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

Satin Spar (Satin Spar Selenite)

Gypsum (CaSO4·2H2O)

Hardness: 2 on Mohs scale (can be scratched by fingernail). Color: White or pearly. Luster: Silky/satin-like. Crystal Structure: Monoclinic, typically found in fibrous, parallel bundles. Cleavage: Perfect in one direction.

Hardness
2 on Mohs scale (can be scratched by fingernail)
Color
White or pearly
Luster
Silky/satin-like
Identified More mineral
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Physical properties

Hardness: 2 on Mohs scale (can be scratched by fingernail). Color: White or pearly. Luster: Silky/satin-like. Crystal Structure: Monoclinic, typically found in fibrous, parallel bundles. Cleavage: Perfect in one direction.

Formation & geological history

Formed as an evaporite mineral in sedimentary environments, often resulting from the evaporation of seawater or in hydrothermal veins and clay beds. Specimens like this are frequently from the Cretaceous period.

Uses & applications

Commonly used in holistic and metaphysical practices (often mislabeled as 'selenite'), as decorative ornaments, and commercially in the production of plaster of Paris, drywall, and soil fertilizers.

Geological facts

While often sold as 'Selenite', true Selenite is the transparent variety of gypsum. Satin Spar is the fibrous variety shown here. It is highly soluble in water and should not be soaked. The world's largest gypsum crystals are found in the Naica Mine in Mexico.

Field identification & locations

Identify in the field by its extreme softness (scratches with a thumbnail) and its fibrous, silky luster. Common locations include Morocco, Mexico, USA (Utah), and various desert evaporite basins.