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How to identify Sunstone

Oligoclase (variety of Feldspar)

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To correctly identify Sunstone (Oligoclase (variety of 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 orange, pink, red, yellow, or colorless, often with a metallic glitter. Can also be green.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-vitreous, with a distinct metallic or spangled aventurescence.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular, depending on crystal size and habit.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Usually found as anhedral to subhedral grains in igneous rocks, or as well-formed tabular crystals in pegmatites. Often massive.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect in two directions, nearly at right angles (approximately 90 degrees).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Commonly found in mafic igneous rocks (e.g., basalt, gabbro), pegmatites, and some metamorphic rocks. Also found in placer deposits due to its relative hardness and resistance to weathering.

Key Facts

Hardness
6 - 6.5 on the Mohs scale
Specific Gravity
2.62 - 2.67
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 in two directions ({001} and {010}) at nearly 90 degrees.
Composition
Sodium calcium aluminum silicate, (Na,Ca)(Al,Si)AlSi2O8, with inclusions of hematite, goethite, or copper.

Physical characteristics

  • Crystal Habit: Typically anhedral to subhedral grains, massive, or as tabular crystals.
  • Cleavage Type: Perfect in two directions, nearly at right angles.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-vitreous, with aventurescence.

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