GEDRITE
Class : Silicates
Subclass : Inosilicates
Crystal system : Orthorhombic
Chemistry : (Mg,Fe)5Al2(Si6Al2)O22(OH)2
Rarity : Common
Gedrite belongs to the group of orthorhombic amphiboles and forms two series with magnesiogedrite and ferrogedrite. Formerly classified as a variety of anthophyllite ; gedrite is now considered a mineral species in its own right which is distinguished from anthophyllite by its high aluminum contents. It is an amphibole of medium to high metamorphic grade, and rocks of contact metamorphism. It owes its name to its location of discovery : the Héas valley near Gèdre (Hautes-Pyrénées, France). Gedrite generally occurs in fibrous masses, sometimes in asbestiform aggregates (partly making up amosite), rarely in unfinished prismatic crystals. It is dark greenish brown to dark grayish green, sometimes brown. As with other asbestos, it was used in construction, insulation, the manufacture of fireproof materials, etc...
Main photo : Gédrite from Väster Silvberg, Smedjebacken, Dalarna County, Sweden © Michael Roarke
Gedrite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 5.5 to 6
Density : 3.15 to 3.26
Fracture : Fibrous
Streak : White
TP : Translucent to transparent
RI : 1.671 to 1.690
Birefringence : 0.019
Optical character : Biaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Insoluble
Magnetism : Paramagnetic
Radioactivity : None