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cerussite

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cerussite (sēr`əsīt), colorless to white or gray mineral, sometimes yellowish or greenish, transparent to opaque, very brittle, crystallizing in the orthorhombic system and occurring also in granular and massive form. It is a carbonate of lead, PbCO3, formed by the action of carbonate and bicarbonate solutions on galena galena (gəlē`nə) or lead glance,
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. It is an important ore of lead widely distributed throughout the world and found associated with galena and other lead minerals.

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Within the oxidized zones, the primary sulfide minerals were commonly converted to limonite, pyrolusite, cerussite, anglesite, argentojarosite and plumbojarosite (basic sulfates of Fe), and native silver, with traces of malachite and azurite.
Examination and sampling of the Esmeralda Lead Manto stopes has revealed that the host rock for the cerussite mineralization is a high iron oxide rock containing oxide zinc mineralization similar to the Iron Oxide Manto and that the stope back-fill contains oxide zinc mineralization.
 
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