A wide variety of calcifications may develop in the urinary tract. Cal
culi, the most common form of urinary tract calcification, are usually
radiopaque due to their calcium content, whereas cystine stones tend
to be less opaque. In cortical nephrocalcinosis, calcification may be
spotty or may appear as a thin rim outlining the cortex. Intracystic c
alcification is usually thin and peripheral and is often described as
having an ''eggshell'' appearance. In renal masses, pure central calci
fication usually indicates malignancy, although malignancy may also be
present with pure peripheral calcification. An incomplete ring of cal
cification seen over the central portion of the kidney should suggest
the presence of an abnormal vascular structure. A sloughed papilla may
lead to calcification that is usually triangular or ring-shaped or ha
s a broken rim pattern. Ureteral calculi usually have a uniform radiop
acity, whereas phleboliths are often less opaque centrally. Like renal
calculi, bladder calculi usually contain a calcium component; they ma
y be laminated, faceted, spiculated, or seedlike in appearance. Uracha
l carcinoma is commonly associated with tumor calcification, which typ
ically occurs at the dome of the bladder. Schistosomiasis of the bladd
er may produce mural calcification with a typical thin arcuate pattern
and may be associated with calcification in other portions of the uri
nary tract. Although urinary tract calcifications may be difficult to
characterize specifically, they can be classified according to locatio
n, appearance, and relation to various pathologic conditions.