
mineral
Black Tourmaline
Schorl (Sodium Iron Aluminum Borosilicate Hydroxide), NaFe3Al6(BO3)3Si6O18(OH)4
AI-generated identification · may be incorrectHardness: 7-7.5 (Mohs); Color: Inky black; Luster: Vitreous to sub-metallic; Crystal structure: Trigonal/Hexagonal; Cleavage: Indistinct; Specific Gravity: 3.0-3.2
- Hardness
- 7-7
- Color
- Inky black
- Luster
- Vitreous to sub-metallic
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Physical properties
Hardness: 7-7.5 (Mohs); Color: Inky black; Luster: Vitreous to sub-metallic; Crystal structure: Trigonal/Hexagonal; Cleavage: Indistinct; Specific Gravity: 3.0-3.2
Formation & geological history
Formed primarily in pegmatites through hydrothermal processes and in metamorphic rocks like schists during the late stages of magmatic cooling, often as accessory minerals.
Uses & applications
Used in high-pressure gauges (due to piezoelectric properties), minor industrial abrasive, metaphysical crystals, and semi-precious jewelry.
Geological facts
It is both pyroelectric (generates electricity when heated) and piezoelectric (generates electricity under pressure). Historically, Dutch traders called it 'Aschentrekker' because it could attract fireplace ashes when heated.
Field identification & locations
Identify by its characteristic vertical striations (if untumbled), triangular cross-section, and deep opaque black color. Commonly found in Brazil, Africa, and the USA (California and Maine). Collectors look for well-terminated unchipped crystals.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous