
mineral
Desert Rose
Gypsum (CaSO4·2H2O) or Baryte (BaSO4) rosette
Hardness: 2 on Mohs scale (Gypsum) or 3-3.5 (Baryte). Color: Tan, beige, or sandy brown. Luster: Pearly to dull. Crystal structure: Monoclinic or Orthorhombic blades. Cleavage: Perfect in one direction.
- Hardness
- 2 on Mohs scale (Gypsum) or 3-3
- Color
- Tan, beige, or sandy brown
- Luster
- Pearly to dull
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Physical properties
Hardness: 2 on Mohs scale (Gypsum) or 3-3.5 (Baryte). Color: Tan, beige, or sandy brown. Luster: Pearly to dull. Crystal structure: Monoclinic or Orthorhombic blades. Cleavage: Perfect in one direction.
Formation & geological history
Formed in arid, sandy environments through the evaporation of salt-rich water. As the water evaporates, minerals crystallize in circular, bladed patterns that incorporate surrounding sand grains. They can form over several hundred to thousands of years.
Uses & applications
Primary use is as a collector's specimen or decorative item. In technical forms, gypsum is used in plaster, drywall, and fertilizer, while baryte is used in drilling fluids.
Geological facts
Desert roses are unique because they are technically pseudomorphs or crystal clusters that trap sand inside them, making them look like petrified flowers. Saharan specimens from Algeria and Tunisia are particularly famous.
Field identification & locations
Identify by its distinctive rose-like cluster of flat blades and sandy texture. It is often found in desert regions with high evaporation rates such as Chihuahua (Mexico), the Sahara, or the Southwestern United States.
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