
mineral
Sunstone
Oligoclase (a plagioclase feldspar variant), (Na,Ca)(Al,Si)4O8
Hardness: 6-6.5 (Mohs scale); Color: Orange, reddish-brown, or yellow-gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Features: Aventurescence (metallic glitter caused by hematite or copper inclusions).
- Hardness
- 6-6
- Color
- Orange, reddish-brown, or yellow-gold
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 (Mohs scale); Color: Orange, reddish-brown, or yellow-gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Features: Aventurescence (metallic glitter caused by hematite or copper inclusions).
Formation & geological history
Formed in cooling igneous rocks like pegmatites or basaltic lavas. The metallic glitter is caused by inclusions that crystallize under high temperatures during the cooling process. Common in Cenozoic deposits (approx. 15-30 million years old in some regions like Oregon).
Uses & applications
Primarily used as a gemstone for jewelry (rings, pendants, earrings), ornamental carvings, and by mineral collectors for its unique optical properties.
Geological facts
Also known as 'Heliolite.' Historically, some legends suggest Viking navigators used sunstones (or similar calcite 'Sunstones') as a polarizing filter to locate the sun on cloudy days. It became the official state gemstone of Oregon in 1987.
Field identification & locations
Identify in the field by its distinct orange-hued metallic 'schiller' or glitter when rotated under light. Commonly found in Oregon (USA), Norway, Tanzania, and India. Collectors should look for depth of color and clarity of metallic inclusions.
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