From Wikipedia, the free encyclopedia
Jump to: navigation, search
Sugilite from Wessels Mine in Northern Cape Province, South Africa
Category Cyclosilicate
(repeating unit)
Strunz classification 09.CM.05
Dana classification 63.02.01a.09
Crystal symmetry Hexagonal
Formula mass 1,041.66
Color Light brownish-yellow, purple, violet, reddish violet, pale pink, colourless
Crystal habit Granular
Mohs scale hardness 6–6½
Luster Vitreous
Streak White
Diaphaneity Transparent to translucent
Specific gravity 2.74
References [1][2]

Sugilite (also known as lavulite) 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 to 6.5 and a specific gravity of 2.75 to 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.

Note: The mineral is commonly pronounced with a soft "g", as in "ginger". However, as with most minerals, its pronunciation is intended to be the same as the person it is named after; in this case, the Japanese name Sugi has a hard "g", as in "geese": /ˈsɡɨlt/ SOO-gi-lyt.


See also[edit]


External links[edit]