Rock Identifier
Likely rose quartz (Quartz, silicon dioxide (SiO₂), probably iron- or titanium-colored rose quartz) — mineral
mineral

Likely rose quartz

Quartz, silicon dioxide (SiO₂), probably iron- or titanium-colored rose quartz

AI-generated identification · may be incorrect

Small rough pink-to-reddish translucent specimen with a vitreous luster and irregular fracture; quartz has Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. The image does not show enough detail to confirm the identification.

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Physical properties

Small rough pink-to-reddish translucent specimen with a vitreous luster and irregular fracture; quartz has Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. The image does not show enough detail to confirm the identification.

Formation & geological history

Quartz forms in many igneous, metamorphic, and hydrothermal settings; rose coloration is commonly associated with trace elements or microscopic inclusions. The geological age cannot be determined from the photo.

Uses & applications

Used as a decorative and lapidary stone, in carvings and beads, and occasionally as a low-cost gemstone or collector specimen.

Geological facts

Quartz is one of Earth’s most abundant minerals and commonly breaks with curved, shell-like (conchoidal) surfaces.

Field identification & locations

Check for glassy luster, hardness sufficient to scratch ordinary glass, and absence of cleavage; these help distinguish quartz from softer pink minerals. Pink quartz is widespread, including in pegmatites, but this small image is insufficient to verify a local source near the reported coordinates.