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 March 18, 2026More 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 in pegmatites (igneous) through hydrothermal processes. Most specimens are millions of years old, originating from the Precambrian or Paleozoic eras.

Uses & applications

Used primarily in lapidary work for jewelry (cabochons, beads), decorative carvings, spiritual/metaphysical healing practices, and as ornamental stone in interior design.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces and is usually found as massive lumps. The color is often stable but can fade if exposed to prolonged direct sunlight.

Field identification & locations

Identified by its distinctive pink color and lack of transparency (it is usually translucent or cloudy). Major deposits are located in Brazil (Minas Gerais), Madagascar, and South Dakota (USA). Collectors look for deep saturation of color and clarity.

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