sugilite

{{Infobox mineral | boxbgcolor= #a142d6 |boxtextcolor = #fff | name = Sugilite | category = Cyclosilicate | image = Smithsonian Exhibit Stone.jpg | imagesize = 260px | caption = 16kg Manganoan Sugilite, GIA Laboratory Certified, Smithsonian Exhibition Stone, I.Kurgan Royal Azel, Hall of Gems Smithsonian Museum 1981, Wessels Mine in Northern Cape Province, South Africa | formula = KNa2(Fe,Mn,Al)2Li3Si12O30 | IMAsymbol = Sug | strunz = 9.CM.05 | dana = 63.02.01a.09 | system = Hexagonal | class = Dihexagonal dipyramidal (6/mmm) H-M symbol: (6/m 2/m 2/m) | symmetry = P6/mcc | unit cell = a = 10, c = 14 [Å]; Z = 2 | color = Light brownish-yellow, purple, violet, reddish violet, pale pink, colorless | habit = Prismatic crystals, typically granular to massive | twinning = | cleavage = Poor on {0001} | fracture = | tenacity = | mohs = 6– | luster = Vitreous | refractive = nω = 1.610 nε = 1.607 | opticalprop = Uniaxial (−) | birefringence = δ = 0.003 | pleochroism = Weak | streak = White | gravity = 2.74 | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Transparent to translucent | other = | references = }}

Sugilite ( ) is a relatively rare pink to purple cyclosilicate mineral with the complex chemical formula KNa2(Fe, Mn, Al)2Li3Si12O30. Sugilite crystallizes in the hexagonal system with prismatic crystals. The crystals are rarely found and the form is usually massive. It has a Mohs hardness of 5.5–6.5 and a specific gravity of 2.75–2.80. It is mostly translucent. Sugilite was first described in 1944 by the Japanese petrologist Ken-ichi Sugi (1901–1948) for an occurrence on Iwagi Islet, Japan, where it is found in an aegirine syenite intrusive stock. It is found in a similar environment at Mont Saint-Hilaire, Quebec, Canada. In the Wessels mine in Northern Cape Province of South Africa, sugilite is mined from a strata-bound manganese deposit. It is also reported from Liguria and Tuscany, Italy; New South Wales, Australia and Madhya Pradesh, India.