
mineral
Tumbled rose quartz
Quartz, silicon dioxide (SiO₂), pink variety
AI-generated identification · may be incorrectMohs hardness 7; pale pink, translucent, vitreous luster, and trigonal crystal structure. The pictured piece is tumbled and polished; quartz has no cleavage and uneven to conchoidal fracture.
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Physical properties
Mohs hardness 7; pale pink, translucent, vitreous luster, and trigonal crystal structure. The pictured piece is tumbled and polished; quartz has no cleavage and uneven to conchoidal fracture.
Formation & geological history
Rose quartz forms in silica-rich pegmatites and other quartz-bearing rocks, commonly crystallizing as veins or massive aggregates during igneous activity. Its age varies with the host deposit.
Uses & applications
Used for jewelry, carvings, beads, and decorative objects; quartz is also important in glassmaking and electronics.
Geological facts
Its pink color is associated with trace elements or microscopic inclusions; massive rose quartz rarely forms clear, well-defined crystals.
Field identification & locations
Common sources include Brazil, Madagascar, India, and South Dakota. Identify it by its pink hue, glassy polish, and hardness; a small tumbled piece typically sells for about $2–$10.
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Sandstone (with potential mineral staining/concretions)
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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)
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