WOLLASTONITE
Class : Silicates
Subclass : Inosilicates
Crystal system : Triclinic
Chemistry : CaSiO3
Rarity : Fairly common to common
Wollastonite is a silicate characteristic of siliceous limestones transformed by contact metamorphism, skarns, and more rarely alkaline complexes. It has two polymorphs, pseudowollastonite and parawollastonite. Its composition is usually constant, although iron and manganese can replace part of the calcium. It was named in honor of the English chemist and mineralogist William Hyde Wollaston who discovered palladium and rhodium in 1804. Wollastonite forms masses of very elongated and often prickly acicular to lamellar crystals, commonly grouped in rosettes. Its color is white, its luster vitreous to pearly, sometimes straw yellow or pale greenish. Automorphic crystals are rare : they are more or less elongated prismatic individuals (up to 20 cm), or tabular parallel to {001} or {100}. It is a mineral quite widely used in the manufacture of tiles, ceramics, in metallurgy, in papermaking and as a material for the manufacture of electrical insulators.
Main photo : Wollastonite from Diana, New York, USA © Terry Burtzlaff
Wollastonite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 4.5 to 5
Density : 2.86 to 3.09
Fracture : Irregular
Streak : White
TP : Translucent to transparent
RI : 1.616 to 1.653
Birefringence : 0.015
Optical character : Biaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : NoneRadioactivity : None