Ureteral Stone
Also known as: Ureteric Calculus, Ureteric Colic
A ureteral stone is a calculus lodged in the ureter after migrating from the kidney, producing obstruction and renal colic. Lifetime risk is 10 to 15 percent in men and 5 to 10 percent in women. Incidence peaks at 20 to 50 years, and the recurrence rate is about 50 percent at 5 to 10 years.
Stones form in the kidney. When they enter the ureter they stop at the three physiological narrowings:
- The ureteropelvic junction.
- The pelvic brim, where the ureter crosses the iliac vessels.
- The ureterovesical junction (the narrowest part, 1 to 5 mm in diameter).
Stone composition:
- About 80 percent are calcium oxalate or calcium phosphate.
- 10 percent are uric acid.
- 5 to 10 percent are struvite.
- 1 to 2 percent are cystine.
Spontaneous passage depends on size:
- For stones of 4 mm or less, about 80 to 90 percent pass spontaneously.
- For 5 to 7 mm, about 50 to 60 percent.
- For above 8 mm, 20 to 30 percent or less.
Stones in the distal ureter pass more often than proximal ones. Passage typically takes up to 4 to 6 weeks.













