Rock Identifier
Rose Quartz (Rose Quartz (SiO2)) — Mineral
Mineral

Rose Quartz

Rose Quartz (SiO2)

Hardness: 7 on Mohs scale. Color: Pale pink to rose red; often translucent to opaque. Luster: Vitreous to greasy. Crystal Structure: Trigonal (typically massive, anhedral habits). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

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

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Physical properties

Hardness: 7 on Mohs scale. Color: Pale pink to rose red; often translucent to opaque. Luster: Vitreous to greasy. Crystal Structure: Trigonal (typically massive, anhedral habits). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Rose Quartz forms as a late-stage mineral in pegmatites and hydrothermal veins, typically from the cooling of silica-rich solutions. It can also be found in igneous and metamorphic rocks. Its distinctive pink color is believed to be caused by microscopic inclusions of dumortierite, a pink borosilicate mineral, or possibly by irradiation and trace amounts of titanium, iron, or manganese, or a combination of these factors. Geological Age: Varies depending on formation, common in many ancient igneous and metamorphic formations worldwide.

Uses & applications

Rose Quartz is widely used in jewelry (beads, cabochons, carvings) due to its attractive color and reasonable hardness. It's also used for ornamental objects, sculptures, and as tumbled stones. In metaphysical practices, it is associated with love, compassion, and emotional healing.

Geological facts

Rose Quartz is one of the most well-known and popular varieties of quartz. It rarely forms distinct crystals; instead, it usually occurs in massive form. The finest quality Rose Quartz, with vibrant color and good translucency, is highly prized. Historically, ancient civilizations believed it had healing properties and used it in talismans and amulets. The source of the pink color was a mystery for a long time, with various theories proposed.

Field identification & locations

To identify in the field, look for its characteristic pink color (ranging from very pale to medium-pink), its glassy to greasy luster, and its hardness (it will scratch glass). It typically occurs in massive, anhedral form, often as irregular chunks or veins within pegmatite matrices. Common locations include Brazil (especially Minas Gerais, a major source), South Africa, India, Madagascar, and the United States (Maine, South Dakota, California). For collectors, look for good color saturation and translucency. It's generally non-fluorescent under UV light.