How to identify Sunstone
Plagioclase Feldspar (Oligoclase variety)
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Open the appTo 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
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
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
Texture
Grain size and surface feel: coarse, fine, glassy
Crystalline, often granular in massive forms. The aventurescence is the key textural feature.
- 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
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
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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