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How to identify Lepidolite

K(Li,Al)3(Si,Al)4O10(F,OH)2

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To correctly identify Lepidolite (K(Li,Al)3(Si,Al)4O10(F,OH)2), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.

Step-by-step identification

  1. 1

    Color

    Overall color and any zoning or banding

    Typically lilac, pink, or purple; less commonly gray, white, or yellowish. The color is often due to trace amounts of manganese.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to pearly on cleavage surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Often found in scaly aggregates, 'books' of stacked flakes, or radiating masses. Individual crystals are tabular.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Monoclinic, typically forming pseudohexagonal tabular crystals, often in aggregates. Can also be massive or granular.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect basal cleavage (001), allowing it to be split into thin, flexible, and elastic sheets.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Predominantly found in granitic pegmatites, especially those enriched in lithium. Also occurs in high-temperature hydrothermal veins and greisens associated with granitic intrusions.

Key Facts

Hardness
2.5-3.5 on the Mohs scale
Specific Gravity
2.8-2.9 g/cm³
Crystal System
Monoclinic
Color
Lilac, pink, purple, gray, white, yellowish
Luster
Vitreous to pearly
Transparency
Transparent to translucent
Fracture
Uneven to splintery (not typically observed due to perfect cleavage)
Cleavage
Perfect basal cleavage on {001}
Composition
Potassium lithium aluminum silicate hydroxide fluoride

Physical characteristics

  • Crystal Habit: Pseudohexagonal tabular crystals, often in scaly aggregates, 'books', or radiating masses. Can also be massive or granular.
  • Cleavage Type: Perfect basal cleavage (one direction)
  • Fracture Type: Uneven to splintery (rarely observed)
  • Tenacity: Flexible and elastic (thin sheets)
  • Luster Type: Vitreous to pearly

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