mineral
Sunstone (Orthoclase Feldspar variant)
Orthoclase (KAlSi3O8) with inclusions
AI-generated identification · may be incorrectHardness: 6.0-6.5 on Mohs scale. Color: Peach, orange, or reddish-brown. Luster: Vitreous to pearly. Crystal Structure: Monoclinic or Triclinic. Notable for 'aventurescence,' a metallic glitter caused by tiny plate-like inclusions.
- Hardness
- 6
- Color
- Peach, orange, or reddish-brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6.0-6.5 on Mohs scale. Color: Peach, orange, or reddish-brown. Luster: Vitreous to pearly. Crystal Structure: Monoclinic or Triclinic. Notable for 'aventurescence,' a metallic glitter caused by tiny plate-like inclusions.
Formation & geological history
Formed in igneous environments, particularly in pegmatites and lava flows. The unique optical effect is created by the exsolution of copper or hematite crystals during the cooling of molten rock over thousands of years.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons and beads). It is also a popular specimen for crystal collectors and sometimes used in decorative carvings.
Geological facts
Oregon Sunstone is unique because it contains microscopic inclusions of elemental copper rather than hematite, resulting in colors ranging from clear to deep red and green. It was designated as the state gemstone of Oregon in 1987.
Field identification & locations
Identify in the field by its distinct peach-to-orange hue and the characteristic golden or reddish shimmer when rotated under light. Commonly found in Oregon (USA), Norway, Tanzania, and India.
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