
mineral
Sunstone
Andesine-Labradorite Feldspar ((Ca,Na)(Al,Si)4O8)
Hardness: 6-6.5 on Mohs scale; Color: Orange, reddish-brown, or gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific gravity: 2.62-2.67; Distinguished by aventurescence (metallic glitter).
- Hardness
- 6-6
- Color
- Orange, reddish-brown, or gold
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Orange, reddish-brown, or gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific gravity: 2.62-2.67; Distinguished by aventurescence (metallic glitter).
Formation & geological history
Formed in igneous environments, specifically within basaltic lava flows and pegmatites. The characteristic glitter is caused by tiny plate-like inclusions of hematite, goethite, or copper metal.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings), and as a popular specimen for mineral collectors and metaphysical practitioners.
Geological facts
The metallic 'schiller' effect or aventurescence is the most defining feature. Oregon Sunstone is unique in that its inclusions are made of pure copper, often leading to a wide variety of colors including green and bicolor specimens.
Field identification & locations
Identify by rotating under light to observe the metallic flash or 'glitter' within the stone. Found commonly in Oregon (USA), Norway, Tanzania, and India. Collectors look for clarity and the intensity of the schiller effect.
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