
mineral
Sunstone
Oligoclase (Plagioclase Feldspar) - (Ca,Na)(Al,Si)4O8
Hardness: 6-6.5; Color: Orange, reddish-brown, or gold with metallic flashes; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees; Specific gravity: 2.62-2.65
- Hardness
- 6-6
- Color
- Orange, reddish-brown, or gold with metallic flashes
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5; Color: Orange, reddish-brown, or gold with metallic flashes; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees; Specific gravity: 2.62-2.65
Formation & geological history
Formed in igneous rocks like basalt or rhyolite, and in pegmatites. The metallic 'schiller' effect or aventurescence is caused by tiny inclusions of copper, hematite, or goethite. Ages vary by location, often associated with Cenozoic volcanic flows.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons or faceted stones) and for lapidary carving. It is popular among crystal collectors for its unique optical properties.
Geological facts
Sunstone is the official state gemstone of Oregon, USA. The 'schiller' effect seen in these stones is a result of light reflecting off microscopic copper or hematite platelets embedded within the feldspar lattice.
Field identification & locations
Identify in the field by its distinct orange-to-pink coloration and the presence of glittering metallic reflections when tilted under light. High-quality specimens are frequently found in Oregon, Norway, India, and Tanzania.
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