In the gallbladder, gallstones are produced when elements in the bile produce hard, crystal-like particles. As their name suggests, cholesterol stones are formed of cholesterol and have a light hue. This process accounts for 80% of gallstone formation. Little, dark stones known as pigment stones are created from bilirubin and calcium salts that are present in bile. Pigment stones make up about 20% of gallstones. A golf ball-sized gallstone can be as little as a salt grain. One, frequently huge stone or many smaller ones may form in the gallbladder. It might even produce thousands of stones. Your stomach can become the path for gallstones that leave the gallbladder. The size of the stone or the structure of the biliary tree, however, could cause a stone to become trapped in your bile duct. Thus, gallbladder stones that have moved into the bile duct are known as bile duct stones. It can be painful and dangerous to have stones lodged in the ducts that lead to the duodenum.
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