
mineral
Sunstone
Oligoclase or Andesine (Feldspar Group), (Ca,Na)((Al,Si)4O8)
Hardness: 6–6.5 on the Mohs scale; Color: Orange, reddish-brown, or gold with metallic schiller; Luster: Vitreous to pearly; Crystal structure: Triclinic; Specific gravity: 2.62–2.65.
- 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 the Mohs scale; Color: Orange, reddish-brown, or gold with metallic schiller; Luster: Vitreous to pearly; Crystal structure: Triclinic; Specific gravity: 2.62–2.65.
Formation & geological history
Formed in igneous or metamorphic environments, often crystallizing within basaltic lava flows or pegmatites. The metallic 'glitter' is caused by tiny inclusions of copper or hematite plates following crystal planes.
Uses & applications
Primarily used as a gemstone for jewelry (cabochons and beads) and as a lapidary material for decorative objects or metaphysical collecting.
Geological facts
The optical phenomenon that gives it its sparkle is called 'aventurescence.' It was famously used by Vikings as a 'sunstone' (though this is debated with Iceland Spar) to navigate during cloudy days by detecting polarized light.
Field identification & locations
Identify by its distinctive metallic 'schiller' effect when rotated under light. Commonly found in Oregon (USA), Norway, Tanzania, and India. Collectors should look for rich color and high inclusion density.
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