
mineral
Desert Rose
Gypsum (Calcium Sulfate Dihydrate) with Sand Inclusions, CaSO4·2H2O
AI-generated identification · may be incorrectHardness: 1.5-2.0 on Mohs scale; Color: Tan, brown, or sandy-cream; Luster: Pearly to earthy; Crystal Structure: Monoclinic (rosette habit); Cleavage: Perfect in one direction; Specific Gravity: 2.3
- Hardness
- 1
- Color
- Tan, brown, or sandy-cream
- Luster
- Pearly to earthy
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Physical properties
Hardness: 1.5-2.0 on Mohs scale; Color: Tan, brown, or sandy-cream; Luster: Pearly to earthy; Crystal Structure: Monoclinic (rosette habit); Cleavage: Perfect in one direction; Specific Gravity: 2.3
Formation & geological history
Forms in arid sandy conditions through the evaporation of shallow salt basins or groundwater. These crystals precipitate as bladed clusters that incorporate surrounding sand grains.
Uses & applications
Primarily used as a decorative collector's specimen, in metaphysical practices, and occasionally in lapidary work or as a source of gypsum for plaster.
Geological facts
The unique 'petals' are actually flattened crystals that grow outward in a radiating pattern. While mostly gypsum, some desert roses are formed from barite, which is much heavier.
Field identification & locations
Identified by its distinctive rose-like shape and sandy texture. It is very soft and can often be scratched with a fingernail. Commonly found in the Sahara Desert, Mexico, and the Southwestern United States.
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