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How to identify Peach Moonstone

Orthoclase Feldspar (variety Moonstone)

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To correctly identify Peach Moonstone (Orthoclase Feldspar (variety Moonstone)), 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

    Soft peach, orange-pink, or creamy orange, often with a translucent to semi-transparent body color. The adularescence can appear as a bluish-white or silvery sheen.

  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

    Typically smooth when polished, but can exhibit a slightly uneven surface on rough specimens due to cleavage.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Usually found as anhedral to subhedral masses, or as tabular to prismatic crystals within a matrix. Often cut into cabochons for jewelry.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cleavage in two directions at approximately 90 degrees (specifically, {001} perfect and {010} good).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Occurs in granitic and syenitic pegmatites, hydrothermal veins, and some metamorphic rocks. It is often associated with other feldspars, quartz, mica, and amphiboles.

Key Facts

Hardness
6 - 6.5 on the Mohs scale
Specific Gravity
2.56 - 2.59
Crystal System
Monoclinic
Color
Peach, orange-pink, creamy orange, often with a bluish-white or silvery adularescence
Luster
Vitreous to pearly
Transparency
Translucent to semi-transparent
Fracture
Uneven to conchoidal
Cleavage
Perfect in two directions at approximately 90 degrees ({001} perfect, {010} good)
Composition
Potassium aluminum silicate (KAlSi3O8)

Physical characteristics

  • Crystal Habit: Typically massive, granular, or as tabular to prismatic crystals. Often found as anhedral grains in rocks.
  • Cleavage Type: Perfect in two directions, forming nearly right angles.
  • Fracture Type: Uneven to conchoidal, particularly on surfaces not defined by cleavage.
  • Tenacity: Brittle
  • Luster Type: Vitreous on crystal faces, pearly on cleavage surfaces.

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