
mineral
Sunstone
Plagioclase Feldspar (Na,Ca)(Al,Si)4O8
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Orange, reddish-brown, or gold with metallic schiller; 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, reddish-brown, or gold with metallic schiller
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Orange, reddish-brown, or gold with metallic schiller; 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 environments, specifically in lava flows (basalt) or pegmatites. The metallic 'glitter' is caused by tiny inclusions of copper, hematite, or goethite. Famous deposits include the Oregon Sunstone from the Tertiary period.
Uses & applications
Primarily used as a gemstone in jewelry (earrings, rings, pendants) and as a collector's mineral specimen.
Geological facts
Oregon Sunstone is the official state gemstone of Oregon. The 'shiller' or aventurescence effect is what makes it unique, caused by light reflecting off internal copper platelets.
Field identification & locations
Identify by its unique aventurescence (metallic glitter). Common locations include Oregon (USA), Norway, Tanzania, and India. In the field, look for feldspar cleavage combined with flashes of reddish-orange color.
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