
mineral
Sunstone
Heliolite (Oligoclase or Orthoclase Feldspar), (Ca,Na)(Al,Si)4O8
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Orange, red, or golden with metallic flashes; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees; Specific gravity: 2.62-2.67
- Hardness
- 6-6
- Color
- Orange, red, or golden with metallic flashes
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Orange, red, or golden with metallic flashes; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees; Specific gravity: 2.62-2.67
Formation & geological history
Formed in igneous rocks like basalt or andesite, and occasionally in pegmatites. The metallic 'aventurescence' is caused by tiny plate-like inclusions of hematite, copper, or goethite. Forms in volcanic lava flows or deep-seated plutonic rocks.
Uses & applications
Primarily used as a gemstone for jewelry (rings, pendants, earrings) and as a collector's mineral specimen. High-quality Oregon Sunstone is highly prized for its copper content.
Geological facts
The metallic shimmer is known as aventurescence. Oregon Sunstone is the official state gemstone of Oregon and is unique because its inclusions are pure copper rather than hematite. Ancient Vikings reportedly used sunstones for navigation on cloudy days.
Field identification & locations
Identify by its unique 'schiller' effect or metallic glitter when rotated under light. Common locations include Oregon (USA), Norway, India, Canada, and Russia. Look for feldspar traits with internal reflections.
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Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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