Rock Identifier
Rose Quartz (Silicon Dioxide (SiO2) with trace impurities of titanium, iron, or manganese) — mineral
mineral

Rose Quartz

Silicon Dioxide (SiO2) with trace impurities of titanium, iron, or manganese

Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous (glass-like); Crystal structure: Hexagonal (Trigonal); Cleavage: Indistinct (conchoidal fracture); Specific gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pale pink to rose red
Luster
Vitreous (glass-like)
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous (glass-like); Crystal structure: Hexagonal (Trigonal); Cleavage: Indistinct (conchoidal fracture); Specific gravity: 2.65

Formation & geological history

Formed in pegmatites, high-temperature hydrothermal veins, and igneous rocks through the cooling and crystallization of silica-rich fluids. It does not typically form well-defined crystal faces, usually appearing in massive crystalline form.

Uses & applications

Commonly used in jewelry (beads, cabochons, carvings), decorative sculptures, crystal healing/metaphysical practices, and as a low-cost ornamental stone in landscaping or home decor.

Geological facts

Unlike other quartz varieties, Rose Quartz rarely forms large individual crystals; it is almost always found in massive form. The pink color is often caused by microscopic inclusions of fibrous mineral related to dumortierite.

Field identification & locations

Identify in the field by its characteristic pink hue, high hardness (will scratch glass), and lack of cleavage. Common locations include Brazil, South Africa, India, and the United States (South Dakota and Maine). For collectors, look for deep color saturation and translucency.