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

Rose Quartz

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

Hardness: 7 (Mohs scale); Color: Pink to rose-red; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pink to rose-red
Luster
Vitreous to greasy
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Pink to rose-red; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed in late-stage crystallization of pegmatites, often found in hydrothermal veins. Large specimens are typically found in the core of pegmatite bodies.

Uses & applications

Used extensively in jewelry, ornamental carvings, holistic healing practices, and as a decorative landscaping stone. High-quality pieces are used for faceting.

Geological facts

Unlike other quartz varieties, Rose Quartz rarely forms large, well-defined crystals; it usually appears in massive granular form. The color can fade if left in direct sunlight for extended periods.

Field identification & locations

Identify in the field by its distinct pink hue, lack of clear crystal faces, and smooth, glass-like (conchoidal) fractures. Common in Brazil, South Africa, Madagascar, and the United States (South Dakota and Maine).