EPISTILBITE
Class : Silicates
Subclass : Tectosilicates
Crystal system : Monoclinic
Chemistry : CaAl2Si6O16 5H2O
Rarity : Rare
Epistilbite is a relatively rare species of the zeolite group. It is found mainly in the vacuoles of basalts, sometimes in the cracks of gneisses and exceptionally in beryl pegmatites. Its name is taken from the Greek epi (near) and stilbite because of the resemblance between these two minerals. As with many zeolites, the crystals are elongated prismatic, frequently twinned, grouped in spherolites or sheaves ; the largest do not exceed 3 cm. Epistilbite is colorless or variable in color : white, pinkish, sometimes salmon pink or yellow, exceptionally light green.
Main photo : Epistilbite from Jalgaon, Maharashtra, India © Dan Weinrich
EPIDOTE
Epistilbite in the World
EPIDOTE
Twinning
Twins are known on {100}, sometimes cyclical and on {110} crosswise.
Fakes and treatments
No fake listed for this mineral species.
EPIDOTE
Hardness : 4
Density : 2.22 to 2.28
Fracture : Irregular
Streak : White
TP : Translucent to transparent
RI : 1.502 to 1.512
Birefringence : 0.010
Optical character : Biaxial -
Pleochroism : None
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : None
Radioactivity : None