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

Good crystals of tschermakite come from gabbros from Finland (Kutemajärvi, Perniö) and from kyanite amphibolites from Glenelg (Scotland).

Tschermakite in France

In France, tschermakite is reported at Viala-du-Tarn (Tarn) and in the gabbros of Château-Lambert (Haute-Saône).

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

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