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How to identify Chrysoprase

Chalcedony (cryptocrystalline quartz) colored by nickel

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To correctly identify Chrysoprase (Chalcedony (cryptocrystalline quartz) colored by nickel), 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

    Apple-green to deep green, often uniform, but can show slight banding or mottling. The color is typically stable, though prolonged exposure to sunlight or heat can sometimes cause fading in some specimens.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to vitreous (glassy) when polished, dull to waxy on rough surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Microcrystalline to cryptocrystalline, appearing massive and dense. Smooth to the touch when polished.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Massive, botryoidal, reniform, or stalactitic aggregates. Individual crystals are microscopic and not visible to the naked eye.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, due to its cryptocrystalline nature.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in the weathered zones (laterites) of nickel-bearing ultramafic rocks (e.g., serpentinites, dunites, peridotites). It forms in veins and nodules within these altered host rocks, often associated with other secondary nickel minerals.

Key Facts

Hardness
6.5 - 7 on the Mohs scale
Specific Gravity
2.58 - 2.64
Crystal System
Trigonal (as quartz, but cryptocrystalline aggregates appear massive)
Color
Apple-green to deep green
Luster
Waxy to vitreous
Transparency
Translucent to opaque
Fracture
Conchoidal to uneven
Cleavage
None
Composition
SiO2 (silicon dioxide) with trace amounts of nickel (Ni)

Physical characteristics

  • Crystal Habit: Massive, botryoidal, reniform, stalactitic aggregates
  • Cleavage Type: None
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Waxy to vitreous

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