
mineral
Sunstone (Aventurine Feldspar)
(Ca,Na)((Al,Si)2Si2O8) with inclusions of Cu or Fe2O3
AI-generated identification · may be incorrectHardness: 6-6.5 Mohs scale; Color: Orange, reddish-brown with metallic schiller; 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 metallic schiller
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 Mohs scale; Color: Orange, reddish-brown with metallic schiller; 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 pegmatites. The metallic glitter (aventurescence) is caused by tiny plate-like inclusions of hematite, goethite, or copper that reflect light.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings) and as a lapidary material for carvings and metaphysical collecting.
Geological facts
Oregon Sunstone is unique because its inclusions are made of pure copper, whereas most others use hematite. In 1987, it was designated as the state gemstone of Oregon.
Field identification & locations
Identify by looking for the schiller effect (a metallic glitter) when the stone is rotated under light. Commonly found in Oregon (USA), Norway, Tanzania, India, and Madagascar.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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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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