Rock Identifier
Black tourmaline (schorl), likely polished or tumbled (Schorl tourmaline — complex borosilicate, commonly approximated as NaFe²⁺₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) — mineral
mineral

Black tourmaline (schorl), likely polished or tumbled

Schorl tourmaline — complex borosilicate, commonly approximated as NaFe²⁺₃Al₆(BO₃)₃Si₆O₁₈(OH)₄

AI-generated identification · may be incorrect

Opaque black, vitreous to resinous luster, uneven fracture and commonly strong prismatic striations; Mohs hardness 7–7.5, specific gravity about 3.0–3.3. The image shows a dense dark specimen with a rough-polished surface; crystal faces are not clearly visible.

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Physical properties

Opaque black, vitreous to resinous luster, uneven fracture and commonly strong prismatic striations; Mohs hardness 7–7.5, specific gravity about 3.0–3.3. The image shows a dense dark specimen with a rough-polished surface; crystal faces are not clearly visible.

Formation & geological history

Forms mainly in granitic pegmatites and hydrothermal veins as late-stage crystals, typically in Precambrian to Phanerozoic rocks. Associated minerals include quartz, feldspar, mica, and lepidolite.

Uses & applications

Used as a collector mineral, ornamental stone, beads, carvings, and occasionally jewelry; gem-quality transparent tourmaline is more valuable than opaque schorl.

Geological facts

Tourmaline is piezoelectric and can become electrically charged when heated or pressed. Schorl is the most common tourmaline species and is generally iron-rich.

Field identification & locations

Identify it by black color, high hardness, elongated striated crystals, and inability to scratch it with a steel knife easily; a streak test is usually pale or colorless. Common localities include Brazil, Afghanistan, Pakistan, the United States, Madagascar, and Namibia.