Rock Identifier
Blue aventurine or dyed blue quartzite pendant (Quartz (SiO₂), likely aventurine quartz/quartzite; exact identification requires testing) — metamorphic
metamorphic

Blue aventurine or dyed blue quartzite pendant

Quartz (SiO₂), likely aventurine quartz/quartzite; exact identification requires testing

AI-generated identification · may be incorrect

Dark blue, polished, mostly opaque with a vitreous to waxy luster; quartz hardness is about Mohs 7, with no cleavage and conchoidal fracture. The visible metal wirework and polish indicate a crafted jewelry piece rather than a raw specimen.

Identified More metamorphic
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Physical properties

Dark blue, polished, mostly opaque with a vitreous to waxy luster; quartz hardness is about Mohs 7, with no cleavage and conchoidal fracture. The visible metal wirework and polish indicate a crafted jewelry piece rather than a raw specimen.

Formation & geological history

Quartz-rich material formed through hydrothermal growth or metamorphism of sandstone; the blue color may result from inclusions, irradiation, or dyeing. Geological age and locality cannot be determined from the image.

Uses & applications

Used as ornamental stone and costume jewelry; value is primarily determined by craftsmanship, stone quality, and whether the color is natural. The metal setting appears decorative rather than diagnostic of the stone.

Geological facts

Blue aventurine is commonly colored by mineral inclusions such as dumortierite or riebeckite, while strongly uniform blue material is often dyed quartzite or glass. A scratch, streak, refractive-index, or magnification test is needed for confirmation.

Field identification & locations

Common sources of blue quartz and quartzite include Brazil, India, and Madagascar. Check for dye concentration in cracks, quartz-like hardness, lack of cleavage, and natural inclusions; avoid scratching the finished jewelry.