mineral
Rose Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectMohs hardness of 7, pale pink to rose red color, vitreous to greasy luster, trigonal crystal system, indistinct cleavage, specific gravity of 2.65
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Physical properties
Mohs hardness of 7, pale pink to rose red color, vitreous to greasy luster, trigonal crystal system, indistinct cleavage, specific gravity of 2.65
Formation & geological history
Forms primarily in pegmatites and hydrothermal veins through the crystallization of silica-rich magma with trace amounts of titanium, iron, or manganese which cause the pink color
Uses & applications
Used widely in tumbled stones, gemstone jewelry, decorative carvings, and as a popular specimen for mineral collectors
Geological facts
Ancient civilizations such as the Assyrians and Romans used rose quartz as early as 800-600 BC for jewelry and seals. Its pink color is often attributed to microscopic fibers of pink dumortierite
Field identification & locations
Identified by its distinct pink coloration and conchoidal fracture. Commonly found in Brazil, Madagascar, South Africa, and the United States
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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