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 color 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 aluminum 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 color and make attractive mineral
specimens.
PHYSICAL CHARACTERISTICS:
Color is violet to pale pink or white and rarely gray or yellow.
Luster is vitreous to pearly.
Transparency crystals are transparent to translucent.
Crystal System is monoclinic; 2/m
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 is perfect in one direction producing thin sheets or flakes.
Fracture is not readily observed due to cleavage but is uneven.
Hardness is 2.5.
Specific Gravity is approximately 2.8+ (average)
Streak is white.
Associated Minerals are quartz, feldspars, spodumene, ambygonite and
tourmaline especially elbaite.
Other Characteristics: cleavage sheets are flexible and elastic, meaning
they can be bent and will flex back to original shape. Also some specimens
may show triboluminescence.
Notable Occurrences include Brazil; Ural Mountains, Russia; several
African localities and California, USA.
Best Field Indicators are crystal habit, color, cleavage, elastic sheets
and associations.
Art,
Passion, and Life
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 color 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 aluminum 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 color and make attractive mineral
specimens. 
