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How to identify Moonstone

Adularia (variety of Orthoclase Feldspar)

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To correctly identify Moonstone (Adularia (variety of Orthoclase Feldspar)), 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, but can also be 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 'schiller' or 'adularescence' effect.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Usually found in massive or tabular forms. Crystals are typically monoclinic, often prismatic or blocky, but well-formed crystals are rare in gem quality material.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect in two directions, intersecting at approximately 90 degrees (specifically 90 degrees and 90 degrees 30 minutes).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Occurs in pegmatites, granites, syenites, and some metamorphic rocks. It is often found in hydrothermal veins and alpine-type fissures, particularly the adularia variety.

Key Facts

Hardness
6-6.5 on the Mohs scale.
Specific Gravity
2.56-2.59.
Crystal System
Monoclinic.
Color
Colorless, white, gray, brown, yellow, pink, green; with blue or white adularescence.
Luster
Vitreous to pearly.
Transparency
Transparent to translucent.
Fracture
Uneven to conchoidal.
Cleavage
Perfect in two directions (basal {001} and prismatic {010}) at approximately 90 degrees.
Composition
Potassium aluminum silicate (KAlSi3O8).

Physical characteristics

  • Crystal Habit: Typically massive, tabular, or prismatic. Often found as cleavage fragments or anhedral grains in rocks. Well-formed crystals are rare in gem quality.
  • Cleavage Type: Perfect in two directions, intersecting at 90 degrees and 90 degrees 30 minutes.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to pearly on cleavage surfaces.

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