Rock Identifier
Polished rose quartz (Quartz (silicon dioxide, SiO₂), rose-colored variety) — mineral
mineral

Polished rose quartz

Quartz (silicon dioxide, SiO₂), rose-colored variety

AI-generated identification · may be incorrect

Pink, translucent to cloudy, with a vitreous luster and massive texture; Mohs hardness 7, no cleavage, and uneven to conchoidal fracture. Quartz has a trigonal crystal structure; specific gravity is about 2.65.

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Physical properties

Pink, translucent to cloudy, with a vitreous luster and massive texture; Mohs hardness 7, no cleavage, and uneven to conchoidal fracture. Quartz has a trigonal crystal structure; specific gravity is about 2.65.

Formation & geological history

Forms mainly in pegmatites and quartz veins as silica-rich fluids cool; the pink color is associated with trace elements and microscopic inclusions. Rose quartz occurs in rocks of varied ages, often Precambrian.

Uses & applications

Used for carvings, ornamental objects, beads, and inexpensive jewelry; large polished pieces are popular decorative and collector specimens.

Geological facts

The specimen is shaped and polished, so its original crystal faces and field context are not visible.

Field identification & locations

Identify by its pink color, glassy sheen, hardness, and lack of cleavage; common sources include Brazil, Madagascar, South Africa, and the United States. The pictured egg-shaped polished specimen is roughly 15 cm tall.