mineral

Rose Quartz (Dyed)

Silicon Dioxide (SiO2) with trace impurities

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.

Hardness: 7 on Mohs scale
Luster: Vitreous/Glassy

Identified June 9, 2026More mineral →

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Physical properties

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.

Other mineral specimens

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Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Schist

Metamorphic

Epidote

Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)

metamorphic

Nephrite Jade

Nephrite

Mineral/Rock

Banded Gneiss (River Rock/Pebble)

Gneiss (specifically a banded variety often found as a river rock)

Metamorphic Rock

Biotite Schist

Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]

metamorphic