Rock Identifier
Rose Quartz (tumbled) (Rose Quartz (variety of Quartz, chemical formula SiO₂)) — Mineral
Mineral

Rose Quartz (tumbled)

Rose Quartz (variety of Quartz, chemical formula SiO₂)

Hardness: 7 on Mohs scale. Color: Pale pink to deep rose red, often translucent or turbid. Luster: Vitreous (glassy) to dull. Crystal Structure: Trigonal, typically massive or as aggregates, well-formed crystals are rare. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Pale pink to deep rose red, often translucent or turbid
Luster
Vitreous (glassy) to dull
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale. Color: Pale pink to deep rose red, often translucent or turbid. Luster: Vitreous (glassy) to dull. Crystal Structure: Trigonal, typically massive or as aggregates, well-formed crystals are rare. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Rose Quartz typically forms in hydrothermal veins and pegmatites. The pink color is believed to be caused by microscopic inclusions of dumortierite, though some theories suggest irradiation and the presence of titanium, iron, or manganese. Its geological age varies widely depending on the specific deposit, but it is found in formations ranging from Precambrian to Cenozoic.

Uses & applications

Rose Quartz is primarily used as a gemstone in jewelry (cabochons, beads, carvings) and for ornamental purposes. Due to its attractive color and reasonable hardness, it is popular for sculptures, decorative objects, and as tumbled stones. It is also used in crystal healing practices.

Geological facts

Rose Quartz is often called the 'stone of universal love.' While true rose quartz crystals are extremely rare, the massive form is quite common. The color can fade with prolonged exposure to sunlight. The finest specimens often come from Brazil and South Africa.

Field identification & locations

In the field, Rose Quartz can be identified by its distinctive pink color, glassy luster, and hardness (it will scratch glass). It typically occurs as large, anhedral masses within pegmatites or hydrothermal veins. Tumbled specimens like the one pictured are smooth and polished, making identification often based on color and translucency. Common locations include Brazil, South Africa, India, Madagascar, and parts of the USA. For collectors, look for vibrant, evenly colored pieces without significant inclusions or cloudiness, though some cloudiness is characteristic.