
mineral
Schorl (Black Tourmaline)
Sodium Iron Aluminum Borosilicate Hydroxide; NaFe2+3Al6Si6O18(BO3)3(OH)3OH
Hardness: 7-7.5 (Mohs); Color: Jet black; Luster: Vitreous to sub-metallic; Crystal structure: Trigonal/Hexagonal with vertical striations (heavy ribbing); Cleavage: Indistinct; Specific Gravity: 3.0-3.2
- Hardness
- 7-7
- Color
- Jet black
- Luster
- Vitreous to sub-metallic
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Physical properties
Hardness: 7-7.5 (Mohs); Color: Jet black; Luster: Vitreous to sub-metallic; Crystal structure: Trigonal/Hexagonal with vertical striations (heavy ribbing); Cleavage: Indistinct; Specific Gravity: 3.0-3.2
Formation & geological history
Forms primarily in granitic pegmatites, hydrothermal veins, and metamorphic rocks such as schists and gneisses. It forms from boron-rich fluids during the final stages of magma crystallization.
Uses & applications
Used industrially in pressure gauges (due to piezoelectric properties), as an ore of boron, and widely in the gemstone/jewelry trade and metaphysical collecting markets.
Geological facts
Schorl is both pyroelectric (generates electricity when heated) and piezoelectric (generates electricity under pressure). It was reportedly used by early Dutch traders to pull ash out of meerschaum pipes, earning it the nickname 'Aschentrekker' (ash puller).
Field identification & locations
Identify in the field by its distinct triangular or rounded-triangular cross-section and deep vertical striations. Commonly found in Brazil, Namibia, and the USA (California and Maine). Look for it in coarse-grained igneous environments.
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