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 on Mohs scale; Color: pale pink to rose red; Luster: vitreous (glassy) to greasy; Crystal Structure: Hexagonal (Trigonal), though rarely forms visible crystals; Cleavage: none; Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
pale pink to rose red
Luster
vitreous (glassy) to greasy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: vitreous (glassy) to greasy; Crystal Structure: Hexagonal (Trigonal), though rarely forms visible crystals; Cleavage: none; Specific Gravity: 2.65.

Formation & geological history

Formed in high-temperature silica-rich environments, typically in pegmatites (igneous) but can also be found in hydrothermal veins. It can be found in formations dating from the Precambrian to much younger geological eras.

Uses & applications

Extensively used in lapidary work for cabochons, beads, and carvings. Also popular in the metaphysical community and used as an ornamental stone in interior design and landscaping.

Geological facts

Unlike typical quartz, rose quartz rarely forms external crystal faces and is usually found as massive lumps. The pink color is often attributed to microscopic inclusions of a fibrous pink mineral-like dumortierite within the quartz matrix.

Field identification & locations

Identify in the field by its distinct pink hue, lack of cleavage (conchoidal fracture), and ability to scratch glass easily. Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota). To identify, look for the 'greasy' appearance on fractured surfaces.