
mineral
Pink Quartz (likely dyed)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Vivid pink to magenta, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Vivid pink to magenta, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Specific Gravity: 2.65
Formation & geological history
Formed through crystallization of silica-rich hydrothermal fluids or within igneous pegmatites. Note: This specific intensity of pink in a uniform tumbled stone often suggests a standard quartz or chalcedony that has undergone a dyeing process.
Uses & applications
Used primarily for metaphysical purposes, decorative home decor, aquarium gravel, inexpensive costume jewelry, and as pocket stones for collectors.
Geological facts
Natural rose quartz usually has a softer, pastel pink hue caused by trace amounts of titanium, iron, or manganese. Highly saturated or neon pinks are almost universally the result of artificial dye being injected into the micro-fissures of a lower-grade quartz.
Field identification & locations
Identify by its hardness (will scratch glass) and consistent waxy or glassy luster. Field identification involves looking for crystal habits in veins; dyed versions are identified by dye concentrations in cracks.
More like this
Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary