Rock Identifier
Charoite (Charoite; (K,Sr,Ba,Ca)15-16(Na,Ca)8(Si,Al)24O60(OH,F)4·nH2O) — metamorphic
metamorphic

Charoite

Charoite; (K,Sr,Ba,Ca)15-16(Na,Ca)8(Si,Al)24O60(OH,F)4·nH2O

Hardness: 5.0-6.0 on Mohs scale; Color: Bright violet to deep purple with white or black swirls/inclusions; Luster: Vitreous to pearly/silky; Crystal Structure: Monoclinic; Cleavage: Good; Specific Gravity: 2.54-2.58.

Hardness
5
Luster
Vitreous to pearly/silky
Identified More metamorphic

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Physical properties

Hardness: 5.0-6.0 on Mohs scale; Color: Bright violet to deep purple with white or black swirls/inclusions; Luster: Vitreous to pearly/silky; Crystal Structure: Monoclinic; Cleavage: Good; Specific Gravity: 2.54-2.58.

Formation & geological history

Formed via contact metamorphism through the alteration of limestone by an alkaline syenite intrusion. It is associated with the Murun Massif in the Chara River area, Yakutia, Russia, and is typically dated to the Mesozoic era.

Uses & applications

Primarily used as a lapidary stone for high-end jewelry (cabochons, beads), decorative carvings, and as a sought-after collector's specimen due to its rarity.

Geological facts

It was only officially discovered in 1978. It is renowned for its chatoyancy—a silky, shimmering optical effect created by its fibrous structure. Despite its appearance, the purple color is attributed to manganese impurities.

Field identification & locations

Found exclusively in one location: the Murun Massif in Siberia, Russia. In the field, its distinct 'swirling' lavender pattern and fibrous texture are diagnostic. Look for black Aegirine-augite or orange Tinaksite inclusions to confirm authenticity.