FERROSILITE

    Class : Silicates
    Subclass : Inosilicates
    Crystal system : Orthorhombic
    Chemistry : FeSiO3
    Rarity : Common


Ferrosilite belongs to the group of orthorhombic pyroxenes (orthopyroxenes). It forms a series with enstatite (magnesian) and hypersthene. It is a constituent of basic and ultrabasic rocks (especially gabbros and norites) as well as BIFs. It is also present but rarer in high grade metamorphic rocks (granulites and charnockites), contact deposits (hornfel), and volcanic rocks. Its name comes from its chemical composition : iron + silicon. Clear crystals are rare and only known in gabbroic pegmatites : they are then flattened prisms. Ferrosilite generally occurs in fibrous, lamellar, grainy or compact masses, greenish black to brownish black, sometimes dark green or dark brown. It changes into amphibole (uralitization). It is exceptionally used as a gem.

Main photo : Ferrosilite from Caspar quarry, Ettringen, Germany © Volker Betz

Ferrosilite in the World

Beautiful ferrosilite crystals have been extracted from the BIFs of Montana (Ruby Range, Ruby Creek, etc...) and Nigeria (Bauchi). Large crystals are also known from the Broken Hill granulite (Australia).

Ferrosilite in France

In France, ferrosilite is reported at Roca Gelera near Céret (Pyrénées-Orientales).

Twinning

No twins known for this mineral species.

Fakes and treatments

No fakes recorded for this mineral species.



Hardness : 5 to 6
Density : 3.6 à 4
Fracture : Irregular
Streak : Gray-brown


TP : Translucent to transparent
RI : 1.71 to 1.788
Birefringence : 0.016 to 0.021
Optical character : Biaxial +
Pleochroism : Low
Fluorescence : None


Solubility : Hydrochloric acid


Magnetism : Paramagnetic

Radioactivity : None