
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous (glassy)
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of magma in igneous pegmatites or in hydrothermal veins. The pink color is attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite.
Uses & applications
Commonly used in lapidary work for cabochons, beads, and carvings. High-quality specimens are used in jewelry. Also widely used as a decorative stone in landscaping and crystal healing practices.
Geological facts
Unlike other varieties of quartz, rose quartz rarely forms well-defined external crystal faces. The largest deposits are found in Brazil, but it was also the official state mineral of South Dakota for many years.
Field identification & locations
Identify in the field by its distinct pink hue and lack of visible crystal faces (anhedral). Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota). It will scratch glass easily.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral