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How to identify Sunstone

Oligoclase (feldspar group)

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To correctly identify Sunstone (Oligoclase (feldspar group)), 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 yellow, orange, pink, red, or green, often with a metallic glitter from inclusions.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-vitreous on cleavage surfaces; aventurescent (spangled) due to inclusions.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often granular or massive. Individual crystals can be tabular or prismatic.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically anhedral to subhedral grains in igneous and metamorphic rocks. Well-formed crystals are monoclinic (for orthoclase component) or triclinic (for albite-anorthite series, including oligoclase), often tabular or prismatic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Two distinct cleavages at approximately 90 degrees (86-94 degrees), characteristic of feldspars.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Felsic to intermediate igneous rocks (volcanic and plutonic), some metamorphic rocks, and placer deposits.

Key Facts

Hardness
6 to 6.5 on the Mohs scale
Specific Gravity
2.62 to 2.68
Crystal System
Triclinic
Color
Colorless, yellow, orange, pink, red, green, often with metallic glitter (aventurescence).
Luster
Vitreous to sub-vitreous, with aventurescence.
Transparency
Transparent to translucent.
Fracture
Uneven to conchoidal.
Cleavage
Perfect on {001} and good on {010}, intersecting at approximately 86-94 degrees.
Composition
Sodium calcium aluminum silicate, (Na,Ca)(Al,Si)AlSi2O8, with NaAlSi3O8 (albite) content between 70% and 90% and CaAl2Si2O8 (anorthite) content between 10% and 30%.

Physical characteristics

  • Crystal Habit: Typically anhedral to subhedral grains, massive, or in tabular to prismatic crystals.
  • Cleavage Type: Perfect on {001} and good on {010}, forming two planes at nearly 90 degrees.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-vitreous, with aventurescence.

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