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How to identify Kunzite

Spodumene (variety Kunzite)

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To correctly identify Kunzite (Spodumene (variety Kunzite)), 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

    Pink to lilac, sometimes violet-pink. Can be colorless, yellow, or green (Hiddenite) in other spodumene varieties. The color is often unevenly distributed.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to pearly on cleavage surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth, glassy feel on crystal faces; splintery or uneven on fracture surfaces.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically occurs as prismatic crystals, often flattened and striated parallel to the c-axis. Crystals can be very large and well-formed.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cleavage in two directions at nearly 90 degrees (87 and 93 degrees), and a distinct parting parallel to {100}.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Exclusively found in lithium-rich granitic pegmatites, often associated with other pegmatite minerals such as quartz, feldspar, mica, tourmaline, beryl, and other lithium minerals like lepidolite.

Key Facts

Hardness
6.5-7 on the Mohs scale
Specific Gravity
3.16-3.20 g/cm³
Crystal System
Monoclinic
Color
Pink, lilac, violet-pink (due to Mn3+)
Luster
Vitreous to pearly
Transparency
Transparent to translucent
Fracture
Uneven to splintery
Cleavage
Perfect on {110} and {110} (two directions at nearly 90 degrees), with distinct parting on {100}
Composition
Lithium aluminum inosilicate (LiAlSi2O6)

Physical characteristics

  • Crystal Habit: Prismatic, often flattened and striated parallel to the c-axis; also massive.
  • Cleavage Type: Perfect in two directions (prismatic) at approximately 87° and 93°, and distinct parting parallel to {100}.
  • Fracture Type: Uneven to splintery.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) to pearly on cleavage surfaces.

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