CMFs are extremely rare benign cartilaginous bone neoplasms that were initially described by Jaffe and Lichtenstein in 1948 (
10). There is no gender predilection, but in some of the published case series, higher numbers of males have been reported. It usually occurs in the second or third decades and the majority appears before the age of 30 years. Most of the CMFs are located in the metaphyseal region of the long bones. One third of them forms in the tibia, small tubular bones of foot, and the distal femur and pelvis (
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12). CMFs in the vertebral columns are rare, especially in the cervical region and related soft tissue vicinity. Lopez et al. reported CMF of the cervical spine in a 20-year-old man with neck pain that was located in the body of the C2 vertebra. X-ray showed a lytic lesion in the C2 body that causes instability of the craniocervical vertebra without extension into the soft tissue (
5). Our case was an adult female who had suffered from a long history of neck pain and there was an imperceptible lump on an x-ray in the right paravertebral soft tissue. Although the radiological findings were not diagnostic for CMF, it originated from the lamina and spinous processes of the cervical bones and extended into the adjacent soft tissue. Spinal CMF was first reported by Benson and Bass (
1). Radiological features are not characteristic, but may present as a lobulated, eccentric radiolucent lesion with no periosteal reaction, and in all of the patients, geographic bone destruction is visible. The margin of the CMF is sclerotic, and defined with pseudotrabeculation in 57% of the cases, and matrix calcification is seen in about 12.5% of the cases (
11). MRI features of CMF of vertebral column are not specific, but the helpful features are the peripheral intermediate signal band, central high signal intensity on T2-WI, and peripheral nodular enhancement or central non-enhancing focus on contrast-enhanced T1-WI (
12). In addition, a doughnut sign is seen in bone scans of CMFs; however, this is a non-specific finding because it may be found in other bone tumors (
11,
12). Other benign tumors, such as aneurysmal bone cyst, giant cell tumor, enchondroma, non-ossifying fibroma and chondroblastoma could be listed in the differential diagnoses. In long bones, CMF originates from the metaphysis close to the physis, and it may also extend into the epiphysis or diaphysis. Furthermore, it usually appears as an eccentric, oval shape lesion. In small bones, a CMF may involve the diaphysis, metaphysis, and epiphysis (
1). The preferred imaging study is conventional radiography with its specific characteristics composed of a bubbly cystic appearance, but a computed tomography (CT) scan displays a sclerotic calcification margin and trabeculation better than conventional radiography (
11). In our case, a plain X-ray showed a barely discernible ill-defined soft-tissue density within the deep soft tissues of the posterior aspect of the C3 and C4 vertebrae just posterior to the related spinous process without characteristic features of CMF in the vertebral bones. CMFs have different tissue components with a heterogeneous appearance on MRI studies. For example, chondroid and myxoid tissues create an intermediate to high signal on proton-density and T2-WI or low signal on T1-WI (
12). CMFs show a high accumulation of fluorodeoxyglucose in positron emission tomography (PET) scan, but we did not perform this study for our patient. The most common site of vertebral column involvement by CMF is in the thoracic region, with a predilection for the posterior neural arc (
4). Chondrosarcoma, osteoblastoma, aneurysmal bone cyst, giant cell tumor of the bone, metastasis, multiple myeloma, and collapsed hemangioma of the vertebral bodies are the most common differential diagnoses in radiological investigations. Jonathan et al. reported CMF in the seventh cervical vertebra of a 35-year-old man, in whom X-ray, MRI and bone scans, suggested an aneurysmal bone cyst or a giant cell tumor (
1). Two adjacent vertebral bone involvements, especially in the cervical vertebrae have not been reported yet. Bruder et al. reported a case of CMF in two thoracic vertebrae that originated from vertebral bodies, but our case was CMF in two cervical vertebrae with involvement of the laminas and spinous processes (
13). The symptoms of this benign tumor seem to be progressive longstanding pain, swelling, and motion restriction of the affected limb (
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8). Histopathologically, the tumor is composed of chondroid, myxoid, and fibrous connective tissue, which are arranged in a lobular pattern. Scattered osteoclast-like multinucleated giant cells are occasionally seen inside the tumor, especially at the periphery. Areas of calcification are also present in some cases. Mitotic figures are rare or absent (
10). The main differential diagnosis of CMF from chondrosarcoma histologically is the sharp borders of the lobules and also radiologic studies which could help to make the correct diagnosis (
11). En bloc excision of the tumor is the treatment of choice, but recurrences after curettage have been reported. Our case has not had any recurrence after the excision.
Although CMF is a rare benign bone tumor, involvement of the vertebral column especially the cervical vertebrae is very rare, but we listed it in the differential diagnosis despite the unusual soft tissue extension. Conventional radiology with MRI and PET scan could give us better diagnostic information.