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

Rose Quartz

Quartz (SiO₂), variety Rose Quartz

Hardness: 7 on the Mohs scale. Color: Often pink to reddish-pink due to manganese impurities. Can also be colorless, yellow, blue, or green. Luster: Vitreous to sub-vitreous. Crystal Structure: Hexagonal (trigonal), often found as prismatic crystals, but also massive, granular, or compact. Cleavage: Indistinct.…

Hardness
7 on the Mohs scale
Color
Often pink to reddish-pink due to manganese impurities
Luster
Vitreous to sub-vitreous
Identified More mineral

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Physical properties

Hardness: 7 on the Mohs scale. Color: Often pink to reddish-pink due to manganese impurities. Can also be colorless, yellow, blue, or green. Luster: Vitreous to sub-vitreous. Crystal Structure: Hexagonal (trigonal), often found as prismatic crystals, but also massive, granular, or compact. Cleavage: Indistinct. Specific Gravity: 2.65-2.91.

Formation & geological history

Rose Quartz forms in pegmatites and hydrothermal veins, often at high temperatures but can also form at lower temperatures. The pink color is believed to be caused by microscopic inclusions of dumortierite, a fibrous mineral, or by small amounts of titanium, iron, or manganese, or irradiation. Its geological age varies widely depending on the specific deposit, dating back millions to billions of years.

Uses & applications

Rose Quartz is primarily used as a gemstone in jewelry (cabochons, beads, carvings) and for ornamental purposes. It's also popular in the mineral collecting community and is widely used for metaphysical and healing practices.

Geological facts

Rose Quartz is strongly associated with love, compassion, and emotional healing. It's often used in meditation and crystal healing practices. Though common, high-quality, deeply colored transparent rose quartz is rare and highly prized by collectors.

Field identification & locations

In the field, Rose Quartz can be identified by its distinctive pink color, its vitreous luster, and its hardness (it can scratch glass and steel). It often occurs in massive forms, sometimes with a milky or translucent appearance. Common locations include Brazil (especially Minas Gerais), South Africa, United States (South Dakota), India, and Madagascar. For collectors, look for specimens with good color saturation, translucency, and minimal fractures. Tumbled pieces are very common and easily recognizable.