
mineral
Satin Spar Selenite
Gypsum (Calcium Sulfate Dihydrate, CaSO4·2H2O)
Hardness: 2 on Mohs scale (can be scratched by a fingernail); Color: Translucent white with a pearly or silky sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect; Specific gravity: 2.3
- Hardness
- 2 on Mohs scale (can be scratched by a fingernail)
- Color
- Translucent white with a pearly or silky sheen
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2 on Mohs scale (can be scratched by a fingernail); Color: Translucent white with a pearly or silky sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect; Specific gravity: 2.3
Formation & geological history
Forms primarily as an evaporite mineral in sedimentary environments such as saline lakes, lagoons, and deep-sea basins where calcium-rich waters evaporate. It can also form through the oxidation of sulfides in hydrothermal veins.
Uses & applications
Used in the manufacture of plaster of Paris, drywall (gypsum board), and fertilizers. In the spiritual and mineral collecting communities, it is popular for decorative carvings, palm stones, and wands due to its optical properties.
Geological facts
In its common silky fibrous form, it is known as 'satin spar.' It is so soft that it can be scratched by a human fingernail, which is a primary diagnostic test for identifying it against similar-looking minerals like calcite or quartz.
Field identification & locations
Identify in the field by its characteristic silky luster and extreme softness. It is commonly found in Morocco, Mexico, and the United States (Utah and New Mexico). Collectors should avoid getting it wet, as it is slightly soluble in water over time.
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