mineral

Rose Quartz

Quartz (Silicon Dioxide - SiO2) with trace impurities of Titanium, Manganese, or Iron

Hardness: 7 (Mohs scale), Color: Pale pink to rose red, Luster: Vitreous to greasy, Crystal structure: Trigonal (often massive in form), Cleavage: None (conchoidal fracture), Specific gravity: 2.65

Identified March 25, 2026More mineral →

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Physical properties

Hardness: 7 (Mohs scale), Color: Pale pink to rose red, Luster: Vitreous to greasy, Crystal structure: Trigonal (often massive in form), Cleavage: None (conchoidal fracture), Specific gravity: 2.65

Formation & geological history

Formed through the crystallization of magma (igneous) or from hydrothermal veins. It typically occurs in pegmatites. These specimens can range in age from hundreds of millions to billions of years old.

Uses & applications

Used primarily in the jewelry and gemstone industry for beads, cabochons, and carvings. Also popular in the metaphysical community (thought to represent love) and as decorative stone for ornaments.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystals; it usually appears as a 'massive' lump. It is the state mineral of South Dakota. Some specimens exhibit asterism (a star-like reflection) due to rutile needle inclusions.

Field identification & locations

Identify in the field by its distinct pink hue, hardness (it scratches glass easily), and lack of cleavage. Common locations include Brazil, Madagascar, South Africa, and the United States (Maine, South Dakota).

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