
mineral
Satin Spar (often marketed as Selenite)
Gypsum (Calcium Sulfate Dihydrate) - CaSO4·2H2O
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White or pearly white. Luster: Pearly to silky (satin-like). Crystal structure: Monoclinic, often fibrous. Cleavage: Perfect one-way cleavage. Specific Gravity: 2.3.
- Hardness
- 2 on Mohs scale (can be scratched by a fingernail)
- Color
- White or pearly white
- Luster
- Pearly to silky (satin-like)
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Physical properties
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White or pearly white. Luster: Pearly to silky (satin-like). Crystal structure: Monoclinic, often fibrous. Cleavage: Perfect one-way cleavage. Specific Gravity: 2.3.
Formation & geological history
Formed as an evaporite mineral in sedimentary environments, such as ancient seabeds and salt flats where mineral-rich water evaporates. It can form in various geological ages where saline lakes or marine basins were present.
Uses & applications
Primarily used in the metaphysical and spiritual industry for 'cleansing' other stones. Gypsum is used industrially in drywall (plasterboard), cement, and as a soil conditioner (land plaster).
Geological facts
While commonly sold as 'Selenite,' this fibrous white variety is technically 'Satin Spar.' True Selenite is transparent and forms flat, window-like plates. This specimen is shaped into a 'skyscraper' or 'tower' form, which is a popular decorative cut.
Field identification & locations
Identify in the field by its extreme softness (scratches with a nail) and its fibrous, silky luster. Commonly found in Morocco, Mexico, and the USA (Utah/New Mexico). Note: It is water-soluble over time and should not be soaked.
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