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); Cleavage: None (Conchoidal fracture); 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); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in late-stage igneous crystallization within pegmatites; cooling of hydrothermal solutions at low temperatures. It is found in deposits ranging from Precambrian to more recent geological ages.

Uses & applications

Commonly used in lapidary work for cabochons, carvings, beads, and tumbled stones. Also used as a decorative material in home décor and highly valued in some spiritual communities.

Geological facts

Unlike اکثر varieties of quartz, rose quartz generally occurs in massive form rather than well-formed crystal points. Some specimens exhibit 'asterism' (a star-like effect) when cut as cabochons due to tiny rutile inclusions.

Field identification & locations

Identify in the field by its distinct translucent pink color and lack of crystal faces. It is frequently found in Brazil, South Africa, Madagascar, and the United States (South Dakota and New England).