Corkite
{{Short description|Phosphate mineral}}
{{Infobox mineral
| name = Corkite
| category = Phosphate minerals
| boxwidth = 24
| boxbgcolor =
| image = Corkite-Goethite.jpg
| caption = Corkite on a goethite matrix
| formula = PbFe3[(OH)6:SO4:PO4]
| molweight = 667.82 g/mol
| strunz = 8.BL.05
| dana = 43.4.1.2
| system = Trigonal
| class = Ditrigonal pyramidal (3/m)
(same H-M symbol)
| symmetry = R3m
| unit cell = a = 7.3065(5) Å,
c = 16.897(2) Å;
V = 781.2 ų; Z = 3
| color = Brown to light yellowish brown, pale yellow, yellowish green to dark green
| habit = Crystals pseudocubic rhombohedral with prominent {10{{overline|1}}1}. Commonly in crusts and massive
| lattice =
| twinning =
| cleavage = Perfect on {0001}
| fracture =
| tenacity =
| mohs = 3.5–4.5
| luster = Vitreous, resinous
| refractive = nω = 1.930 nε = 1.930 n = 1.93 – 1.96
| opticalprop = Uniaxial (−), may appear anomalously biaxial
| birefringence = δ = 0.000
| pleochroism =
| 2V =
| dispersion =
| streak =
| gravity = 4.295 (measured), 4.31 (calculated)
| density =
| melt =
| fusibility =
| diagnostic =
| solubility =
| diaphaneity = transparent
| other = Readily soluble in warm HCl
|references = [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Corkite Mineralienatlas]Mindat.org http://www.mindat.org/min-1130.htmlWebmineral.com http://webmineral.com/data/Corkite.shtmlEuroMin.net http://euromin.w3sites.net//mineraux/CORKITE.html{{Cite web |url=http://www.handbookofmineralogy.com/pdfs/corkite.pdf |title=Handbook of Mineralogy |access-date=2010-07-30 |archive-date=2011-07-28 |archive-url=https://web.archive.org/web/20110728180705/http://www.handbookofmineralogy.com/pdfs/corkite.pdf |url-status=dead }}
}}
Corkite is a phosphate mineral in the beudantite subgroup of the alunite group. Corkite is the phosphate analogue of beudantite and with it, a complete solid solution range exists. Corkite will also form a solid solution with kintoreite.
Corkite is named after County Cork, Ireland; the location where the first notable amount was discovered in 1869. Like many of the other minerals in the beudantite group, corkite is a relatively uncommon, secondary mineral that occurs in oxidation zones near hydrothermal base metal deposits. It occurs associated with pyromorphite, malachite, plumbojarosite, limonite and quartz.