Monazite

Monazite is a very rare gem that is slightly radioactive as defined in 49 CFR 173.403 (greater than 70 Bq/gram) due to the presence of Thorium (Th). The fact table material is very rare as most Monazite is a dull and opaque brown. Faceted gems are usually very small but an intense reddish brown.

Monazite is a primary ore of several rare earth elements (REE) such as Thorium, Cerium, and Lanthanum. Thorium is highly radioactive. Since Monazite is radioactive it is often metamict. Metamict is the condition when the radiation destroys the crystal lattice completely while leaving the outward appearance of the crystal unchanged. Increased metamictation will increase the transformation of the mineral’s fracture from irregular/uneven to conchoidal.Monazite is widely distributed but gem quality crystals are quite rare. The main sources of gems are Minas Gerais, Brazil, and Tsumeb, Namibia. 

Category: Phosphate minerals
Formula: (Ce, La)PO4
Crystallography: Monoclinic – Prismatic
Crystal Habit: Crystals typically tabular on [100], may be prismatic, equant or wedge-shaped, to 27 cm; granular, massive.
Twinning: Common, [100] as twin and composition plane, as contact twins.
   

 

Cleavage: [100] Distinct, [010] Poor; parting on [001] or [111]
Fracture: Conchoidal to Irregular/Uneven
Tenacity: Brittle
Hardness (Mohs): 5.0 – 5.5
Density: 4.98 – 5.43 (g/cm3)
Luminescence: Dull brown cathodluminescence
Radioactivity: If rich in Thorium: Weak; GRapi = 91,584.19 (Gamma Ray American Petroleum Institute Units)
Other: Metamict if rich in Thorium. Paramagnetic

 

Color: Reddish Brown, Brown, Pale Yellow, Pink, Grayish White
Transparency: Translucent to Opaque
Luster: Vitreous to Sub-Adamantine, Resinous, Waxy
Refractive Index: 1.770 – 1.860 Biaxial (+)
Birefringence: 0.053 – 0.067
Dispersion:  r < v  or  r > v, weak, horizontal
Pleochroism: Weak; Faint to imperceptible. In pale yellows.