
mineral
Satin Spar (Gypsum)
Calcium Sulfate Dihydrate (CaSO4·2H2O)
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Pearly to silky. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction, yielding thin sheets or fibers.
- Hardness
- 2 on Mohs scale (can be scratched by a fingernail)
- Color
- White, pearly, or translucent
- Luster
- Pearly to silky
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Physical properties
Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Pearly to silky. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction, yielding thin sheets or fibers.
Formation & geological history
Formed as an evaporite mineral in sedimentary environments, typically where seawater or saline lake water evaporates. It can also form through the hydration of anhydrite or in hydrothermal veins.
Uses & applications
Used in the manufacture of wallboard (drywall), cement, and plaster of Paris. In its fibrous 'satin spar' form, it is popular for ornamental carvings, meditation stones, and metaphysical collecting.
Geological facts
Satin spar is often mislabeled as 'selenite' in the gemstone market; while both are gypsum, selenite is the transparent, plate-like variety, while satin spar is the fibrous, silky variety. It is so soft that it can be easily carved with simple hand tools.
Field identification & locations
Identify in the field by its extreme softness (scratch with a fingernail) and its distinctive silky, fibrous appearance that reflects light in a 'cat's eye' effect. Commonly found in desert regions like Morocco, the USA (Utah/New Mexico), and Mexico.
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