Rock Identifier
Rose Quartz (Silicon dioxide (SiO2) with trace impurities of titanium, iron, or manganese) — mineral
mineral

Rose Quartz

Silicon dioxide (SiO2) with trace impurities of titanium, iron, or manganese

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal (usually found in massive form); Cleavage: None (conchoidal fracture); Specific gravity: 2.65

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

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Physical properties

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal (usually found in massive form); Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & geological history

Formed in igneous pegmatites through the cooling and crystallization of silica-rich magma or hydrothermal fluids. Most specimens are millions of years old, dating back tovarious tectonic events throughout Earth's history.

Uses & applications

Commonly used in jewelry, decorative carvings, and ornamental objects. In the metaphysical community, it is highly valued as a 'stone of love.' Industrial use for high-quality quartz includes electronics and optics, though massive rose quartz is mostly decorative.

Geological facts

Rose quartz rarely forms visible crystal faces; it is almost always found in large, shapeless masses. High-quality specimens can exhibit 'asterism' (a star-like light effect) due to microscopic rutile inclusions.

Field identification & locations

Identify in the field by its distinct pink hue, lack of cleavage (it breaks like glass), and high hardness (it will scratch steel and glass). It is widely found in Brazil, Madagascar, South Dakota (USA), and India.