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How to identify Sunstone

Plagioclase Feldspar (Oligoclase variety)

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To correctly identify Sunstone (Plagioclase Feldspar (Oligoclase 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, red, or brown, often with a metallic or glittery sheen due to aventurescence. Can also be colorless.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-vitreous on cleavage surfaces, with a distinctive metallic or spangled aventurescent effect.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often granular in massive forms. The aventurescence is the key textural feature.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically occurs as anhedral to subhedral grains within igneous or metamorphic rocks. Euhedral crystals are less common but can be tabular or prismatic. Cleavage fragments are common.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect in two directions, intersecting at approximately 90 degrees (specifically, 86° and 94°), characteristic of plagioclase feldspar.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in mafic igneous rocks (basalts, andesites, gabbros), some felsic igneous rocks (granites, granodiorites), and occasionally in metamorphic rocks. Also found in placer deposits where it has weathered out of its host rock.

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, red, brown, often with a metallic glitter (aventurescence).
Luster
Vitreous to sub-vitreous, with aventurescence.
Transparency
Transparent to translucent.
Fracture
Uneven to conchoidal.
Cleavage
Perfect in two directions (pinacoidal), intersecting at approximately 86° and 94°.
Composition
Sodium calcium aluminum silicate (Na,Ca)(Al,Si)AlSi2O8, specifically the oligoclase variety with 10-30% anorthite (CaAl2Si2O8) and 70-90% albite (NaAlSi3O8) end-members, plus inclusions of hematite or goethite.

Physical characteristics

  • Crystal Habit: Typically anhedral to subhedral grains; less commonly tabular or prismatic crystals. Massive forms are common.
  • Cleavage Type: Perfect in two directions, {001} and {010}, intersecting at nearly 90 degrees (86° and 94°).
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-vitreous, with aventurescence (schiller effect).

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