GORMANITE
Class : Phosphates, arsenates, vanadates
Subclass : Hydrated phosphates
Crystal System : Triclinic
Chemistry : Fe3Al4(PO4)4(OH)6 2H2O
Rarity : Very rare
Gormanite is a secondary phosphate that forms a series with souzalite, the magnesian term. It owes its name to Canadian mineralogy professor Donald Hermet Gorman of the University of Toronto. It is a very rare mineral which is formed preferentially in granitic pegmatites, but seems to be able to be satisfied with varied contexts since it is also found in the oxidation zone of ferriferous phosphate deposits and it is known exceptionally in tonalite fissures. It forms small elongated lamellar crystals, not exceeding one centimeter, frequently united in radial aggregates, of a dark blue-green color. It is a mineral intended only for the collection which is little known to the general public.
Main photo : Gormanite from Big Fish River, Yukon, Canada
Gormanite in the World
Twinning
This mineral twins around the {001} compositional plane and the [010] axis, but is not observable due to crystal size and morphology.
Fakes ans treatments
Hardness : 4 to 5
Density : 3.1
Fracture : Splintery
Streak : Green
TP : Translucent to transparent
IR : 1.619 to 1.660
Birefringence : 0.041
Optical character : Biaxial -
Pleochroism : Strong
Fluorescence : None
Solubility : Not specified
Magnetism : None
Radioactivity : None