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How to identify Moonstone

Adularia (Orthoclase variety)

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To correctly identify Moonstone (Adularia (Orthoclase variety)), 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 colorless to white, with shades of gray, brown, yellow, pink, or green. The most desirable moonstones exhibit a blue adularescence.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to pearly.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth when polished, often exhibiting a characteristic internal glow.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Monoclinic (orthoclase variety) or Triclinic (plagioclase variety). Crystals are typically prismatic, tabular, or blocky, but moonstone is usually found in massive or granular forms, often cut as cabochons.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect in two directions, intersecting at approximately 90 degrees (orthoclase) or slightly less than 90 degrees (plagioclase).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Moonstone (adularia) is typically found in low-temperature hydrothermal veins and alpine-type fissures, often associated with granitic pegmatites, syenites, and other igneous rocks. Peristerite moonstone is found in pegmatites and metamorphic rocks.

Key Facts

Hardness
6.0 - 6.5 on the Mohs scale.
Specific Gravity
2.56 - 2.59 (Orthoclase); 2.55 - 2.75 (Plagioclase).
Crystal System
Monoclinic (Orthoclase variety, Adularia) or Triclinic (Plagioclase variety, Peristerite).
Color
Colorless, white, gray, brown, yellow, pink, green; with characteristic adularescence.
Luster
Vitreous to pearly.
Transparency
Transparent to translucent.
Fracture
Uneven to conchoidal.
Cleavage
Perfect in two directions, intersecting at approximately 90 degrees (orthoclase) or slightly less (plagioclase).
Composition
Potassium aluminum silicate (KAlSi3O8) for orthoclase varieties; Sodium calcium aluminum silicate (Na,Ca)(Al,Si)AlSi2O8) for plagioclase varieties.

Physical characteristics

  • Crystal Habit: Prismatic, tabular, blocky, massive, granular. Often cut as cabochons to enhance adularescence.
  • Cleavage Type: Perfect in two directions, {001} and {010}.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to pearly on cleavage surfaces.

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