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Kidney Stones

Urinary Nephrolithiasis

Hard mineral pebbles that form in the kidney and cause severe pain when they block the drainage tube to the bladder.

Educational summary only — not medical advice, and no substitute for assessment by a clinician. Diagrams are simplified illustrations.

A stone wedged in the ureter dams the urine and stretches the kidney behind it — the source of the classic, crippling pain.
A stone wedged in the ureter dams the urine and stretches the kidney behind it — the source of the classic, crippling pain.

Overview

A kidney stone is a small, hard lump that forms when dissolved minerals in the urine become so concentrated that they crystallize and clump together. Many stones are tiny and pass unnoticed. The trouble — and the famously severe pain — begins when a stone large enough to get stuck travels out of the kidney and into the ureter, the thin muscular tube that carries urine to the bladder.

How the system normally works

Each kidney filters waste from the blood and produces urine, which collects in a funnel-shaped space (the renal pelvis) and drains down the ureter into the bladder. The ureter is only a few millimetres wide and pushes urine along with gentle squeezing waves. Because it is so narrow, even a small stone can plug it completely.

What goes wrong

When the urine is too concentrated — from not drinking enough, or from too much calcium, oxalate or uric acid — crystals form and grow into a stone. If that stone enters the ureter and lodges, urine can no longer drain. It backs up, stretching the ureter and the kidney behind it (a state called hydronephrosis). The ureter also squeezes hard in spasms trying to push the stone along. This stretching and spasm is what produces the intense, colicky pain.

Diagram of the urinary tract marking the three narrow points where kidney stones commonly get stuck: the ureteropelvic junction, the pelvic brim, and the entry into the bladder.
Stones tend to lodge at three natural narrowings of the ureter — the top (where the kidney narrows), the middle (crossing the pelvic brim), and the bottom (entering the bladder).

Symptoms and why they happen

Causes and risk factors

How it's diagnosed

A CT scan of the abdomen without contrast is the most accurate test and shows the stone's size and exact position; ultrasound is often used first, especially in pregnancy or to avoid radiation. Urine tests look for blood and infection, and blood tests check kidney function. The stone's size matters: small ones (under ~5 mm) usually pass on their own; larger ones often need help.

Diagram of shock-wave lithotripsy: focused sound waves from outside the body breaking a kidney stone into small fragments.
Shock-wave lithotripsy focuses sound waves through the skin to shatter a stone into sand-like fragments that can pass naturally.

Treatment and management

For a passing stone, the mainstays are pain relief, fluids, and time, sometimes with a medication that relaxes the ureter to ease the stone out. Stones that are too large, won't pass, or cause infection or blockage may be treated with shock-wave lithotripsy (breaking the stone with focused sound waves), ureteroscopy (a thin scope passed up to remove or laser the stone), or rarely keyhole surgery. A temporary stent may be placed to keep the ureter open.

Possible complications

A stone that fully blocks the kidney can damage it over time. The most dangerous combination is a blocked kidney plus infection, which can lead to a rapidly spreading, life-threatening infection requiring urgent drainage.

Prevention and outlook

Most people recover fully, but stones commonly recur. The single best prevention is drinking enough water to keep urine pale, alongside reducing salt, moderating animal protein, and following any diet tailored to the stone's mineral type. With good fluid habits, recurrence can be cut substantially.

When to seek emergency care