Rock Identifier
Rose Quartz (Silicon dioxide (SiO2)) — mineral
mineral

Rose Quartz

Silicon dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous to greasy; Crystal Structure: Trigonal (often occurs in massive form); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Pale pink to rose red
Luster
Vitreous to greasy
Identified More mineral
Explore Rose Quartz in the encyclopedia →

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 to greasy; Crystal Structure: Trigonal (often occurs in massive form); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Forms in late-stage crystallization of pegmatites (igneous) at high temperatures. The pink color is generally attributed to microscopic inclusions of fibrous dumortierite or similar minerals. Most deposits are millions of years old.

Uses & applications

Used extensively in jewelry, ornamental carvings, lapidary arts, and as a popular collectable specimen for metaphysical practitioners.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces; it is almost always found in large, shapeless masses. Large amounts are found in Brazil and Madagascar.

Field identification & locations

Identify by its characteristic pink hue and ability to scratch glass. It is common in pegmatites. Collectors should look for deep color saturation and clarity, though most specimens are translucent.