Rock Identifier
Tumbled black stone, likely black tourmaline (schorl) (Schorl, NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) — mineral
mineral

Tumbled black stone, likely black tourmaline (schorl)

Schorl, NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄

AI-generated identification · may be incorrect

Opaque black with a polished, vitreous-to-submetallic luster; tourmaline is trigonal, Mohs hardness 7–7.5, and has poor cleavage. The photo does not show enough detail to confirm the identification.

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Physical properties

Opaque black with a polished, vitreous-to-submetallic luster; tourmaline is trigonal, Mohs hardness 7–7.5, and has poor cleavage. The photo does not show enough detail to confirm the identification.

Formation & geological history

Black tourmaline forms in boron-rich granitic pegmatites and metamorphic rocks, commonly during late-stage crystallization. Such deposits occur across a wide range of geological ages.

Uses & applications

Tumbled pieces are used for jewelry, ornament, and mineral collecting; tourmaline is also valued as a gemstone.

Geological facts

Schorl is the most common tourmaline species and often grows as strongly striated, elongated crystals before being cut or tumbled.

Field identification & locations

A tumbled specimen may have its diagnostic crystal shape and striations removed; confirm by hardness and, ideally, mineral testing. Tourmaline is found in pegmatites worldwide, including Brazil, Africa, and the United States.