
mineral
Desert Rose
Gypsum (Calcium Sulfate Dihydrate) - CaSO4·2H2O
Hardness: 2.0 (Mohs scale); Color: Tan, sandy brown, or white; Luster: Pearly to earthy; Crystal Structure: Monoclinic; Cleavage: Good in one direction but brittle; Specific Gravity: 2.3
- Hardness
- 2
- Color
- Tan, sandy brown, or white
- Luster
- Pearly to earthy
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Physical properties
Hardness: 2.0 (Mohs scale); Color: Tan, sandy brown, or white; Luster: Pearly to earthy; Crystal Structure: Monoclinic; Cleavage: Good in one direction but brittle; Specific Gravity: 2.3
Formation & geological history
Formed in arid sandy conditions through the evaporation of shallow salt basins. The crystals form circular patterns of flat plates that incorporate sand grains during growth. Most are from the Quaternary period.
Uses & applications
Primarily used as a decorative collector's specimen, in metaphysical practices, and occasionally as a source of gypsum for plaster.
Geological facts
The unique 'rose' shape is formed by the twinning of crystals. It is the official state rock of Oklahoma where it is found in the Garber Sandstone. It feels sandy to the touch because of the trapped sediment.
Field identification & locations
Identified by its distinctive rosette shape and soft, sandy texture. Commonly found in North Africa (Sahara), Mexico (Chihuahua), and the USA (Oklahoma and Arizona). Collectors should handle carefully as they are very fragile.
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