
mineral
Satin Spar (Selenite)
Gypsum (Calcium Sulfate Dihydrate) - CaSO4·2H2O
AI-generated identification · may be incorrectHardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White or colorless. Luster: Pearly or silky (satin-like). Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction. Specific gravity: 2.3.
- Hardness
- 2 on Mohs scale (can be scratched by a fingernail)
- Color
- White or colorless
- Luster
- Pearly or silky (satin-like)
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Physical properties
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White or colorless. Luster: Pearly or silky (satin-like). Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction. Specific gravity: 2.3.
Formation & geological history
Formed as an evaporite mineral in sedimentary environments, typically from the evaporation of seawater or saline lake water. It can also form through the hydration of anhydrite or in hydrothermal veins.
Uses & applications
Commonly used for decorative carvings, crystal healing, and metaphysical practices. Industrially, gypsum is essential for making drywall (plasterboard), cement, and soil conditioners in agriculture.
Geological facts
While often sold and referred to as 'Selenite' in trade, this specific fibrous variety is technically Satin Spar. True Selenite is transparent and platelike. It is one of the softest minerals and is soluble in water over long periods.
Field identification & locations
Identify in the field by its extreme softness (scratched by a fingernail) and fibrous, silky appearance. Commonly found in Morocco, Mexico, and the USA (Utah/New Mexico). Collectors should avoid getting it wet.
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