
mineral
Rose quartz
Quartz (SiO₂), pink variety
AI-generated identification · may be incorrectHardness 7 Mohs; pale pink, translucent to semi-transparent, with a vitreous luster and irregular fracture. It is typically massive rather than visibly well-crystallized and has no cleavage; density is about 2.65 g/cm³.
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Physical properties
Hardness 7 Mohs; pale pink, translucent to semi-transparent, with a vitreous luster and irregular fracture. It is typically massive rather than visibly well-crystallized and has no cleavage; density is about 2.65 g/cm³.
Formation & geological history
Forms mainly in granite-related pegmatites and hydrothermal veins when silica-rich fluids crystallize; its pink color commonly results from trace inclusions or defects. Specimens range from Precambrian to younger geologic ages.
Uses & applications
Used for carvings, cabochons, beads, decorative stone, and inexpensive metaphysical or mineral-collection pieces; rarely used as an architectural stone.
Geological facts
Rose quartz is distinct from pink crystalline quartz varieties that may owe color to irradiation or trace elements. The pictured rough, translucent pink material is consistent with massive rose quartz.
Field identification & locations
Identify by its pink color, glassy luster, lack of cleavage, and quartz hardness; it should scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Madagascar, South Africa, India, and the United States.
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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