
mineral
Tumbled pink quartz (likely rose quartz)
Quartz, silicon dioxide (SiO₂), commonly called rose quartz
AI-generated identification · may be incorrectMohs hardness 7; pale pink to lavender-pink, translucent to opaque, vitreous luster, and typically massive rather than visibly crystalline. No obvious cleavage; conchoidal fracture; the rounded shape is from tumbling and polishing.
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Physical properties
Mohs hardness 7; pale pink to lavender-pink, translucent to opaque, vitreous luster, and typically massive rather than visibly crystalline. No obvious cleavage; conchoidal fracture; the rounded shape is from tumbling and polishing.
Formation & geological history
Forms mainly in silica-rich pegmatites and hydrothermal veins, with pink color caused by microscopic inclusions or trace elements. It is generally Precambrian to younger, depending on its host deposit.
Uses & applications
Used as an inexpensive ornamental stone, cabochon, bead, carving material, and decorative aggregate; less commonly used industrially than clear quartz. Typical tumbled pieces have modest collector value.
Geological facts
Rose quartz is commonly cloudy and massive, unlike rare transparent pink quartz crystals. Color may fade with prolonged intense light or heat.
Field identification & locations
Common in Brazil, Madagascar, South Africa, India, and the United States. Identify by its pink color, glassy luster, hardness, and inability to scratch it with a steel knife; definitive identification may require testing because pink calcite or dyed stone can look similar.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary