Lepidolite

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Crystal of lepidolite, Brazil

Lepidolite (KLi2Al(Al,Si)3O10(F,OH)2) is a lilac or rose-violet colored phyllosilicate mineral of the mica group that is a secondary source of lithium.[1] It is associated with other lithium-bearing minerals like spodumene in pegmatite bodies. It is one of the major sources of the rare alkali metals, rubidium and caesium.[2]

Physical Properties

Color: violet lombo pale pink to white, sometimes gray or yellow.
Luster: vitreous to pearly
Transparency: transparent to translucent.
Crystal System: monoclinic; 2/m.
Crystal Habits: include tabular to prismatic crystals with a prominent pinacoid termination. Lepidolite forms pseudo-hexagonal "books." Also as micaceous or granular masses.
Cleavage: perfect in one direction perpendicular to the c-axis.
Fracture: uneven.
Hardness: 2.5
Specific Gravity: 2.8+
Streak: white
Density:2.8-2.9 Average size 2.84

Associated Minerals: quartz, feldspar, spodumene, amblygonite, tourmaline.

Notable Occurrences: Brazil; Ural Mountains, Russia; California; Tanco Pegmatite, Bernic Lake Manitoba, Canada.

References
ISBN links support NWE through referral fees

  1. "Manual of Mineralogy, 20th Ed." by Cornelius Hurlbut and Cornelis Klein.
  2. H. Nechamkin, The Chemistry of the Elements, McGraw-Hill, New York, 1968.

See also: List of minerals

ca:Lepidolita gl:Lepidolita it:Lepidolite nl:Lepidoliet pl:Lepidolit pt:Lepidolite fi:Lepidoliitti