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Also known as: lead sulfate
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anglesite, naturally occurring lead sulfate (PbSO4). A common secondary mineral that is a minor ore of lead, it is usually formed by the oxidation of galena and often forms a concentrically banded mass surrounding a core of unaltered galena. The formation of cerussite (lead carbonate) often accompanies or follows the formation of anglesite. For detailed physical properties, see sulfate mineral (table).

This article was most recently revised and updated by Amy Tikkanen.