mineral

Likely rose quartz fragment

Quartz (SiO₂), likely pale rose quartz

AI-generated identification · may be incorrect

Small, translucent pale pink-to-tan fragment with a vitreous to slightly dull surface; quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and conchoidal fracture. The image alone does not show enough detail to confirm the identification.

Identified September 29, 2026More mineral →

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Physical properties

Formation & geological history

Quartz forms in igneous and metamorphic settings and in hydrothermal veins; rose coloration is commonly associated with trace elements or microscopic inclusions. Quartz deposits range widely in age, from ancient crustal rocks to younger veins.

Uses & applications

Quartz is used in glass, electronics, abrasives, and construction; attractive rose quartz is cut or polished for jewelry and ornaments.

Geological facts

Quartz is among Earth’s most abundant minerals and often breaks with curved, shell-like surfaces rather than splitting along flat cleavage planes.

Field identification & locations

Check for glassy luster, hardness sufficient to scratch ordinary glass, and lack of cleavage; pink quartz commonly occurs in pegmatites and veins, notably in Brazil, Madagascar, and the United States. This small, unverified fragment has limited collector value.