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How to identify Sunstone

Plagioclase Feldspar (Oligoclase or Labradorite variety)

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To correctly identify Sunstone (Plagioclase Feldspar (Oligoclase or Labradorite variety)), 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 reddish-brown, often with a metallic glitter. Can also be colorless, green, or blue.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-vitreous, with a distinct metallic glitter (aventurescence) from inclusions.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

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

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically anhedral to subhedral grains within igneous or metamorphic rocks. When well-formed, it exhibits triclinic crystal habits, often tabular or prismatic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect in two directions, nearly at 90 degrees (86 degrees and 94 degrees), characteristic of plagioclase feldspars.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in mafic igneous rocks (e.g., basalts, gabbros), felsic igneous rocks (e.g., granites, pegmatites), and some metamorphic rocks. The most famous occurrences are in basaltic lava flows where it forms phenocrysts.

Key Facts

Hardness
6 to 6.5 on the Mohs scale
Specific Gravity
2.62 to 2.67 g/cm3
Crystal System
Triclinic
Color
Colorless, yellow, orange, pink, red, reddish-brown, green, blue, often with metallic glitter.
Luster
Vitreous to sub-vitreous, with aventurescence (schiller effect).
Transparency
Transparent to translucent
Fracture
Uneven to conchoidal
Cleavage
Perfect in two directions (pinacoidal), nearly at 90 degrees (86° and 94°).
Composition
Sodium calcium aluminum silicate (Na,Ca)(Al,Si)AlSi2O8)

Physical characteristics

  • Crystal Habit: Typically anhedral to subhedral grains, massive, granular. Can form tabular or prismatic crystals.
  • Cleavage Type: Perfect on {001} and {010}, nearly at right angles.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-vitreous, with aventurescence.

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