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); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Pale pink to rose red
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in late-stage crystallization of pegmatites (igneous rocks) and in hydrothermal veins. Because it forms at high temperatures without defined external crystal faces, it is typically found in massive chunks rather than individual crystals.

Uses & applications

Primary use is decorative, including lapidary work (cabochons, beads, carvings) and landscaping. It is also highly popular in the metaphysical and crystal collecting communities.

Geological facts

Unlike other varieties of quartz like Amethyst or Citrine, Rose Quartz almost never forms well-terminated crystals; it is almost always found in massive form. The color is sensitive to light and can fade if left in direct sunlight for long periods.

Field identification & locations

Identify in the field by its distinct pink hue, lack of cleavage, and ability to scratch glass (hardness of 7). It is commonly found in Brazil, Madagascar, South Dakota (USA), and India. Collectors value specimens with deep pink color and high translucency.