MULLITE
Class : Silicates
Subclass : Nesosilicates
Crystal system : Orthorhombic
Chemistry : PbCu(VO4)(OH)
Rarity : Uncommon
Mullite is a rare aluminum silicate in nature. It is especially known in clayey xenoliths vitrified by lavas. Elsewhere, it is only observed in tiny patches in volcanic rocks, aluminous rocks subject to intense metamorphism or even diamondiferous kimberlites. On the other hand, it is formed in abundance in industrial furnaces by heating andalusite to 1450°C and kyanite or sillimanite to 1600°C : it is the basic material of the refractory industry. It is also used in the composition of various ceramics requiring high thermal resistance (automobile spark plugs for example). Calcined kaolin used for very white paints is a trade name which designates a mixture of mullite and cristobalite. The structure of mullite is close to that of sillimanite, the aluminum being partially replaced by silicon. It owes its name to its location of discovery : the Isle of Mull in Scotland. Mullite crystals are prismatic to acicular, colorless to pale pink, sometimes grayish.
Main photo : Mullite from Nickenicher Sattel, Eifel, Germany © Volker Betz
Mullite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 6 to 7
Density : 3.11 to 3.25
Fracture : Undetermined
Streak : White to gray
TP : Opaque to transparent
RI : 1.642 to 1.679
Birefringence : 0.012 to 0.026
Optical character : Biaxial +
Pleochroism : Visible
Fluorescence : None
Solubility : Insoluble
Magnetism : NoneRadioactivity : None