It occurs naturally as the mineral cerussite. It occurs in association with brochantite, anglesite, caledonite, leadhillite, cerussite, malachite and hemimorphite. It occurs associated with smithsonite, hemimorphite, willemite, cerussite, aurichalcite, calcite and limonite. Associated minerals include bismutite, mica, jarosite, alunite, cerussite, atacamite, connellite. Carminite also occurs as masses mixed with cerussite, anglesite and plumbojarosite. It commonly occurs in association with hemimorphite, willemite, hydrozincite, cerussite, malachite, azurite, aurichalcite and anglesite. Original surface oxidized ore contained cerussite, anglesite and pyromorphite. This deposit contains cerussite and iron oxides. Associated minerals are descloizite, duftite, mimetite, wulfenite, cerussite, azurite and dioptase. Associated minerals include azurite, smithsonite, malachite, cerussite, mimetite, wulfenite and olivenite. Other associated minerals include mimetite, duftite, cerussite, anglesite and wulfenite. It occurs in the upper lead deposits through the oxidation of galena or cerussite. The main yields were lead and zinc ores, in particular galena, blende, cerussite and gossan. Common associates are wulfenite, scorodite, plumbojarosite, mimetite, dussertite, cerussite, beudantite, bayldonite, arseniosiderite and anglesite. This deposit consists of cerussite (lead carbonate) and smithsonite (zinc carbonate) ores.