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Covellite
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{{Short description|Sulfide mineral}} {{Infobox mineral | name = Covellite | category = [[Sulfide mineral]] | boxwidth = | boxbgcolor = | image = Covellite-252597.jpg | imagesize = 260px | caption = | formula = CuS ([[copper monosulfide]]) | IMAsymbol = Cv<ref>{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}</ref> | molweight = | strunz = 2.CA.05a | dana = 02.08.12.01 | system = [[Hexagonal crystal system|Hexagonal]] | class = Dihexagonal dipyramidal (6/mmm) <br/>[[H–M Symbol]] (6/m 2/m 2/m) | symmetry = ''P''6<sub>3</sub>/mmc | unit cell = a = 3.7938 Å, c = 16.341 Å; Z = 6 | color = Indigo-blue or darker, commonly highly iridescent, brass-yellow to deep red | habit = Thin platy hexagonal crystals and rosettes also massive to granular. | twinning = | cleavage = Perfect on {0001} | fracture = | tenacity = Flexible | mohs = 1.5–2 | luster = Submetallic, inclining to resinous to dull | refractive = n<sub>ω</sub> = 1.450 n<sub>ε</sub> = 2.620 | opticalprop = Uniaxial (+) | birefringence = | pleochroism = Marked, deep blue to pale blue | streak = Lead gray | gravity = 4.6–4.8 | melt = | fusibility = 2.5 | diagnostic = | solubility = | diaphaneity = Opaque | other = Micaceous cleavage | references = <ref name=Handbook>[http://rruff.geo.arizona.edu/doclib/hom/covellite.pdf Handbook of Mineralogy]</ref><ref name=Webmin>[http://webmineral.com/data/Covellite.shtml Webmineral data]</ref><ref name=Mindat>[http://www.mindat.org/min-1144.html Mindat.org]</ref> }} [[Image:Cp--Covellite.jpg|thumb|Covellite (gray) replacing and embaying chalcopyrite (light), polished section from Horn Silver Mine, San Francisco Mining District, [[Utah]]. Enlarged to 210 diameters. |alt=]] '''Covellite''' (also known as '''covelline''') is a rare [[copper sulfide]] mineral with the [[chemical formula|formula]] CuS.<ref name="Mindat" /> This indigo blue [[mineral]] is commonly a secondary mineral in limited abundance and although it is not an important ore of copper itself, it is well known to mineral collectors.<ref name="Mindat" /> The mineral is generally found in zones of secondary enrichment ([[Supergene (geology)|supergene]]) of copper sulfide deposits. Commonly found as coatings on [[chalcocite]], [[chalcopyrite]], [[bornite]], [[enargite]], [[pyrite]], and other sulfides, it often occurs as pseudomorphic replacements of other minerals.<ref>{{Cite book|title=Chlorine Compounds-Advances in Research and Application|last=Q. Ashton Acton|date=2012|publisher=ScholarlyMedia LLC|isbn=9781481600040|oclc=1024280169}}</ref> The first records are from [[Mount Vesuvius]], formally named in 1832 after N. Covelli.<ref name=Mindat/>
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