
mineral
Satin Spar (often marketed as Selenite)
Gypsum (CaSO4·2H2O)
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Silky or pearly. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction.
- Hardness
- 2 on Mohs scale (can be scratched by a fingernail)
- Color
- White, pearly, or translucent
- Luster
- Silky or pearly
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Physical properties
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Silky or pearly. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction.
Formation & geological history
Formed as an evaporite mineral in sedimentary environments, typically from the evaporation of ancient seawater or saline lakes. Most commercial specimens are from Morocco.
Uses & applications
Commonly used in the metaphysical and gemstone trade as decorative towers, wands, and bowls. Industrial gypsum is used for plaster, drywall, and fertilizer.
Geological facts
While commonly called 'Selenite' in the crystal trade, this fibrous variety is technically 'Satin Spar.' True Selenite is transparent and plate-like. It is extremely water-soluble and will dissolve if left in water for long periods.
Field identification & locations
Identify by its extreme softness and fibrous, silky appearance. It is very common in arid regions like Morocco, Mexico, and the USA (Utah/New Mexico). Collectors should avoid getting it wet.
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