Rock Identifier
Polished tourmalinated quartz (Quartz (SiO₂) with black schorl tourmaline (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) inclusions) — mineral
mineral

Polished tourmalinated quartz

Quartz (SiO₂) with black schorl tourmaline (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) inclusions

AI-generated identification · may be incorrect

Typically hardness 7 for quartz and 7–7.5 for schorl; translucent gray-clear quartz contains irregular black, vitreous tourmaline patches or needles. Quartz is trigonal with no cleavage; tourmaline is trigonal and has indistinct cleavage. Specific gravity is about 2.65–3.2.

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Physical properties

Typically hardness 7 for quartz and 7–7.5 for schorl; translucent gray-clear quartz contains irregular black, vitreous tourmaline patches or needles. Quartz is trigonal with no cleavage; tourmaline is trigonal and has indistinct cleavage. Specific gravity is about 2.65–3.2.

Formation & geological history

Forms in hydrothermal quartz veins and pegmatites, where tourmaline crystallizes within growing quartz. Specimens may range from Paleozoic to Mesozoic or younger depending on locality.

Uses & applications

Used for cabochons, polished palm stones, beads, and ornamental objects; attractive examples are popular with mineral collectors.

Geological facts

The black component is usually schorl, the most common iron-rich tourmaline. The specimen appears intentionally cut and polished into a rounded cabochon or worry stone.

Field identification & locations

Identify it by its glassy quartz matrix and contrasting black tourmaline inclusions; unlike black mica, tourmaline does not split into flexible sheets. Common sources include Brazil, Madagascar, Pakistan, and the United States.