mineral

Likely rough rose quartz

Quartz, SiO₂; pink color is typically caused by trace inclusions or defects

AI-generated identification · may be incorrect

Pale pink, translucent, glassy to slightly dull; quartz has a trigonal crystal structure, Mohs hardness 7, no cleavage, and conchoidal fracture. The photo is not detailed enough for a certain identification.

Identified October 3, 2026More mineral →

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Physical properties

Formation & geological history

Quartz commonly crystallizes from silica-rich fluids in pegmatites and hydrothermal veins; the specimen’s age and exact source cannot be determined from the image.

Uses & applications

Used for jewelry, carvings, ornamental objects, and mineral collecting; this small rough piece has little commercial value.

Geological facts

Rose quartz is often massive rather than forming distinct crystals; its pink color can fade with prolonged sunlight exposure.

Field identification & locations

Its pale pink color and hard, glassy fracture are consistent with rose quartz, but a scratch/hardness test and closer inspection would help distinguish it from other pink minerals. Quartz occurs worldwide, notably in Brazil, Madagascar, and the United States.