Phlebolith

Last revised by Francis Fortin on 27 Nov 2023

Phleboliths are literally "vein stones", and represent calcification within venous structures. They are particularly common in the pelvis, where they may mimic ureteric calculi, and are also encountered frequently in venous malformations. They can also be seen in spindle-cell hemangiomas and occasionally in macrocystic lymphatic malformations after they've bled. 

Phleboliths appear as focal calcifications, often with radiolucent centers (if present, a helpful sign to distinguish them from urolithiasis). This appearance is attributed to calcification peripherally within the vessel and is frequently seen on abdominal radiographs (66% of phleboliths 2). It can also be seen on CT provided thin sections are obtained (at 5 mm thick slices, radiolucent centers will be inapparent in 99% of phleboliths 2).

The word phlebolith is derived from the Ancient Greek words, φλεψ (phleps) meaning vein, and λιθος (lithos) meaning stone or rock 3.

Two signs are helpful in distinguishing a ureteric calculus from a phlebolith:

  1. comet tail sign: favors a phlebolith

  2. soft tissue rim sign: favors a ureteric calculus

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