Kunzite (Spodumene)

Kunzite is a known member of the Spodumene category of minerals which also includes Hiddenite. It’s a treasure that is beautiful is discovered as colourless, pale to deep pink and purplish pink. Kunzite is strongly pleochroic, meaning a colour is had by it intensity distinction when viewed from different directions. Spodumene is a lithium aluminium silicate[LiAl[Si2O6] ]with a hardness of 6.5 to 7 on the Mohs scale. It typically exhibits excellent transparency and a vitreous lustre when cut and polished. Spodumene can often be distinguished by its crystal habit, fracture, and perfect prismatic cleavage, a property it shares with diamond and topaz.  Other colours of Spodumene are colourless, yellowish triphane that is pale to deep green (Hiddenite), blue-green and rarely blue.

You can find numerous localities for fine Kunzite crystals Nuristan that is including district Laghman Province, Afghanistan; Minas Gerais, Brazil; Maharashtra, Mt. City, and Anjanabonoina, Madagascar. Into the USA, giant crystals in the Etta mine, near Keystone, Pennington County, South Dakota, and from the Pala district, San Diego County, Ca.

Category: Inosilicate
Chemical Formula: LiAl[Si2O6] Lithium aluminium silicate
Crystallography: Monoclinic – Prismatic
Crystal Habit: Spodumene: Crystals are prismatic, typically flattened and striated, to 12.5 m and 54 t. Commonly massive.
Twinning: Common on [100].
   

 

Cleavage: [110] Good, [100] Good, [010] Partings
Fracture: Uneven to Subconchoidal
Tenacity: Brittle
Hardness (Mohs): 6.5 – 7.0
Density: 3.03 – 3.23 (g/cm3)
Luminescence: May show Yellow, Orange or Pink fluorescence under LW and SW UV.
Radioactivity: Not Radioactive

 

Color: Colorless, pale to deep Pink
Transparency: Transparent to Translucent
Luster: Vitreous, Dull; Pearly on cleavages
Refractive Index: 1.653 – 1.682  Biaxial ( + )
Birefringence: 0.0140 – 0.0270
Dispersion: Weak; r < v; 0.012
Pleochroism: Distinct; X = Colorless; Y = Violet Pink; Z = Purple Pink