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About: Cotunnite     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Whole105869584, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingdul:ChemicalObjectchemical substanceMineralmineralyago:WikicatChloridesyago:WikicatLeadCompoundsyago:WikicatLeadMineralsyago:WikicatMetalHalidesyago:WikicatMineralsyago:WikicatOrthorhombicMineralsyago:Abstraction100002137yago:Chemical114806838yago:Chloride115017604yago:Cognition100023271yago:Compound105870180yago:Compound114818238yago:Concept105835747yago:Content105809192yago:Halide114904359yago:Idea105833840yago:Material114580897yago:Matter100020827yago:Mineral114662574yago:Part113809207yago:PhysicalEntity100001930yago:PsychologicalFeature100023100yago:Relation100031921yago:WikicatHalideMineralsyago:Salt115010703yago:Substance100019613yago:Whole105869584 New Facet based on Instances of this Class

Cotunnite is the natural mineral form of lead(II) chloride with formula PbCl2. It was first described in 1825 from an occurrence on Mount Vesuvius, Naples Province, Campania, Italy. It was named for Domenico Cotugno (Cotunnius) (1736–1822), Italian physician and Professor of Anatomy. It was first recognized in volcanic fumarole deposits. It occurs as a secondary alteration product in lead ore deposits. It has also been reported as an alteration of archaeological objects that contain lead.