soft tissue.

The most constant symptoms identified in our study were bone marrow oedema (93%) and soft tissue oedema (77%). Changes in structures in which accessory bones were located or in adjacent structures to accessory bone were identified: tendon changes 51%, fluid adjacent to bone 51% and tenosynovitis 46%. MRI revealed changes in bone structure that are not seen on X-ray, including changes in contour (28%), sclerosis (3%) or osteonecrosis (3%).

MRI plays an important role in determining whether accessory bones cause symptoms because it shows specific and accurate changes in accessory bone and/or in adjacent soft tissue.

This paper presents some of the more commonly encountered non-metric traits and minor anatomical variants in the adult human skeleton that can mimic or be mistaken for trauma. Distinguishing non-metric traits is contingent upon both a knowledge of potential non-metric traits as well as the normal developmental timing, location, and anatomy of maturational markers in the human skeleton. Distinguishing non-metric traits from trauma in dry bone is an essential component in establishing an accurate and thorough forensic analysis of human remains, especially as it deals with antemortem and perimortem trauma, and postmortem damage.