mineral
Rose Quartz (Dyed)
Silicon Dioxide (SiO2) with trace impurities
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent to opaque pink (often chemically enhanced with dyes in bead form); Luster: Vitreous/Glassy; Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous/Glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent to opaque pink (often chemically enhanced with dyes in bead form); Luster: Vitreous/Glassy; Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture.
Formation & geological history
Commonly forms in magmatic pegmatites at high temperatures. These specific specimens are polished beads, likely originating from hydrothermal quartz deposits.
Uses & applications
Primarily used for jewelry, beadwork, ornamental carvings, and in the metaphysical/holistic community.
Geological facts
While natural rose quartz gets its color from microscopic inclusions of pink borosilicate, many mass-produced beads (like these) are dyed to achieve deeper pink spots or streaks, which is why the color appears blotchy.
Field identification & locations
Identify by its hardness (scratches glass) and lack of cleavage. In the field, look for pink massive quartz associated with granite or pegmatite veins.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
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