
mineral
Charoite
K(Ca,Na)2Si4O10(OH,F)wH2O
Hardness: 5-6 (Mohs scale); Color: Bright lavender to deep violet/purple with swirling white, black, and orange inclusions; Luster: Vitreous to pearly/silky; Crystal Structure: Monoclinic; Cleavage: Good in three directions; Specific Gravity: 2.54-2.58.
- Hardness
- 5-6 (Mohs scale)
- Luster
- Vitreous to pearly/silky
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Physical properties
Hardness: 5-6 (Mohs scale); Color: Bright lavender to deep violet/purple with swirling white, black, and orange inclusions; Luster: Vitreous to pearly/silky; Crystal Structure: Monoclinic; Cleavage: Good in three directions; Specific Gravity: 2.54-2.58.
Formation & geological history
Formed through contact metamorphism where an alkali syenite intrusion entered limestone deposits, resulting in a unique hydrothermal chemical environment. It is exclusively found in the Murun Massif in Siberia, Russia, and is approximately 115-145 million years old.
Uses & applications
Primarily used as an ornamental stone for carvings, decorative objects, and cabochon jewelry. It is highly prized by collectors due to its rarity and unique chatoyancy.
Geological facts
Charoite was discovered in the 1940s but not described scientifically until 1978. It is named after the Chara River. It is one of the few minerals that is only found in a single location on the entire planet.
Field identification & locations
Identify by its distinctive 'swirling' or fibrous appearance and vivid purple hue. It often contains inclusions of orange Tinaksite or black Aegirine. Collectors should look for high-grade specimens with strong chatoyancy and minimal dull gray waste rock.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic