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How to identify Jadeite

Na(Al,Fe3+)Si2O6

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To correctly identify Jadeite (Na(Al,Fe3+)Si2O6), 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

    Ranges from white, gray, and pale green to dark green, blue-green, lavender, pink, brown, and black. The most prized color is an intense, translucent emerald green (Imperial Jade) due to trace chromium.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to greasy, sometimes pearly on cleavage surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically fine-grained, interlocking granular aggregates, giving it a smooth, waxy feel when polished. Can be massive or fibrous.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Rarely found as distinct crystals; usually occurs as dense, compact, interlocking aggregates of microscopic grains. When crystals are present, they are typically prismatic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Two distinct cleavages at nearly 90 degrees (pyroxene cleavage), but rarely observed in massive material due to its fine-grained, interlocking nature. Fracture is more common.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    High-pressure, low-temperature metamorphic rocks (blueschists, eclogites) in subduction zones. Also found in serpentinite-associated metasomatic deposits and alluvial placers derived from these primary sources.

Key Facts

Hardness
6.5-7 on the Mohs scale.
Specific Gravity
3.30-3.38 (higher than nephrite).
Crystal System
Monoclinic.
Color
White, green, lavender, blue-green, pink, brown, black. Often mottled or variegated.
Luster
Vitreous to greasy, sometimes pearly.
Transparency
Translucent to opaque, rarely semi-transparent.
Fracture
Splintery to uneven, due to its interlocking granular structure.
Cleavage
Perfect on {110} and {110} at nearly 90 degrees, but rarely observed in massive material.
Composition
Sodium aluminum silicate with variable iron: Na(Al,Fe3+)Si2O6.

Physical characteristics

  • Crystal Habit: Typically massive, granular, or fibrous aggregates. Rarely as distinct prismatic crystals.
  • Cleavage Type: Perfect prismatic cleavage at approximately 87 and 93 degrees, but usually not visible in massive material.
  • Fracture Type: Splintery to uneven, conchoidal in rare instances.
  • Tenacity: Extremely tough (resistant to breaking and chipping), making it highly durable.
  • Luster Type: Vitreous to greasy, sometimes waxy on polished surfaces.

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