mineral

Tumbled rose quartz

Quartz, silicon dioxide (SiO₂), with trace elements causing its pink color

AI-generated identification · may be incorrect

Mohs hardness 7; pale pink, translucent, with a vitreous luster and trigonal crystal structure. This polished piece has no visible cleavage and a curved, tumbled surface.

Identified October 7, 2026More mineral →

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Physical properties

Mohs hardness 7; pale pink, translucent, with a vitreous luster and trigonal crystal structure. This polished piece has no visible cleavage and a curved, tumbled surface.

Formation & geological history

Rose quartz forms in silica-rich pegmatites and hydrothermal settings; its pink color is linked to trace impurities or microscopic inclusions. The specimen’s geological age cannot be determined from the image.

Uses & applications

Used for beads, carvings, ornaments, and inexpensive jewelry; also collected as a common decorative mineral.

Geological facts

Quartz is one of Earth’s most abundant minerals. Rose quartz is typically massive rather than found as well-formed crystals.

Field identification & locations

The soft pink color, translucence, and hardness distinguish it from softer pink minerals; common sources include Brazil, Madagascar, India, and South Dakota. Image identification is limited, but it appears to be polished rose quartz.