
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Pale pink to rose red, Luster: Vitreous/Glassy, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pale pink to rose red, Luster: Vitreous/Glassy, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Primary formation occurs within pegmatites (igneous) through hydrothermal processes. It forms at high temperatures deep within the Earth's crust as magma cools slowly, allowing large crystals to form.
Uses & applications
Extensively used for lapidary work including cabochons, beads, and carvings. Significant in the metaphysical market and gift industry. Lower grade material is used as an abrasive or in glassmaking.
Geological facts
Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces and is typically found in massive clusters. The color is often stable but can fade if exposed to prolonged direct sunlight.
Field identification & locations
Identify in the field by its distinct pink hue, lack of cleavage, and ability to scratch glass. Commonly found in Brazil, South Africa, Madagascar, and the United States (specifically South Dakota).
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
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)
igneous