It is often associated with the minerals anglesite and celestine. Carminite also occurs as masses mixed with cerussite, anglesite and plumbojarosite. Galena PbS (primary) alters to secondary anglesite PbSO and cerussite PbCO. Other associated minerals include mimetite, duftite, cerussite, anglesite and wulfenite. Original surface oxidized ore contained cerussite, anglesite and pyromorphite. An example is the lead mineral anglesite PbSO. Scotlandite is found in association with pyromorphite, anglesite, lanarkite, leadhillite, susannite, and barite. It occurs in association with brochantite, anglesite, caledonite, leadhillite, cerussite, malachite and hemimorphite. Frequently associated minerals include&colon; linarite, malachite, cerussite, brochantite, anglesite, leadhillite, and azurite. Leadhillite is a lead sulfate carbonate hydroxide mineral, often associated with anglesite. In upper levels, the ore minerals are oxidized to cerussite, anglesite, and smithsonite. An example is a change from galena (lead sulfide) to anglesite (lead sulfate). It occurs in association with galena, cerussite, anglesite and matlockite in the Caracoles, Chile. Anglesite, Cerussite, Pyromorphite, Mimetite and Wulfenite are other lead ores. It is also known as "fast white", "milk white", "sulfuric acid lead salt" or "anglesite".