mineral

Rose quartz point

Quartz, silicon dioxide (SiO₂), pink variety

AI-generated identification · may be incorrect

Translucent pale pink with a vitreous luster and irregular, naturally rough sides; hardness 7 Mohs, trigonal crystal structure, and no true cleavage. The pointed top appears shaped or partly formed as a crystal termination.

Identified October 7, 2026More mineral →

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Physical properties

Formation & geological history

Rose quartz forms mainly in silica-rich pegmatites and hydrothermal veins, typically crystallizing as massive quartz rather than distinct crystals. Its geological age varies by deposit; pink color is associated with trace elements and microscopic inclusions.

Uses & applications

Used as a decorative and collectible specimen, and commonly cut for beads, carvings, and cabochons; it has little major industrial use compared with ordinary quartz.

Geological facts

Quartz is abundant in Earth’s crust and can scratch glass; rose quartz’s cloudy appearance commonly results from inclusions rather than a uniform pink crystal lattice.

Field identification & locations

Identify it by its pink color, glassy luster, hardness, and lack of cleavage; common sources include Brazil, Madagascar, India, and South Dakota. The image does not establish whether the point was naturally terminated or shaped.