MONTGOMERYITE
Class : Phosphates, arsenates, vanadates
Subclass : Hydrated phosphates
Crystal system : Monoclinic
Chemistry : Ca4MgAl4(PO4)6(OH)4 12H2O
Rarity : Uncommon
Montgomeryite is a secondary phosphate which forms at the end of the oxidation sequence of phosphate nodules in granitic pegmatites and phosphate sedimentary formations : its genesis therefore requires extensive oxidizing conditions. It was named in honor of Professor of Mineralogy, Arthur Montgomery, who was the first to recognize the mineral as a new species. Montgomeryite occurs in fine striated lamellae ending in pyramids, 5 mm maximum, frequently grouped in subparallel aggregates, in masses or in encrustations of coarse lamellae. The hue is extremely variable, from colorless to dark green, including yellow, red or pale green.
Main photo : Montgomeryite from Tip Top Mine, South Dakota, USA © Jason B. Smith
Montgomeryite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 4
Density : 2.53
Fracture : Undetermined
Streak : Pale greenish white
TP : Translucent to transparent
RI : 1.572 to 1.582
Birefringence : 0.010
Optical character : Biaxial -
Pleochroism : Low
Fluorescence : None
Solubility : -
Magnetism : NoneRadioactivity : None