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How to identify Moonstone

Orthoclase Feldspar

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To correctly identify Moonstone (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, with a characteristic bluish or whitish adularescence. Can also be found in peach, pink, green, or gray hues.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to pearly, especially on cleavage surfaces. The adularescence gives it a unique internal glow.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly uneven on fracture surfaces. Cleavage surfaces are typically smooth.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Monoclinic system. Crystals are typically prismatic, often tabular, and can be twinned (e.g., Carlsbad twins). However, moonstone is more commonly found as massive or granular aggregates, or as inclusions within other rocks.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cleavage in two directions, intersecting at approximately 90 degrees (specifically, 90° 0' 0" for orthoclase). This is a key identifying feature of feldspars.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in igneous rocks such as granites, syenites, and especially pegmatites. Also occurs in some metamorphic rocks like gneisses and schists, and in hydrothermal veins. Alluvial deposits are also a significant source due to its relative hardness and resistance to weathering.

Key Facts

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

Physical characteristics

  • Crystal Habit: Prismatic, tabular, massive, granular. Often twinned (Carlsbad, Baveno, Manebach twins).
  • Cleavage Type: Perfect on {001} and {010}, intersecting at 90°.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to pearly.

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