RIEBECKITE
Class : Silicates
Subclass : Inosilicates
Crystal system : Monoclinic
Chemistry : Na2Fe5Si8O22(OH)2
Rarity : Uncommon
Riebeckite belongs to the alkaline amphibole family. It forms a series with glaucophane, the intermediate terms being called "crossite". It is a classic mineral of alkaline granites and especially of nepheline syenites in association with aegyrine ; it is rarer in granitic pegmatites. The asbestiform facies (crocidolite variety) is mainly found in metamorphic environments, particularly in metamorphosed banded iron formations. It was named in honor of the German explorer Emil Riebeck who discovered the mineral. Riebeckite is black to bluish-black in color for the asbestiform varieties and has a good cleavage {110}. Its crystals are prismatic to acicular, and frequently asbestiform.
Main photo : Riebeckite from Zagi Mountain, Pakistan © Eugene & Sharon Cisneros
Riebeckite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 5 to 5.5
Density : 3
Fracture : Conchoidal to irregular
Streak : Gray white
TP : Translucent to opaque
RI : 1.680 to 1.706
Birefringence : 0.008
Optical character : Biaxial -
Pleochroism : Strong
Fluorescence : None
Solubility : Insoluble
Magnetism : ParamagneticRadioactivity : None