TSCHERMAKITE
Class : Silicates
Subclass : Inosilicates
Crystal system : Monoclinic
Chemistry : Ca2Mg3Al2(Si6Al2)O22(OH)2
Rarity : Rare
Tschermakite is a calcium-magnesium amphibole, formerly considered a variety of green hornblende, it is now recognized as a mineral in its own right. It forms a continuous series with ferrotschermakite, its iron-bearing equivalent. Tschermakite is found mainly in metamorphic rocks of the upper amphibolite facies, in ultrabasic rocks and eclogites, in association with kyanite. It was named in honor of Gustave Tschermak von Seysenegg, Professor of Mineralogy at the University of Vienna (Austria). Tschermakite occurs in prismatic crystals that are often stocky with a hexagonal section, rarely doubly terminated. It is also common in masses or aggregates that are more or less fibrous to bacillary, sometimes grainy. Its color is green to green-black.
Main photo : Tschermakite from Varatskoe, Karelia, Russia © Pavel Kartashov
Tschermakite in the World
Twinning
Single or multiple twins parallel to {100} are known.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 5 to 6
Density : 3.15
Fracture : Irregular to conchoidal
Streak : Gray-green
TP : Translucent to transparent
RI : 1.623 to 1.688
Birefringence : 0.015 to 0.028
Optical character : Biaxial -
Pleochroism : Visible
Fluorescence : None
Solubility : Insoluble
Magnetism : NoneRadioactivity : None