
mineral
Sunstone
Aventurine Feldspar (composition: (Ca,Na)((Al,Si)2Si2O8))
AI-generated identification · may be incorrectHardness: 6-6.5 (Mohs scale); Color: Orange, reddish-brown with internal metallic glitters; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.62-2.67
- Hardness
- 6-6
- Color
- Orange, reddish-brown with internal metallic glitters
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 (Mohs scale); Color: Orange, reddish-brown with internal metallic glitters; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.62-2.67
Formation & geological history
Formed in igneous environments, typically within basaltic lava flows or granitic pegmatites. The metallic 'schiller' effect is caused by tiny inclusions of copper, hematite, or goethite that precipitate during the cooling of the magma.
Uses & applications
Primarily used as a gemstone for jewelry (rings, pendants, earrings) and as a collector's mineral specimen. Known for its aesthetic schiller effect.
Geological facts
In 1987, Sunstone was designated the state gemstone of Oregon, USA. Ancient Viking legends suggest Sunstone may have been used as a navigation tool to find the sun through cloudy skies, though historians debate if they meant this specific mineral or Iceland Spar.
Field identification & locations
Identify by its 'aventurescence' (metallic glitter appearing under the surface when rotated). It is commonly found in Oregon (USA), Norway, Tanzania, India, and Russia. Collectors look for high copper content which increases the intensity of the 'sparkle'.
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
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