Rock Identifier
Satin Spar (often marketed as Selenite) (Gypsum (CaSO4·2H2O)) — mineral
mineral

Satin Spar (often marketed as Selenite)

Gypsum (CaSO4·2H2O)

Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Silky or pearly. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction.

Hardness
2 on Mohs scale (can be scratched by a fingernail)
Color
White, pearly, or translucent
Luster
Silky or pearly
Identified More mineral

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Physical properties

Hardness: 2 on Mohs scale (can be scratched by a fingernail). Color: White, pearly, or translucent. Luster: Silky or pearly. Crystal structure: Monoclinic, typically fibrous. Cleavage: Perfect in one direction.

Formation & geological history

Formed as an evaporite mineral in sedimentary environments, typically from the evaporation of ancient seawater or saline lakes. Most commercial specimens are from Morocco.

Uses & applications

Commonly used in the metaphysical and gemstone trade as decorative towers, wands, and bowls. Industrial gypsum is used for plaster, drywall, and fertilizer.

Geological facts

While commonly called 'Selenite' in the crystal trade, this fibrous variety is technically 'Satin Spar.' True Selenite is transparent and plate-like. It is extremely water-soluble and will dissolve if left in water for long periods.

Field identification & locations

Identify by its extreme softness and fibrous, silky appearance. It is very common in arid regions like Morocco, Mexico, and the USA (Utah/New Mexico). Collectors should avoid getting it wet.