
mineral
Rose Quartz with Hematite inclusions
Silicon Dioxide (SiO2) with Fe2O3 inclusions
Hardness: 7 on Mohs scale; Color: Pale pink to rose red with reddish-brown streaks; Luster: Vitreous 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 with reddish-brown streaks
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale pink to rose red with reddish-brown streaks; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in pegmatites and hydrothermal veins through the cooling of silica-rich magma or precipitation from hot mineral-rich fluids. The pink hue is attributed to traces of titanium, iron, or manganese, while the rust-colored spots are iron oxide (hematite) inclusions.
Uses & applications
Used in jewelry (cabochons, beads), decorative carvings, lapidary arts, and highly valued in the 'metaphysical' market as a 'love stone.' Also used in industrial glass production.
Geological facts
Rose quartz is rarely found as individual crystals and usually occurs in massive form. The reddish-brown staining in this specimen is likely 'earthy' hematite, a common companion mineral. It loses its pink color if exposed to too much direct sunlight over time due to UV radiation affecting the mineral's color centers.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and characteristic pinkish hue. Commonly found in Brazil, South Africa, Madagascar, and the United States (South Dakota). Look for it in granitic pegmatite environments.
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