
mineral
Rose Quartz
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: Vitreous; Crystal structure: Trigonal (Hexagonal system); Cleavage: No true cleavage, conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- pale pink to rose red
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: Vitreous; Crystal structure: Trigonal (Hexagonal system); Cleavage: No true cleavage, conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed in high-temperature silica-rich environments, usually found in the cores of pegmatites formed during the late stage of magma crystallization. Often millions of years old.
Uses & applications
Commonly used in jewelry, ornamental carving, and decorative gemstones. In industry, high-purity quartz is used for glassware and electronics, though rose quartz specifically is prized primarily for aesthetics.
Geological facts
The pink color is attributed to microscopic inclusions of fibrous dumortierite or trace amounts of titanium, iron, or manganese. Unlike most quartz, it rarely forms well-defined crystals.
Field identification & locations
Identify in the field by its distinct pink translucent color, glassy luster, and ability to scratch glass. Found in abundance in Brazil, South Africa, Madagascar, and the United States (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
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