Staghorn Calculus
Also known as: Staghorn Stone
A staghorn calculus is a branching stone that fills the renal pelvis and extends into two or more calyces, taking the shape of the collecting system. A complete staghorn fills the entire pelvis and all calyces. A partial staghorn fills the pelvis and at least one calyx.
Most (about 75 percent) are struvite (magnesium ammonium phosphate with carbonate apatite) stones. They form in infected alkaline urine from urease producing organisms (Proteus mirabilis, Klebsiella, Pseudomonas, Providencia, Morganella, Staphylococcus saprophyticus, Ureaplasma, and Corynebacterium urealyticum).
About 25 percent are metabolic (cystine, uric acid, calcium oxalate or calcium phosphate, and brushite) and may become infected.
Urease splits urea to ammonia, which raises urinary pH above 7.2 and produces carbonate, driving crystallisation. Women are affected more than men (about 2:1).
Risk factors:
- Recurrent urinary tract infection.
- Urinary stasis (neurogenic bladder, spinal cord injury, ureteropelvic junction obstruction, urinary diversion).
- Indwelling catheters.
- Previous stone surgery.
Left untreated, the natural history is poor. 30 to 50 percent lose the kidney, and about 25 percent die of sepsis or renal failure within 10 years. Mortality is several fold higher than that of treated patients.













