How to identify Sunstone
Oligoclase (feldspar group)
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Open the appTo 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
Color
Overall color and any zoning or banding
Typically yellow, orange, pink, red, or green, often with a metallic glitter from inclusions.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to sub-vitreous on cleavage surfaces; aventurescent (spangled) due to inclusions.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Crystalline, often granular or massive. Individual crystals can be tabular or prismatic.
- 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
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Two distinct cleavages at approximately 90 degrees (86-94 degrees), characteristic of feldspars.
- 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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