LEPIDOLITE [Potassium Lithium Aluminium Silicate Hydroxide Fluoride]
6/01/2012
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[ Silicates : Phyllosilicates : Micas ]
KLi2Al(Al, Si)3O10(F, OH)2, potassium lithium aluminium Silicate Hydroxide Fluoride
Ore of lithium, ornamental stone and heat insulator for industrial purposes
Lepidolite is an uncommon mica and has only in the past decade become available on the mineral market in large quantities. Lepidolite is an ore of lithium and forms in granitic masses that contain a substantial amount of lithium. The lithium content in lepidolite does vary greatly however and low lithium lepidolite is nearly useless as an ore of lithium. The typical violet to pink colour of lepidolite is characteristic and is the only field test available to identify lepidolite from other micas. Pink muscovite or very pale lepidolite may confuse an identification.
Lepidolite, like other micas, has a layered structure of lithium aluminium silicate sheets weakly bonded together by layers of potassium ions. These potassium ion layers produce the perfect cleavage. Lepidolite crystals accompany such other lithium bearing minerals such as tourmaline, amblygonite and spodumene and can add greatly to the value of these specimens. A rock made of granular pink lepidolite and red to pink tourmaline is used as an ornamental stone for carving. Single large plates or "books" of lepidolite can have appealling violet colour and make attractive mineral specimens.
Luster : vitreous to pearly
Transparency : crystals are transparent to translucent
Crystal Habits :
Include tabular to prismatic crystals with a prominant pinacoid termination. Lepidolite's four prism faces and two pinacoid faces form pseudo-hexagonal crystal "books". The sides of the crystal often tend to tapper. Also as micaseous, lamellar or granular rock forming masses
Cleavage : perfect in one direction producing thin sheets or flakes
Fracture : not readily observed due to cleavage but is uneven
Hardness : 2.5
Specific Gravity : approx. 2.8+ (average)
Streak : white
Other :
sheets are flexible and elastic, meaning they can be bent and will flex back to original shape. Also some specimens may show triboluminescence
Associated Minerals :
quartz, feldspars, spodumene, ambygonite and tourmaline especially elbaite
Major Occurrences :
include Brazil; Ural Mountains, Russia; several African localities and California, USA
Best Indicators :
crystal habit, colour, cleavage, elastic sheets and associations
KLi2Al(Al, Si)3O10(F, OH)2, potassium lithium aluminium Silicate Hydroxide Fluoride
Ore of lithium, ornamental stone and heat insulator for industrial purposes
Lepidolite is an uncommon mica and has only in the past decade become available on the mineral market in large quantities. Lepidolite is an ore of lithium and forms in granitic masses that contain a substantial amount of lithium. The lithium content in lepidolite does vary greatly however and low lithium lepidolite is nearly useless as an ore of lithium. The typical violet to pink colour of lepidolite is characteristic and is the only field test available to identify lepidolite from other micas. Pink muscovite or very pale lepidolite may confuse an identification.
Lepidolite, like other micas, has a layered structure of lithium aluminium silicate sheets weakly bonded together by layers of potassium ions. These potassium ion layers produce the perfect cleavage. Lepidolite crystals accompany such other lithium bearing minerals such as tourmaline, amblygonite and spodumene and can add greatly to the value of these specimens. A rock made of granular pink lepidolite and red to pink tourmaline is used as an ornamental stone for carving. Single large plates or "books" of lepidolite can have appealling violet colour and make attractive mineral specimens.
Physical Characteristics
Colour : violet to pale pink or white and rarely gray or yellowLuster : vitreous to pearly
Transparency : crystals are transparent to translucent
Crystal Habits :
Include tabular to prismatic crystals with a prominant pinacoid termination. Lepidolite's four prism faces and two pinacoid faces form pseudo-hexagonal crystal "books". The sides of the crystal often tend to tapper. Also as micaseous, lamellar or granular rock forming masses
Cleavage : perfect in one direction producing thin sheets or flakes
Fracture : not readily observed due to cleavage but is uneven
Hardness : 2.5
Specific Gravity : approx. 2.8+ (average)
Streak : white
Other :
sheets are flexible and elastic, meaning they can be bent and will flex back to original shape. Also some specimens may show triboluminescence
Associated Minerals :
quartz, feldspars, spodumene, ambygonite and tourmaline especially elbaite
Major Occurrences :
include Brazil; Ural Mountains, Russia; several African localities and California, USA
Best Indicators :
crystal habit, colour, cleavage, elastic sheets and associations