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How to identify Moonstone

Adularia (Potassium Feldspar)

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To correctly identify Moonstone (Adularia (Potassium 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, gray, peach, pink, yellow, or brown, with a characteristic bluish-white to white adularescence.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to pearly on cleavage surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth when polished (cabochon cut). Uneven to conchoidal fracture if broken.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Often found as anhedral to subhedral masses or in tabular to prismatic crystals, though gem-quality material is usually massive and cut into cabochons. Adularia specifically forms pseudo-orthorhombic crystals, often in characteristic 'Adularia habit' (rhombic or tabular).

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cleavage in two directions, intersecting at approximately 90 degrees (characteristic of feldspars).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Moonstone, particularly the adularia variety, is found in low-temperature hydrothermal veins, pegmatites, and alpine-type fissures. It can also occur in some igneous and metamorphic rocks. The formation requires slow cooling to allow for the exsolution of albite and orthoclase lamellae.

Key Facts

Hardness
6-6.5 (Mohs scale)
Specific Gravity
2.56-2.59 g/cm³
Crystal System
Monoclinic (for orthoclase and adularia varieties)
Color
Colorless, white, gray, peach, pink, yellow, brown; with blue or white adularescence.
Luster
Vitreous to pearly.
Transparency
Transparent to translucent.
Fracture
Uneven to conchoidal.
Cleavage
Perfect in two directions, intersecting at approximately 90 degrees.
Composition
Potassium aluminum silicate (KAlSi3O8) with intergrown sodium aluminum silicate (NaAlSi3O8).

Physical characteristics

  • Crystal Habit: Typically massive, granular, or in tabular to prismatic crystals (especially adularia).
  • Cleavage Type: Perfect basal {001} and good prismatic {010} cleavage, intersecting at 90 degrees.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to pearly on cleavage surfaces.

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