Mineral

Rose Quartz

Quartz (SiO₂), specifically a variety of Quartz

AI-generated identification · may be incorrect

Hardness: 7 on the Mohs scale. Color: Pale pink to rose red, often translucent to opaque. Luster: Vitreous (glassy) to dull. Crystal structure: Typically occurs in massive forms, rarely forms distinct crystals. If crystals are present, they are hexagonal prisms. Rose quartz usually does not show cleavage.…

Hardness: 7 on the Mohs scale
Color: Pale pink to rose red, often translucent to opaque
Luster: Vitreous (glassy) to dull

Identified November 7, 2025More mineral →

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Physical properties

Formation & geological history

Rose Quartz forms primarily in pegmatites and hydrothermal veins, and is often found in massive occurrences. The pink color is believed to be caused by microscopic inclusions of dumortierite, or possibly by irradiation-induced color centers involving phosphorus or aluminum in the crystal structure. It forms at moderate to high temperatures, and its geological age can vary widely, from hundreds of millions to billions of years, depending on the specific geological event that formed the pegmatite or vein.

Uses & applications

Rose Quartz is widely used in jewelry (beads, cabochons, carvings), ornamental objects, and as a decorative stone. It is also popular in crystal healing practices and as an art material. Due to its relative abundance and attractive color, it is not considered exceptionally rare, but high-quality, deeply colored specimens are more valued.

Geological facts

Rose Quartz is often called the 'stone of universal love' and is associated with compassion, peace, and healing. While most quartz varieties are common, fine-quality rose quartz with strong coloration is less common. It is distinct from 'pink quartz' which can form euhedral (well-formed) crystals and is believed to get its color from different trace elements.

Field identification & locations

To identify rose quartz in the field, look for its distinctive pale pink to rose color and its glassy luster. It will be hard enough to scratch glass (Mohs 7). It commonly occurs in association with other pegmatite minerals. Major deposits are found in Brazil, South Africa, India, Madagascar, and the United States (especially South Dakota and Maine). Collectors look for good color saturation and translucency. The specimens in the image are polished beads, which would be common in jewelry or craft stores.

Other mineral specimens

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Gneiss or Schist

Gneiss or Mica Schist with Garnet

Metamorphic

Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Calcite–fluorite mineral specimen with iron-oxide staining

Calcite (CaCO₃), likely fluorite (CaF₂), with possible quartz and iron/manganese oxides

mineral

Mineral Sand (Heavy Mineral Sand Concentrate)

Placer deposit concentrate containing minerals such as ilmenite, rutile, zircon, and magnetite

mineral

Septarian Pebble

Septarian nodule / Concretion

sedimentary

Soil with Mineral Detritus and Quartz Fragments

Regolith / Silicate Mineral Aggregate

sedimentary