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, opaque to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None, exhibits conchoidal fracture; Specific Gravity: 2.65

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

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Physical properties

Hardness: 7 on Mohs scale; Color: Pale pink to rose red, opaque to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None, exhibits conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Rose quartz forms in pegmatites and hydrothermal veins, typically at high temperatures. Its pink color is often attributed to microscopic inclusions of dumortierite, though some research suggests titanium, iron, or manganese impurities could also be responsible. It usually forms in large masses within igneous and metamorphic rocks, making well-formed crystal points rare. Geological age varies greatly depending on the specific deposit, ranging from hundreds of millions to billions of years old.

Uses & applications

Predominantly used for ornamental purposes, including beads, cabochons, carvings, and tumbled stones. Also popular in jewelry (pendants, earrings, bracelets) and as decorative items for homes and offices. In alternative healing practices, it is associated with love and emotional healing.

Geological facts

Rose quartz is often called the 'love stone' and is believed to promote unconditional love, self-love, friendship, and deep inner healing. Despite being a variety of quartz, large, transparent single crystals are extremely rare; it typically occurs in massive form. The color can fade with prolonged exposure to sunlight.

Field identification & locations

In the field, rose quartz can be identified by its distinctive pink color, glassy to greasy luster, and hardness (it can scratch glass). It typically lacks crystal faces and appears as irregular masses. Common localities include Brazil (Minas Gerais), South Dakota (USA - State Mineral), Madagascar, India, and Sri Lanka. When identifying, look for its characteristic pale to deep pink hue and its translucent to opaque nature. It can be distinguished from other pink minerals by its hardness and lack of cleavage.