
mineral
Desert Rose
Gypsum (variety Selenite) or Barite: CaSO4 · 2H2O
AI-generated identification · may be incorrectHardness: 2 on Mohs scale; Color: Tan, beige, sandy; Luster: Pearly to dull; Crystal Structure: Monoclinic (tabular blades in rosette clusters); Cleavage: Perfect in one direction; Specific Gravity: 2.3
- Hardness
- 2 on Mohs scale
- Color
- Tan, beige, sandy
- Luster
- Pearly to dull
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Physical properties
Hardness: 2 on Mohs scale; Color: Tan, beige, sandy; Luster: Pearly to dull; Crystal Structure: Monoclinic (tabular blades in rosette clusters); Cleavage: Perfect in one direction; Specific Gravity: 2.3
Formation & geological history
Formed in arid sandy conditions through the evaporation of salt-rich water basins. The crystals incorporate sand grains as they grow, creating the characteristic rose-like structure. They are typically found in Saharan or Southwestern US desert regions.
Uses & applications
Primarily used as decorative specimens, for mineral collecting, and in spiritual/metaphysical practices. Gypsum is also industrially used for plaster and drywall.
Geological facts
Desert roses are not a single mineral but a shape that occurs in sulfate minerals like gypsum or barite. The 'petals' are actually flattened crystals that bloom outward from a central point.
Field identification & locations
Identify by its unique rose-like petal structure and sandy texture. It can be scratched with a fingernail (if gypsum). Found commonly in the Sahara Desert, Mexico, and Oklahoma.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous