
mineral
Satin Spar (Selenite)
Gypsum (Calcium Sulfate Dihydrate) - CaSO4·2H2O
AI-generated identification · may be incorrectHardness: 2 on the Mohs scale (can be scratched by a fingernail). Color: White or transparent with a pearly or silky luster. Crystal structure: Monoclinic with long, fibrous parallel crystals. Cleavage: Perfect in one direction. Specific gravity: 2.3.
- Hardness
- 2 on the Mohs scale (can be scratched by a fingernail)
- Color
- White or transparent with a pearly or silky luster
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Physical properties
Hardness: 2 on the Mohs scale (can be scratched by a fingernail). Color: White or transparent with a pearly or silky luster. Crystal structure: Monoclinic with long, fibrous parallel crystals. Cleavage: Perfect in one direction. Specific gravity: 2.3.
Formation & geological history
Formed as an evaporite mineral in sedimentary environments, typically where ancient seawater has evaporated across many geological ages, from the Permian to the present. Often found in clay beds or near hot springs.
Uses & applications
Primarily used for decorative purposes, crystal healing, and as metaphysical 'cleansing' wands. Industrial gypsum is used for drywall, plaster, and as a soil conditioner (fertilizer).
Geological facts
While commonly sold as 'Selenite,' this fibrous variety is technically Satin Spar. True Selenite is transparent and plate-like. It is extremely water-soluble; soaking this specimen in water will cause it to eventually dissolve or lose its luster.
Field identification & locations
Identify in the field by its extreme softness and fibrous, 'cat's eye' silky chatoyancy. It is commonly found in Morocco, Mexico (Naica Mine), and the USA (Utah and New Mexico). Collectors should look for the characteristic 'fiber optic' effect when light passes through the side.
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