
mineral
Satin Spar Selenite
Fibrous Gypsum (CaSO4·2H2O)
Hardness: 2 (soft enough to scratch with a fingernail); Color: Pearly white to translucent; Luster: Silky/Satin; Crystal Structure: Monoclinic; Specific Gravity: 2.3; Cleavage: Perfect in one direction
- Hardness
- 2 (soft enough to scratch with a fingernail)
- Color
- Pearly white to translucent
- Luster
- Silky/Satin
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Physical properties
Hardness: 2 (soft enough to scratch with a fingernail); Color: Pearly white to translucent; Luster: Silky/Satin; Crystal Structure: Monoclinic; Specific Gravity: 2.3; Cleavage: Perfect in one direction
Formation & geological history
Formed as an evaporite mineral in sedimentary environments such as saline lakes and clay beds where sea water or mineral-rich groundwater evaporates. It can range in age from millions of years old to relatively modern formations.
Uses & applications
Largely used in the metaphysical and wellness community for 'cleansing' other stones. Industrially, gypsum is used in plaster of Paris, drywall, and as a soil conditioner.
Geological facts
While commonly called Selenite in the crystal market, this specific fibrous variety is technically Satin Spar. True Selenite is transparent and platy. It is one of the softest minerals on Earth and is water-soluble over long periods of time.
Field identification & locations
Identified by its signature silky sheen and long fibrous structure. In the field, look in evaporite basins. It is extremely soft and can be easily scratched by a fingernail, which helps distinguish it from similar-looking quartz or calcite.
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sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic